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  • 1
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    Unbekannt
    (Figure 2) Proxy records of sediment core GeoB6007-2 (2010)
    PANGAEA
    In:  Supplement to: Bamberg, Audrey; Rosenthal, Yair; Paul, André; Heslop, David; Mulitza, Stefan; Rühlemann, Carsten; Schulz, Michael (2010): Reduced North Atlantic Central Water formation in response to early Holocene ice-sheet melting. Geophysical Research Letters, 37, L17705, https://doi.org/10.1029/2010GL043878
    Details
    Publikationsdatum: 2024-05-31
    Beschreibung: Central waters of the North Atlantic are fundamental for ventilation of the upper ocean and are also linked to the strength of the Atlantic Meridional Overturning Circulation (AMOC). Here, we show based on benthic foraminiferal Mg/Ca ratios, that during times of enhanced melting from the Laurentide Ice Sheet (LIS) between 9.0-8.5 thousand years before present (ka) the production of central waters weakened the upper AMOC resulting in a cooling over the Northern Hemisphere. Centered at 8.54 ± 0.2 ka and 8.24 ± 0.1 ka our dataset records two ~150-year cooling events in response to the drainage of Lake Agassiz/Ojibway, indicating early slow-down of the upper AMOC in response to the initial freshwater flux into the subpolar gyre (SPG) followed by a more severe weakening of both the upper and lower branches of the AMOC at 8.2 ka. These results highlight the sensitivity of regional North Atlantic climate change to the strength of central-water overturning and exemplify the impact of both gradual and abrupt freshwater fluxes on eastern SPG surface water convection. In light of the possible future increase in Greenland Ice Sheet melting due to global warming these findings may help us to better constrain and possibly predict future North Atlantic climate change.
    Schlagwort(e): BGR; Bundesanstalt für Geowissenschaften und Rohstoffe, Hannover; Center for Marine Environmental Sciences; GeoB6007-2; Gravity corer (Kiel type); Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; M45/5a; MARUM; Meteor (1986); SL
    Materialart: Dataset
    Format: application/zip, 2 datasets
    Standort Signatur Erwartet Verfügbarkeit
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    DATEN PANGAEA
  • 2
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    Unbekannt
    Expanded GHOST database (2010)
    PANGAEA
    In:  Supplement to: Leduc, Guillaume; Schneider, Ralph R; Kim, Jung-Hyun; Lohmann, Gerrit (2010): Holocene and Eemian Sea surface temperature trends as revealed by alkenone and Mg/Ca paleothermometry. Quaternary Science Reviews, 29(7-8), 989-1004, https://doi.org/10.1016/j.quascirev.2010.01.004
    Details
    Publikationsdatum: 2024-05-31
    Beschreibung: In this study we review a global set of alkenone- and foraminiferal Mg/Ca-derived sea surface temperatures (SST) records from the Holocene and compare them with a suite of published Eemian SST records based on the same approach. For the Holocene, the alkenone SST records belong to the actualized GHOST database (Kim, J.-H., Schneider R.R., 2004). The actualized GHOST database not only confirms the SST changes previously described but also documents the Holocene temperature evolution in new oceanic regions such as the Northwestern Atlantic, the eastern equatorial Pacific, and the Southern Ocean. A comparison of Holocene SST records stemming from the two commonly applied paleothermometry methods reveals contrasting - sometimes divergent - SST evolution, particularly at low latitudes where SST records are abundant enough to infer systematic discrepancies at a regional scale. Opposite SST trends at particular locations could be explained by out-of-phase trends in seasonal insolation during the Holocene. This hypothesis assumes that a strong contrast in the ecological responses of coccolithophores and planktonic foraminifera to winter and summer oceanographic conditions is the ultimate reason for seasonal differences in the origin of the temperature signal provided by these organisms. As a simple test for this hypothesis, Eemian SST records are considered because the Holocene and Eemian time periods experienced comparable changes in orbital configurations, but had a higher magnitude in insolation variance during the Eemian. For several regions, SST changes during both interglacials were of a similar sign, but with higher magnitudes during the Eemian as compared to the Holocene. This observation suggests that the ecological mechanism shaping SST trends during the Holocene was comparable during the penultimate interglacial period. Although this "ecology hypothesis" fails to explain all of the available results, we argue that any other mechanism would fail to satisfactorily explain the observed SST discrepancies among proxies.
    Schlagwort(e): 108-658C; 138-846; 160-967D; 160-969E; 161-977; 162-984; 165-1002C; 165-999A; 167-1012B; 167-1017E; 167-1019C; 175-1078C; 175-1084B; 184-1145C; 2; 202-1233; 202-1240; 202-1242; 225514; 225517; 71; 90b; 96; 96-619; A-7; AD91-17; Alboran Sea; also published as VM28-122; Angola Basin; Arabian Sea; Arctic Ocean; Atlantic Ocean; AUSCAN; Bay of Bengal; BCR; BENEFIT/4; BENGAL FAN; Benguela Current, South Atlantic Ocean; BOFS31/1K; BOFS31#1; Box corer (Reineck); BS79-33; BS79-38; CALYPSO; Calypso Corer; Canarias Sea; Caribbean Sea; Cayman Rise, Caribbean Sea; CD159-12; CD53; CEPAG; CH07-98-GGC19; Charles Darwin; Chatham Rise; CHIPAL; Cocos Ridge; COMPCORE; Composite Core; Congo Fan; D13882; D249; De Soto Canyon; Discovery (1962); DRILL; Drilling/drill rig; Eastern Basin; East Pacific; Emperor Seamounts; Equatorial East Pacific; GC; GeoB1023-5; GeoB3129-1; GeoB3313-1; GeoB3910-2; GeoB4509-2; GeoB4905-4; GeoB5546-2; GeoB5844-2; GeoB5901-2; GeoB6007-2; GeoB6518-1; GeoB7139-2; GeoB7926-2; GEOSCIENCES, MARMARCORE; GeoTü SL71; GGC; GGC-15-1; Giant box corer; Giant gravity corer; Giant piston corer; GIK17748-2; GIK17940-2; GIK17964-1; GIK18252-3; GIK18287-3; GIK23258-2; GINCO 3; GKG; Glomar Challenger; GPC; Gravity corer; Gravity corer (Kiel type); Gulf of Mexico; Hakuho-Maru; HOTLINE, HYGAPE; IMAGES I; IMAGES III - IPHIS; IMAGES IV-IPHIS III; IMAGES IX - PAGE; IMAGES V; IMAGES VIII - MONA; IMAGES VII - WEPAMA; Indian Ocean; Indonesia; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; IOW225514; IOW225517; IOW4509B; James Clark Ross; Joides Resolution; JOPSII-6; JR20000727; JR51; JR51GC-35; JT96-0909PC; KAL; Kasten corer; KH-01-3; KH-01-3-19; KL; KL_Mg; Knorr; KNR176-2; KNR176-JPC32; Kurilen Trench; LAPAZ21P; Leg108; Leg138; Leg160; Leg161; Leg162; Leg165; Leg167; Leg175; Leg184; Leg202; Leg96; Le Suroît; M34/4; M35/1; M35003-4; M39/1; M39/1_08-3; M39008-3; M40/4; M40/4_87-6SL; M40/4_SL67; M40/4_SL71; M40/4_SL78; M40/4_SL78-3; M40/4_SL87; M41/1; M42/4b; M44/1; M44/1_74KL; M44/1_KL71; M44/3; M45/1; M45/5a; M47/3; M53/1; M6/6; M7/2; Marge Ibérique; Marion Dufresne (1972); Marion Dufresne (1995); Marmara Sea; MD01-2334; MD012378; MD01-2378; MD012390; MD01-2390; MD012412; MD01-2412; MD012416; MD01-2416; MD01-2443; MD022529; MD02-2529; MD022575; MD02-2575; MD032611G; MD03-2611G; MD03-2707; MD101; MD106; MD111; MD114; MD122; MD123; MD126; MD127; MD13; MD131; MD77-194; MD79-257; MD85674; MD94-103; MD952011; MD95-2011; MD952015; MD95-2015; MD952042; MD95-2042; MD952043; MD95-2043; MD972120; MD97-2120; MD972121; MD97-2121; MD972125; MD97-2125; MD972141; MD97-2141; MD972151; MD97-2151; MD982162; MD98-2162; MD982165; MD98-2165; MD982170; MD98-2170; MD982176; MD98-2176; MD982181; MD98-2181; MD99-2155; MD99-2251; MD99-2334; ME0005A; ME0005A-24JC; Melville; Meteor (1986); MONITOR MONSUN; NE-Brazilian continental margin; NEMO; Northeast Atlantic; Northeast Brasilian Margin; Northern Red Sea; North Pacific Ocean; North-West African margin; OCE326-GGC26; OCE326-GGC30; off Cameroon; OSIRIS4; OSIRIS III; Pacific Ocean; PAKOMIN; PC; PC-17; PC-2; PC-4; Petr Kottsov; Piston corer; Piston corer (BGR type); Piston corer Meischner large; PL07-39PC; Portuguese Margin; PUCK; RAPID-12-1K; RC11; RC1112; RC11-238; Reykjanes Ridge; RL11; Robert Conrad; Rockall; SCS90-36; SL; SO102/1; SO115; SO115_05; SO115_40; SO136; SO136_011GC; SO139; SO139-74KL; SO156/2; SO80_4; SO80a; SO90; SO90_136KL; SO90_39KG; SO90_93KL; SO93/3; SO93/3_126KL; SO95; Sonne; South Atlantic Ocean; South China Sea; South-East Pacific; Southern Ocean; Southern Okhotsk Sea; South Pacific Ocean; SSDP102; St.14; St.20; SU81-18; SUNDAFLUT; Sunda Shelf; TASQWA; Timor Sea; TN057-21; TR163-19; TR163-22; TY93-905; TY93929/P; U938; V19; V19-27; V19-28; V19-30; V21; V21-30; V28; V28-122; Vema; Victor Hensen; Vietnam shelf; Voring Plateau
    Materialart: Dataset
    Format: application/zip, 133 datasets
    Standort Signatur Erwartet Verfügbarkeit
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    DATEN PANGAEA
  • 3
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    Sr/Ca and stable isotope records of Diplora strigosa coral sample BON-9-A from the east coast of Bonaire (2010)
    PANGAEA
    In:  Supplement to: Giry, Cyril; Felis, Thomas; Kölling, Martin; Scheffers, Sander R (2010): Geochemistry and skeletal structure of Diploria strigosa, implications for coral-based climate reconstruction. Palaeogeography, Palaeoclimatology, Palaeoecology, 298, 378-387, https://doi.org/10.1016/j.palaeo.2010.10.022
    Details
    Publikationsdatum: 2024-05-31
    Beschreibung: Geochemical tracers incorporated into the skeleton of reef-building corals are ideal proxies for reconstructing environmental parameters of ambient seawater such as temperature and salinity at subseasonal resolution. However, validation concerns of these environmental proxies due to the complex skeleton of some tropical Atlantic corals have hindered such coral-based environmental reconstructions in this region compared to the tropical Pacific. In order to identify complications associated with the complex skeletal architecture of the massive brain coral Diploria strigosa, we performed microsampling experiments along and across individual skeletal elements. We demonstrate that the mesoscale heterogeneity of Sr/Ca, d18O and d13C is a systematic feature of D. strigosa and is linked to different vital effects between skeletal elements. The thecal wall is significantly depleted in Sr, 18O and 13C compared to the adjacent septa and columella and differences between apparent temperature signatures of several degrees are greater for Sr/Ca suggesting that this temperature proxy is more sensitive to skeletal mixing than d18O. Parallel subseasonal microsampling experiments performed along individual skeletal elements of a single corallite of a D. strigosa coral which grew at a rate of 0.65 cm/year allow for investigating potential biases associated with its complex skeletal mesoarchitecture. Highest correlation between Sr/Ca and d18O from skeletal material retrieved from the centre of the thecal wall suggests that microdrilling the theca provides the best environmental signal compared to adjacent microsampling profiles. Moreover, based on monthly-mean climatology, the temperature dependence of Sr/Ca for this profile is comparable to previous calibrations published from faster growing D. strigosa. Based on these results, we conclude that accurate microsampling along the centre of the thecal wall of D. strigosa is a prerequisite for generating robust climate reconstructions from its skeleton.
    Schlagwort(e): BON-9-A; CaribClim_Coral_2006; Center for Marine Environmental Sciences; DRILL; Drilling/drill rig; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; MARUM; Southern Caribbean Sea, Bonaire
    Materialart: Dataset
    Format: application/zip, 3 datasets
    Standort Signatur Erwartet Verfügbarkeit
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    DATEN PANGAEA
  • 4
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    Planktic foraminiferal distribution and stable isotope ratios of sediment core MSM05/5_712-1 from the Arctic Ocean (2011)
    PANGAEA
    In:  Supplement to: Spielhagen, Robert F; Werner, Kirstin; Sørensen, Steffen Aagaard; Zamelczyk, Katarzyna; Kandiano, Evgenia S; Budéus, Gereon; Husum, Katrine; Marchitto, Thomas M; Hald, Morten (2011): Enhanced modern heat transfer to the Arctic by warm Atlantic water. Science, 331(6016), 450-453, https://doi.org/10.1126/science.1197397
    Details
    Publikationsdatum: 2024-05-31
    Beschreibung: The Arctic is responding more rapidly to global warming than most other areas on our planet. Northward flowing Atlantic Water is the major means of heat advection towards the Arctic and strongly affects the sea ice distribution. Records of its natural variability are critical for the understanding of feedback mechanisms and the future of the Arctic climate system, but continuous historical records reach back only ~150 years. Here, we present a multidecadal scale record of ocean temperature variations during the last 2000 years, derived from marine sediments off Western Svalbard (79°N). We find that early-21st-century temperatures of Atlantic Water entering the Arctic Ocean are unprecedented over the past 2000 years and are presumably linked to the Arctic Amplification of global warming.
    Schlagwort(e): CTD/Rosette; CTD-RO; Fram Strait; Giant box corer; GKG; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; International Polar Year (2007-2008); IPY; Jan Mayen; JM06-WP; JM06-WP-02; Maria S. Merian; MSM05/5; MSM05/5_712-1; MSM05/5_713-1; North Greenland Sea; WarmPast 2006
    Materialart: Dataset
    Format: application/zip, 4 datasets
    Standort Signatur Erwartet Verfügbarkeit
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    DATEN PANGAEA
  • 5
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    Unbekannt
    Geochemistry on Holocene sediments from the Mediterranean (2011)
    PANGAEA
    In:  Supplement to: Möbius, Jürgen; Lahajnar, Niko; Emeis, Kay-Christian (2010): Diagenetic control of nitrogen isotope ratios in Holocene sapropels and recent sediments from the Eastern Mediterranean Sea. Biogeosciences, 7, 3901-3914, https://doi.org/10.5194/bg-7-3901-2010
    Details
    Publikationsdatum: 2024-05-31
    Beschreibung: The enhanced accumulation of organic matter in Eastern Mediterranean sapropels and their unusually low d15N values have been attributed to either enhanced nutrient availability which led to elevated primary production and carbon sequestration or to enhanced organic matter preservation under anoxic conditions. In order to evaluate these two hypothesis we have determined Ba/Al ratios, amino acid composition, N and organic C concentrations and d15N in sinking particles, surface sediments, eight spatially distributed core records of the youngest sapropel S1 (10-6 ka) and older sapropels (S5, S6) from two locations. These data suggest that (i) temporal and spatial variations in d15N of sedimentary N are driven by different degrees of diagenesis at different sites rather than by changes in N-sources or primary productivity and (ii) present day TOC export production would suffice to create a sapropel like S1 under conditions of deep-water anoxia. This implies that both enhanced TOC accumulation and d15N depletion in sapropels were due to the absence of oxygen in deep waters. Thus preservation plays a major role for the accumulation of organic-rich sediments casting doubt on the need of enhanced primary production for sapropel formation.
    Schlagwort(e): 101; 101-105; 106-111; 107; 111; 112-116; 116; 117-122; 118; 123-126; 137-139; 140-142; 143-148; 149-154; 155-162; 163-170; 171-179; 180-187; 188-194; 560; 561; 562; 563; 564; 565; 566; 569; 570; 571; 572; 573; 574; 575; 576; 577; 578; 579; 580; 581; 582; 584; 585; 586; 589; 590; 592; 594; 596; 599; 601; 602; 604; 666; 667; 668; 670; 671; 672; 673; 674; 676; 677; 678; 680; 681; 682; 683; 684; 685; 686; 687; 689; 690; 691; 692; 693; 694; 695; 696; 697; 699; 700; 701; 702; 703; 704; 705; 706; 707; 708; 709; 710; 712; 713; 714; 716; 717; 718; 719; 80; 82; 85; Cyprus; Eastern Mediterranean, Continental slope off Israel; Eratosthenes Seamount; Gargano Promontory; GeoB10701-4; GeoB10702-3; GeoB10703-3; GeoB10704-3; GeoB10705-3; GeoB10706-3; GeoB10707-4; GeoB10708-3; GeoB10710-4; GeoB10711-3; GeoB10712-3; GeoB10713-3; GeoB10714-3; GeoB10715-3; GeoB10716-3; GeoB10717-3; GeoB10718-3; GeoB10719-3; GeoB10720-5; GeoB10721-3; GeoB10722-3; GeoB10723-3; GeoB10724-3; GeoB10725-3; GeoB10726-3; GeoB10727-3; GeoB10728-3; GeoB10729-4; GeoB10730-3; GeoB10731-3; GeoB10732-3; GeoB10733-3; GeoB10734-3; GeoB10735-3; GeoB10736-3; GeoB10737-3; GeoB10738-3; GeoB10739-3; GeoB10740-3; GeoB10741-3; GeoB10742-3; GeoB10743-3; GeoB10744-3; GeoB10746-3; GeoB10747-3; GeoB10748-3; GeoB10749-3; GeoB7704-1; GeoB7705-1; GeoB7706-2; GeoB7714-1; GeoB7718-1; GeoB7720-1; GeoB7723-2; GeoB7725-2; Gravity corer (Kiel type); Greece; Gulf of Manfredonia; Gulf of Taranto; Haifa; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; Lybia; M40/4; M40/4_MUC65; M40/4_MUC66; M40/4_MUC67; M40/4_MUC68; M40/4_MUC69; M40/4_MUC70; M40/4_MUC71; M40/4_MUC72; M40/4_MUC73; M40/4_MUC74; M40/4_MUC75; M40/4_MUC76-2; M40/4_MUC76-3; M40/4_MUC77A; M40/4_MUC77B; M40/4_MUC78-2; M40/4_MUC79; M40/4_MUC81; M40/4_MUC82; M40/4_MUC84; M40/4_MUC85; M40/4_MUC86; M40/4_MUC87; M40/4_MUC88; M40/4_MUC89; M40/4_MUC90; M40/4_MUC91; M40/4_SL80; M51/3; M51/3_560-1; M51/3_561-4; M51/3_562-5; M51/3_563-5; M51/3_564-2; M51/3_565-1; M51/3_566-3; M51/3_569-3; M51/3_570-2; M51/3_571; M51/3_572-2; M51/3_573; M51/3_574-2; M51/3_575-6; M51/3_576-3; M51/3_577-1; M51/3_578; M51/3_579; M51/3_580; M51/3_581; M51/3_582; M51/3_584; M51/3_585; M51/3_586; M51/3_589; M51/3_590; M51/3_592; M51/3_594; M51/3_596; M51/3_599; M51/3_601-3; M51/3_602; M51/3_604; M52/2; M71/3; M71/3_H01; M71/3_H02; M71/3_H03; M71/3_H04; M71/3_H05; M71/3_H06; M71/3_H07; M71/3_H11; M71/3_H12; M71/3_Her01; M71/3_Her03; M71/3_ler01; M71/3_Rho02; M71/3_Sk01; Malta; Meteor (1986); MUC; MultiCorer; Nile Fan; POS339; Poseidon; SL; Strait of Otranto; Turkey; Zyprus
    Materialart: Dataset
    Format: application/zip, 6 datasets
    Standort Signatur Erwartet Verfügbarkeit
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  • 6
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    Alkenone-derived sea surface temperature records of three sediment cores from the southern Benguela upwelling system (2010)
    PANGAEA
    In:  Supplement to: Leduc, Guillaume; Herbert, Caren T; Blanz, Thomas; Martinez, Philippe; Schneider, Ralph R (2010): Contrasting evolution of sea surface temperature in the Benguela upwelling system under natural and anthropogenic climate forcings. Geophysical Research Letters, 37, L20705, https://doi.org/10.1029/2010GL044353
    Details
    Publikationsdatum: 2024-05-31
    Beschreibung: We present alkenone-derived Sea Surface Temperature (SST) records from three marine cores collected within the southern Benguela Upwelling System (BUS) spanning the last 3 ka. The SST evolution over the last 3 millennia is marked by aperiodic millennial-scale oscillations that broadly correspond to climatic anomalies identified over the North Atlantic region. The BUS SST data further suggest cooling and warming trends opposite to the temperature evolution in the Moroccan upwelling region and in Antarctica. In contrast, the last decades are marked by a cooling of unprecedented magnitude in both the Benguela and Moroccan upwelling systems, which is not observed in the Antarctic record. These contrasted responses in Atlantic upwelling systems triggered by natural and anthropogenic forcings shed light on how different climatic mechanisms are mediated by ocean-atmosphere interactions and transmitted to the geological records of past and present climate changes.
    Schlagwort(e): Center for Marine Environmental Sciences; GeoB; Geosciences, University of Bremen; GIK/IfG; Institute for Geosciences, Christian Albrechts University, Kiel; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; MARUM
    Materialart: Dataset
    Format: application/zip, 3 datasets
    Standort Signatur Erwartet Verfügbarkeit
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    DATEN PANGAEA
  • 7
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    Monthly Bonaire coral Sr/Ca from the last interglacial, 120.5 -129.7 ka ago (2016)
    PANGAEA
    In:  Supplement to: Brocas, William M; Felis, Thomas; Obert, J Christina; Gierz, Paul; Lohmann, Gerrit; Scholz, Denis; Kölling, Martin; Scheffers, Sander R (2016): Last interglacial temperature seasonality reconstructed from tropical Atlantic corals. Earth and Planetary Science Letters, 449, 418-429, https://doi.org/10.1016/j.epsl.2016.06.005
    Details
    Publikationsdatum: 2024-05-31
    Beschreibung: Reconstructions of last interglacial (LIG, MIS 5e, ~127-117 ka) climate offer insights into the natural response and variability of the climate system during a period partially analogous to future climate change scenarios. We present well preserved fossil corals (Diploria strigosa) recovered from the southern Caribbean island of Bonaire (Caribbean Netherlands). These have been precisely dated by the 230Th/U-method to between 130 and 120 ka ago. Annual banding of the coral skeleton enabled construction of time windows of monthly resolved strontium/calcium (Sr/Ca) temperature proxy records. In conjunction with a previously published 118 ka coral record, our eight records of up to 37 years in length, cover a total of 105 years within the LIG period. From these, sea surface temperature (SST) seasonality and variability in the tropical North Atlantic Ocean is reconstructed. We detect similar to modern SST seasonality of ~2.9 °C during the early (130 ka) and the late LIG (120-118 ka). However, within the mid-LIG, a significantly higher than modern SST seasonality of 4.9 °C (at 126 ka) and 4.1 °C (at 124 ka) is observed. These findings are supported by climate model simulations and are consistent with the evolving amplitude of orbitally induced changes in seasonality of insolation throughout the LIG, irrespective of wider climatic instabilities that characterised this period. The climate model simulations suggest that the SST seasonality changes documented in our LIG coral Sr/Ca records are representative of larger regions within the tropical North Atlantic. These simulations also suggest that the reconstructed SST seasonality increase during the mid-LIG is caused primarily by summer warming. A 124 ka old coral documents, for the first time, evidence of decadal SST variability in the tropical North Atlantic during the LIG, akin to that observed in modern instrumental records.
    Schlagwort(e): Center for Marine Environmental Sciences; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; MARUM
    Materialart: Dataset
    Format: application/zip, 7 datasets
    Standort Signatur Erwartet Verfügbarkeit
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  • 8
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    Monthly Bonaire coral δ¹⁸O and d18Oseawater from the last interglacial, 120.5 -129.7 ka ago (2017)
    PANGAEA
    In:  Supplement to: Brocas, William M; Felis, Thomas; Gierz, Paul; Lohmann, Gerrit; Werner, Martin; Obert, J Christina; Scholz, Denis; Kölling, Martin; Scheffers, Sander R (2018): Last interglacial hydroclimate seasonality reconstructed from tropical Atlantic corals. Paleoceanography and Paleoclimatology, 33(2), 198-213, https://doi.org/10.1002/2017PA003216
    Details
    Publikationsdatum: 2024-05-31
    Beschreibung: The seasonality of hydroclimate during past periods of warmer than modern global temperatures is a critical component for understanding future climate change scenarios. Although partially analogous to these scenarios, the last interglacial (LIG, Marine Isotope Stage 5e, ~127-117 ka) is a popular test-bed. We present coral d18O monthly resolved records from multiple Bonaire (southern Caribbean) fossil corals (Diploria strigosa) that date to between 130 and 118 ka. These records represent up to 37 years and cover a total of 105 years, offering insights into the seasonality and characteristics of LIG tropical Atlantic hydroclimate. Our coral d18O records and available coral Sr/Ca- sea surface temperature (SST) records reveal new insights into the variable relationship between the seasonality of tropical Atlantic seawater d18O (d18Oseawater) and SST. Coral d18O seasonality is found to coevolve with SST and insolation seasonality throughout the LIG, culminating in significantly higher than modern values at 124 and 126 ka. At 124 ka, we reconstruct a 2-month lead of the coral d18O vs. the Sr/Ca-SST annual cycle and increased d18Oseawater seasonality. A fully-coupled climate model simulates a concomitant increase of southern Caribbean Sea summer precipitation and depletion of summer d18Oseawater. LIG regional hydroclimate differed from today's semiarid climate with a minor rainy season during winter. Cumulatively our coral d18O, d18Oseawater and model findings indicate a mid-LIG northward expansion of the South American Intertropical Convergence Zone into the southern Caribbean Sea, highlighting the importance of regional aspects within reconstructions of LIG hydroclimate seasonality.
    Schlagwort(e): Center for Marine Environmental Sciences; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; MARUM
    Materialart: Dataset
    Format: application/zip, 7 datasets
    Standort Signatur Erwartet Verfügbarkeit
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  • 9
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    Unbekannt
    Reference list of sources used for two experimental data files dataBSRN and dataMixed (2011)
    PANGAEA
    Details
    Publikationsdatum: 2024-05-31
    Beschreibung: Increasing amounts of data is collected in most areas of research and application. The degree to which this data can be accessed, analyzed, and retrieved, is a decisive in obtaining progress in fields such as scientific research or industrial production. We present a novel methodology supporting content-based retrieval and exploratory search in repositories of multivariate research data. In particular, our methods are able to describe two-dimensional functional dependencies in research data, e.g. the relationship between ination and unemployment in economics. Our basic idea is to use feature vectors based on the goodness-of-fit of a set of regression models to describe the data mathematically. We denote this approach Regressional Features and use it for content-based search and, since our approach motivates an intuitive definition of interestingness, for exploring the most interesting data. We apply our method on considerable real-world research datasets, showing the usefulness of our approach for user-centered access to research data in a Digital Library system.
    Materialart: Dataset
    Format: 7498 datasets
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  • 10
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    Unbekannt
    Raw data from 2.35 ka Bonaire coral, sample BON-6-A (2011)
    PANGAEA
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): Attributed to extreme Sr/Ca values of any single year; BON-6-A; CaribClim_Coral_2006; Center for Marine Environmental Sciences; Diploria strigosa, Strontium/Calcium ratio; Diploria strigosa, δ18O; DISTANCE; DRILL; Drilling/drill rig; Estimated based on subannual extension-rate and tie points; ICP-OES, Perkin-Elmer, Optima 3300R; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; Internal coral chronology; MARUM; Mass spectrometer Finnigan MAT 251; referred samples; Sample ID; Southern Caribbean Sea, Bonaire; Tie point
    Materialart: Dataset
    Format: text/tab-separated-values, 3189 data points
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  • 11
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    (Fig. 4) Multiproxy data set of box core MSM5/5-712-1 (2011)
    PANGAEA
    In:  Supplement to: Werner, Kirstin; Spielhagen, Robert F; Bauch, Dorothea; Hass, H Christian; Kandiano, Evgenia S; Zamelczyk, Katarzyna (2011): Atlantic Water advection to the eastern Fram Strait - multiproxy evidence for late Holocene variability. Palaeogeography, Palaeoclimatology, Palaeoecology, 308(3-4), 264-276, https://doi.org/10.1016/j.palaeo.2011.05.030
    Details
    Publikationsdatum: 2024-05-31
    Beschreibung: A multiproxy data set of an AMS radiocarbon dated 46 cm long sediment core from the continental margin off western Svalbard reveals multidecadal climatic variability during the past two millennia. Investigation of planktic and benthic stable isotopes, planktic foraminiferal fauna, and lithogenic parameters aims to unveil the Atlantic Water advection to the eastern Fram Strait by intensity, temperatures, and salinities. Atlantic Water has been continuously present at the site over the last 2,000 years. Superimposed on the increase in sea ice/icebergs, a strengthened intensity of Atlantic Water inflow and seasonal ice-free conditions were detected at ~ 1000 to 1200 AD, during the well-known Medieval Climate Anomaly (MCA). However, temperatures of the MCA never exceeded those of the 20th century. Since ~ 1400 AD significantly higher portions of ice rafted debris and high planktic foraminifer fluxes suggest that the site was located in the region of a seasonal highly fluctuating sea ice margin. A sharp reduction in planktic foraminifer fluxes around 800 AD and after 1730 AD indicates cool summer conditions with major influence of sea ice/icebergs. High amounts of the subpolar planktic foraminifer species Turborotalia quinqueloba in size fraction 150–250 µm indicate strengthened Atlantic Water inflow to the eastern Fram Strait already after ~ 1860 AD. Nevertheless surface conditions stayed cold well into the 20th century indicated by low planktic foraminiferal fluxes. Most likely at the beginning of the 20th century, cold conditions of the terminating Little Ice Age period persisted at the surface whereas warm and saline Atlantic Water already strengthened, hereby subsiding below the cold upper mixed layer. Surface sediments with high abundances of subpolar planktic foraminifers indicate a strong inflow of Atlantic Water providing seasonal ice-free conditions in the eastern Fram Strait during the last few decades.
    Schlagwort(e): Accumulation rate, ice rafted debris by number; Age; AGE; Calculated, see reference(s); Cibicidoides wuellerstorfi, δ13C; Cibicidoides wuellerstorfi, δ18O; DEPTH, sediment/rock; Foraminifera, planktic, flux; Fram Strait; Giant box corer; GKG; Ice rafted debris; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; Maria S. Merian; Mass spectrometer, Finnigan, MAT 253; MSM05/5; MSM05/5_712-1; Neogloboquadrina pachyderma sinistral, δ13C; Neogloboquadrina pachyderma sinistral, δ18O; Sea surface salinity; Size fraction 1.000-0.063 mm; Sortable-silt mean
    Materialart: Dataset
    Format: text/tab-separated-values, 971 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 12
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    40-year long monthly-resolved Sr/Ca record from 2.35 ka Bonaire coral, sample BON-6-A (2010)
    PANGAEA
    In:  Supplement to: Giry, Cyril; Felis, Thomas; Scheffers, Sander R; Fensterer, Claudia (2010): Assessing the potential of Southern Caribbean corals for reconstructions of Holocene temperature variability. IOP Conference Series: Earth and Environmental Science, 9(1), 012021, https://doi.org/10.1088/1755-1315/9/1/012021
    Details
    Publikationsdatum: 2024-05-31
    Beschreibung: We present a 40-year long monthly resolved Sr/Ca record from a fossil Diploria strigosa coral from Bonaire (Southern Caribbean Sea) dated with U/Th at 2.35 ka before present (BP). Secondary modifiers of this sea surface temperature (SST) proxy in annually-banded corals such as diagenetic alteration of the skeleton and skeletal growth-rate are investigated. Extensive diagenetic investigations reveal that this fossil coral skeleton is pristine which is further supported by clear annual cycles in the coral Sr/Ca record. No significant correlation between annual growth rate and Sr/Ca is observed, suggesting that the Sr/Ca record is not affected by coral growth. Therefore, we conclude that the observed interannual Sr/Ca variability was influenced by ambient SST variability. Spectral analysis of the annual mean Sr/Ca record reveals a dominant frequency centred at 6–7 years that is not associated with changes of the annual growth rate. The first monthly resolved coral Sr/Ca record from the Southern Caribbean Sea for preindustrial time suggests that fossil corals from Bonaire are suitable tools for reconstructing past SST variability. Coastal deposits on Bonaire provide abundant fossil D. strigosa colonies of Holocene age that can be accurately dated and used to reconstruct climate variability. Comparisons of long monthly resolved Sr/Ca records from multiple fossil corals will provide a mean to estimate seasonality and interannual to interdecadal SST variability of the Southern Caribbean Sea during the Holocene.
    Schlagwort(e): BON-6-A; Calculated, see reference(s); CaribClim_Coral_2006; Center for Marine Environmental Sciences; Diploria strigosa, Strontium/Calcium ratio; DRILL; Drilling/drill rig; ICP-OES, Perkin-Elmer, Optima 3300R; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; Internal coral chronology; MARUM; Southern Caribbean Sea, Bonaire
    Materialart: Dataset
    Format: text/tab-separated-values, 960 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 13
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    Raw data from 4.27 ka Bonaire coral, sample BON-4-G (2011)
    PANGAEA
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): Attributed to extreme Sr/Ca values of any single year; BON-4-G; CaribClim_Coral_2006; Center for Marine Environmental Sciences; Diploria strigosa, Strontium/Calcium ratio; Diploria strigosa, δ18O; DISTANCE; DRILL; Drilling/drill rig; Estimated based on subannual extension-rate and tie points; ICP-OES, Perkin-Elmer, Optima 3300R; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; Internal coral chronology; MARUM; Mass spectrometer Finnigan MAT 251; referred samples; Sample ID; Southern Caribbean Sea, Bonaire; Tie point
    Materialart: Dataset
    Format: text/tab-separated-values, 1069 data points
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  • 14
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    Simulated climatically disturbed emergence of agricultures in Western Eurasia 8500-3000 BC (2014)
    PANGAEA
    In:  Supplement to: Lemmen, Carsten; Wirtz, Kai W (2014): On the sensitivity of the simulated European Neolithic transition to climate extremes. Journal of Archaeological Science, 51, 65-72, https://doi.org/10.1016/j.jas.2012.10.023
    Details
    Publikationsdatum: 2024-05-31
    Beschreibung: Was the spread of agropastoralism from the Fertile Crescent throughout Europe influenced by rapid climatic shifts? We here generate idealized climate events using palaeoclimate records. In a mathematical model of regional sociocultural development, these events disturb the subsistence base of simulated forager and farmer societies. We evaluate the regional simulated transition timings and durations against a published large set of radiocarbon dates for western Eurasia; the model is able to realistically hindcast much of the inhomogeneous space-time evolution of regional Neolithic transitions. Our study shows that the inclusion of climate events improves the simulation of typical lags between cultural complexes, but that the overall difference to a model without climate events is not significant. Climate events may not have been as important for early sociocultural dynamics as endogenous factors.
    Schlagwort(e): GLUES_LBK; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; Model; Model version 1.1.18; western Eurasia
    Materialart: Dataset
    Format: application/x-gzip, 681.8 kBytes
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  • 15
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    Reference list of 265 sources used for the discovery of relationships between data clusters and metadata properties (2012)
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    Details
    Publikationsdatum: 2024-05-31
    Beschreibung: Visual cluster analysis provides valuable tools that help analysts to understand large data sets in terms of representative clusters and relationships thereof. Often, the found clusters are to be understood in context of belonging categorical, numerical or textual metadata which are given for the data elements. While often not part of the clustering process, such metadata play an important role and need to be considered during the interactive cluster exploration process. Traditionally, linked-views allow to relate (or loosely speaking: correlate) clusters with metadata or other properties of the underlying cluster data. Manually inspecting the distribution of metadata for each cluster in a linked-view approach is tedious, specially for large data sets, where a large search problem arises. Fully interactive search for potentially useful or interesting cluster to metadata relationships may constitute a cumbersome and long process. To remedy this problem, we propose a novel approach for guiding users in discovering interesting relationships between clusters and associated metadata. Its goal is to guide the analyst through the potentially huge search space. We focus in our work on metadata of categorical type, which can be summarized for a cluster in form of a histogram. We start from a given visual cluster representation, and compute certain measures of interestingness defined on the distribution of metadata categories for the clusters. These measures are used to automatically score and rank the clusters for potential interestingness regarding the distribution of categorical metadata. Identified interesting relationships are highlighted in the visual cluster representation for easy inspection by the user. We present a system implementing an encompassing, yet extensible, set of interestingness scores for categorical metadata, which can also be extended to numerical metadata. Appropriate visual representations are provided for showing the visual correlations, as well as the calculated ranking scores. Focusing on clusters of time series data, we test our approach on a large real-world data set of time-oriented scientific research data, demonstrating how specific interesting views are automatically identified, supporting the analyst discovering interesting and visually understandable relationships.
    Schlagwort(e): Alaska, USA; Antarctica; Australia; AWIPEV; AWIPEV_based; BAR; Barrow; BER; Bermuda; BOU; Boulder; Brasilia; Brasilia City, Distrito Federal, Brazil; Brazil; BRB; CAB; Cabauw; Canada; CAR; Carpentras; Chesapeake Light; CLH; Colorado, United States of America; Cosmonauts Sea; DAR; Darwin; Dronning Maud Land, Antarctica; E13; France; Georg von Neumayer; Germany; GVN; Israel; Japan; KWA; Kwajalein; LIN; Lindenberg; MAN; Momote; Monitoring station; MONS; NAU; Nauru; Nauru Island; Neumayer_based; NEUMAYER III; North Pacific Ocean; NYA; Ny-Ålesund; Ny-Ålesund, Spitsbergen; Oklahoma, United States of America; PAL; Palaiseau, SIRTA Observatory; Papua New Guinea; PAY; Payerne; Petrolina; PTR; REG; Regina; São Martinho da Serra; SBO; Sede Boqer; SMS; South Atlantic Ocean; Southern Great Plains; South Pole; SPO; Switzerland; SYO; Syowa; TAT; Tateno; The Netherlands
    Materialart: Dataset
    Format: 265 datasets
    Standort Signatur Erwartet Verfügbarkeit
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  • 16
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    Basic and other measurements of radiation at station Tateno (TAT), reference list of 233 datasets (1996-02 to 2015-06) (2019)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): Baseline Surface Radiation Network; BSRN
    Materialart: Dataset
    Format: 233 datasets
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  • 17
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    Station list and links to master tracks in different resolutions of POLARSTERN cruise ARK-XVII/2, Tromsø - Bremerhaven, 2001-07-31 - 2001-10-07 (2015)
    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): ARK-XVII/2; Calculated; Course; CT; DATE/TIME; LATITUDE; LONGITUDE; Polarstern; PS59/2-track; PS59 AMORE; Speed; Underway cruise track measurements
    Materialart: Dataset
    Format: text/tab-separated-values, 19834 data points
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  • 18
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    Diatom assemblages in surface sediments from southern Drake Passage and the Bransfield Strait, Antarctic Peninsula, sampled during POLARSTERN cruise PS97 (ANT-XXXI/3) (2019)
    PANGAEA
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): ANT-XXXI/3; Azpeitia tabularis; Bransfield Strait; Counting, diatoms; DEPTH, sediment/rock; Diatoms, sea ice; Drake Passage; Eucampia antarctica; Event label; Fragilariopsis curta; Fragilariopsis cylindrus; Fragilariopsis kerguelensis; Fragilariopsis obliquecostata; Fragilariopsis sublinearis; Fragilariopsis vanheurckii; Modern analog technique (MAT), D274/28/4an; MUC; MultiCorer; Navicula directa; Odontella weissflogii; Polarstern; Porosira pseudodenticulata; PS97; PS97/042-1; PS97/046-6; PS97/048-1; PS97/049-2; PS97/052-3; PS97/053-1; PS97/054-2; PS97/056-1; PS97/068-2; PS97/069-1; PS97/072-2; PS97/073-2; PS97/074-1; PS97/077-1; PS97/079-1; PS97/080-2; Pseudo-nitzschia lineola-turgiduloides group; Rhizosolenia alata; Rhizosolenia hebetata forma semispina; Scotia Sea; Stellarima microtrias; Stephanopyxis sp.; Thalassiosira antarctica; Thalassiosira lentiginosa; Thalassiosira oliverana
    Materialart: Dataset
    Format: text/tab-separated-values, 320 data points
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  • 19
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    Stable isotope and geochemical analyses of sediment core SO164-17-2 from the southern Florida Straits (2011)
    PANGAEA
    In:  Supplement to: Bahr, André; Nürnberg, Dirk; Schönfeld, Joachim; Garbe-Schönberg, Dieter (2011): Hydrological variability in Florida Straits during marine isotope stage 5 cold events. Paleoceanography, 26, PA2214, https://doi.org/10.1029/2010PA002015
    Details
    Publikationsdatum: 2024-05-31
    Beschreibung: Modeling and proxy studies indicate that a reduction of Atlantic Meridional Overturning Circulation (AMOC) strength profoundly impacts temperatures and salinities in the (sub)tropical Atlantic, especially on subsurface levels. While previous studies focused on prominent periods of AMOC reduction during the last deglaciation, we aim to test whether similar reconfigurations of the subtropical hydrography occurred during the moderate climatic alterations punctuating the last interglacial, Marine Isotope Stage (MIS) 5. Here, we present temperature and salinity records from a Florida Straits core by combining d18O and Mg/Ca analyses on surface (Globigerinoides ruber, white) and deep-dwelling (Globorotalia crassaformis) foraminifera, covering MIS 5 in high resolution. The data reveal increasing salinities at intermediate depths during interglacial cooling episodes, decoupled from relatively stable surface conditions. This probably indicates the spatial expansion of saline Subtropical Gyre waters due to enhanced Ekman downwelling and might also point to a changed density structure and altered geostrophic balance in Florida Straits. Notably, these oceanographic alterations are not consistently occurring during periods of AMOC reduction. The data suggest that the expansion of gyre waters into Florida Straits was impeded by the increasing influence of Antarctic Intermediate Water (AAIW) from MIS 5.5 to ~107 kyr BP. Afterwards, increasingly positive benthic d13C values imply a recession of AAIW, allowing the temporary expansion of Gyre waters into Florida Straits. We argue that the inferred transient subtropical salt accumulation and warm pool expansion might have played a pivotal role in reinvigorating meridional overturning and dampen the severity of interglacial cold phases.
    Schlagwort(e): Florida Strait; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; PC; Piston corer; RASTA/GOLDFLOS; SO164; SO164-17-2; Sonne
    Materialart: Dataset
    Format: application/zip, 5 datasets
    Standort Signatur Erwartet Verfügbarkeit
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  • 20
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    Planktonic foraminiferal (Globigerinoides ruber) Mg/Ca ratios and SSTs of sediment cores GeoB9501-4 and GeoB9501-5 (2011)
    PANGAEA
    Details
    Publikationsdatum: 2024-05-31
    Beschreibung: Multidecadal variations in Atlantic sea surface temperatures (SST) influence the climate of the Northern Hemisphere. However, prior to the instrumental time period, information on multidecadal climate variability becomes limited, and there is a particular scarcity of sufficiently resolved SST reconstructions. Here, we present an eastern tropical North Atlantic reconstruction of SSTs based on foraminiferal (Globigerinoides ruber pink) Mg/Ca ratios that resolves multidecadal variability over the past 1700 years. Spectral power in the multidecadal band (50 to 70 years period) is significant over several time intervals suggesting that the Atlantic Multidecadal Oscillation (AMO) has been influencing local SST. Since our data exhibit high scatter the absence of multidecadal variability in the remaining record does not exclude the possibility that SST variations on this time scale might have been present without being detected in our data. Cooling by ~0.5 °C takes place between about AD 1250 and AD 1500; while this corresponds to the inception of the Little Ice Age (LIA), the end of the LIA is not reflected in our record and SST remains relatively low. This transition to cooler SSTs parallels the previously reconstructed shift in the North Atlantic Oscillation towards a low pre-20th century mean state and possibly reflects common solar forcing.
    Schlagwort(e): 286; Center for Marine Environmental Sciences; GeoB9501-4; GeoB9501-5; Gravity corer (Kiel type); Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; M65/1; MARUM; Mauritania Canyon; Meteor (1986); MUC; MultiCorer; SL
    Materialart: Dataset
    Format: application/zip, 2 datasets
    Standort Signatur Erwartet Verfügbarkeit
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  • 21
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    Age model, raw data and interpolated raw data from proxy records of sediment cores GeoB6007-1 and GeoB6007-2 (2011)
    PANGAEA
    Details
    Publikationsdatum: 2024-05-31
    Beschreibung: Here we present a 1200 yr long benthic foraminiferal Mg/Ca based temperature and oxygen isotope record from a ~900 m deep sediment core off northwest Africa to show that atmosphere-ocean interactions in the eastern subpolar gyre are transferred at central water depth into the eastern boundary of the subtropical gyre. Further we link the variability of the NAO (over the past 165 yrs) and solar irradiance (Late Holocene) and their control on subpolar mode water formation to the multidecadal variability observed at mid-depth in the eastern subtropical gyre. Our results show that eastern North Atlantic central waters cooled by up to ~0.8± 0.7 °C and densities decreased by Sigma theta=0.3±0.2 during positive NAO years and during minima in solar irradiance during the Late Holocene. The presented records demonstrate the sensitivity of central water formation to enhanced atmospheric forcing and ice/freshwater fluxes into the eastern subpolar gyre and the importance of central water circulation for cross-gyre climate signal propagation during the Late Holocene.
    Schlagwort(e): Center for Marine Environmental Sciences; GeoB6007-1; GeoB6007-2; Gravity corer (Kiel type); Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; M45/5a; MARUM; Meteor (1986); MUC; MultiCorer; SL
    Materialart: Dataset
    Format: application/zip, 3 datasets
    Standort Signatur Erwartet Verfügbarkeit
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  • 22
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    Unbekannt
    Coral Sr/Ca records from Bonaire Holocene corals (2012)
    PANGAEA
    In:  Supplement to: Giry, Cyril; Felis, Thomas; Kölling, Martin; Scholz, Denis; Wei, Wei; Lohmann, Gerrit; Scheffers, Sander R (2012): Mid- to late Holocene changes in tropical Atlantic temperature seasonality and interannual to multidecadal variability documented in southern Caribbean corals. Earth and Planetary Science Letters, 331-332, 187–200, https://doi.org/10.1016/j.epsl.2012.03.019
    Details
    Publikationsdatum: 2024-05-31
    Beschreibung: Proxy reconstructions of tropical Atlantic sea surface temperature (SST) that extend beyond the period of instrumental observations have primarily focused on centennial to millennial variability rather than on seasonal to multidecadal variability. Here we present monthly-resolved records of Sr/Ca (a proxy of SST) from fossil annually-banded Diploria strigosa corals from Bonaire (southern Caribbean Sea). The individual corals provide time-windows of up to 68 years length, and the total number of 295 years of record allows for assessing the natural range of seasonal to multidecadal SST variability in the western tropical Atlantic during snapshots of the mid- to late Holocene. Comparable to modern climate, the coral Sr/Ca records reveal that mid- to late Holocene SST was characterised by clear seasonal cycles, persistent quasi-biennial and prominent interannual as well as inter- to multidecadal-scale variability. However, the magnitude of SST variations on these timescales has varied over the last 6.2 ka. The coral records show increased seasonality during the mid-Holocene consistent with climate model simulations indicating that southern Caribbean SST seasonality is induced by insolation changes on orbital timescales, whereas internal dynamics of the climate system play an important role on shorter timescales. Interannual SST variability is linked to ocean-atmosphere interactions of Atlantic and Pacific origin. Pronounced interannual variability in the western tropical Atlantic is indicated by a 2.35 ka coral, possibly related to a strengthening of the variability of the El Niño/Southern Oscillation throughout the Holocene. Prominent inter- to multidecadal SST variability is evident in the coral records and slightly more pronounced in the mid-Holocene. We finally argue that our coral data provide a target for studying Holocene climate variability on seasonal and interannual to multidecadal timescales, when using further numerical models and high-resolution proxy data.
    Schlagwort(e): BON-0-A; BON-20-A; BON-3-E; BON-4-G; BON-6-A; BON-7-A; BON-7-B; BON-9-A; BON-9-B; CaribClim_Coral_2006; CaribClim_Coral_Jan 2009; Center for Marine Environmental Sciences; DRILL; Drilling/drill rig; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; MARUM; Southern Caribbean Sea, Bonaire
    Materialart: Dataset
    Format: application/zip, 13 datasets
    Standort Signatur Erwartet Verfügbarkeit
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  • 23
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    Age determination, planktic foraminifera and stable istopes of sediment core MSM05/5_712-2 (2013)
    PANGAEA
    In:  Supplement to: Werner, Kirstin; Spielhagen, Robert F; Bauch, Dorothea; Hass, H Christian; Kandiano, Evgenia S (2013): Atlantic Water advection versus sea-ice advances in the eastern Fram Strait during the last 9 ka: Multiproxy evidence for a two-phase Holocene. Paleoceanography, 28(2), 283-295, https://doi.org/10.1002/palo.20028
    Details
    Publikationsdatum: 2024-05-31
    Beschreibung: A sediment core from the West Spitsbergen continental margin was studied to reconstruct climate and paleoceanographic variability during the last ~9 ka in the eastern Fram Strait. Our multiproxy evidence suggests that the establishment of the modern oceanographic configuration in the eastern Fram Strait occurred stepwise, in response to the postglacial sea-level rise and the related onset of modern sea-ice production on the shallow Siberian shelves. The late Early and Mid Holocene interval (9 to 5 ka) was generally characterized by relatively unstable conditions. High abundance of the subpolar planktic foraminifer species Turborotalita quinqueloba implies strong intensity of Atlantic Water (AW) inflow with high productivity and/or high AW temperatures, resulting in a strong heat flux to the Arctic. A series of short-lived cooling events (8.2, 6.9. and 6.1 ka) occurred superimposed on the warm late Early and Mid Holocene conditions. Our proxy data imply that simultaneous to the complete postglacial flooding of Arctic shallow shelves and the initiation of modern sea-ice production, strong advance of polar waters initiated modern oceanographic conditions in the eastern Fram Strait at ~5.2 ka. The Late Holocene was marked by the dominance of the polar planktic foraminifer species Neogloboquadrina pachyderma, a significant expansion of sea ice/icebergs, and strong stratification of the water column. Although planktic foraminiferal assemblages as well as sea surface and subsurface temperatures suggest a return of slightly strengthened advection of subsurface Atlantic Water after 3 ka, a relatively stable cold-water layer prevailed at the sea surface and the study site was probably located within the seasonally fluctuating marginal ice zone during the Neoglacial period.
    Schlagwort(e): Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK
    Materialart: Dataset
    Format: application/zip, 7 datasets
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  • 24
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    Monthly interpolated coral δ¹⁸O records from Bonaire corals (2013)
    PANGAEA
    In:  Supplement to: Giry, Cyril; Felis, Thomas; Kölling, Martin; Wei, Wei; Lohmann, Gerrit; Scheffers, Sander R (2013): Controls of Caribbean surface hydrology during the mid- to late Holocene: insights from monthly resolved coral records. Climate of the Past, 9, 841-858, https://doi.org/10.5194/cp-9-841-2013
    Details
    Publikationsdatum: 2024-05-31
    Beschreibung: Several proxy-based and modeling studies have investigated long-term changes in Caribbean climate during the Holocene, however, very little is known on its variability on short timescales. Here we reconstruct seasonality and interannual to multidecadal variability of sea surface hydrology of the southern Caribbean Sea by applying paired coral Sr/Ca and d18O measurements on fossil annually banded Diploria strigosa corals from Bonaire. This allows for better understanding of seasonal to multidecadal variability of the Caribbean hydrological cycle during the mid- to late Holocene. The monthly resolved coral Delta d18O records are used as a proxy for the oxygen isotopic composition of seawater (d18Osw) of the southern Caribbean Sea. Consistent with modern day conditions, annual d18Osw cycles reconstructed from three modern corals reveal that freshwater budget at the study site is influenced by both net precipitation and advection of tropical freshwater brought by wind-driven surface currents. In contrast, the annual d18Osw cycle reconstructed from a mid-Holocene coral indicates a sharp peak towards more negative values in summer, suggesting intense summer precipitation at 6 ka BP (before present). In line with this, our model simulations indicate that increased seasonality of the hydrological cycle at 6 ka BP results from enhanced precipitation in summertime. On interannual to multidecadal timescales, the systematic positive correlation observed between reconstructed sea surface temperature and salinity suggests that freshwater discharged from the Orinoco and Amazon rivers and transported into the Caribbean by wind-driven surface currents is a critical component influencing sea surface hydrology on these timescales.
    Schlagwort(e): Center for Marine Environmental Sciences; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; MARUM
    Materialart: Dataset
    Format: application/zip, 9 datasets
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  • 25
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    Unbekannt
    Modelled global ocean temperature from 6 ka to present (2013)
    PANGAEA
    In:  Supplement to: Lohmann, Gerrit; Pfeiffer, Madlene; Laepple, Thomas; Leduc, Guillaume; Kim, Jung-Hyun (2013): A model-data comparison of the Holocene global sea surface temperature evolution. Climate of the Past, 9(4), 1807-1839, https://doi.org/10.5194/cp-9-1807-2013
    Details
    Publikationsdatum: 2024-05-31
    Beschreibung: We compare the ocean temperature evolution of the Holocene as simulated by climate models and reconstructed from marine temperature proxies. This site provides informations about the Holocene temperature trends as simulated by the models. We use transient simulations from a coupled atmosphere-ocean general circulation model, as well as an ensemble of time slice simulations from the Paleoclimate Modelling Intercomparison Project. The general pattern of sea surface temperature (SST) in the models shows a high latitude cooling and a low latitude warming. The proxy dataset comprises a global compilation of marine alkenone- and Mg/Ca-derived SST estimates. Independently of the choice of the climate model, we observe significant mismatches between modelled and estimated SST amplitudes in the trends for the last 6000 years. Alkenone-based SST records show a similar pattern as the simulated annual mean SSTs, but the simulated SST trends underestimate the alkenone-based SST trends by a factor of two to five. For Mg/Ca, no significant relationship between model simulations and proxy reconstructions can be detected. We tested if such discrepancies can be caused by too simplistic interpretations of the proxy data. We tested different seasons and depths in the model to compare the proxy data trends, and can reconcile only part of the mismatches on a regional scale. We therefore considered the additional environmental factor changes in the planktonic organisms' habitat depth and a time-shift in the recording season to diagnose whether invoking those environmental factors can help reconciling the proxy records and the model simulations. We find that invoking shifts in the living season and habitat depth can remove some of the model-data discrepancies in SST trends. Regardless whether such adjustments in the environmental parameters during the Holocene are realistic, they indicate that when modeled temperature trends are set up to allow drastic shifts in the ecological behavior of planktonic organisms, they do not capture the full range of reconstructed SST trends. Our findings indicate that climate model and reconstructed temperature trends are to a large degree only qualitatively comparable, thus providing a challenge for the interpretation of proxy data as well as the models' sensitivity to orbital forcing.
    Schlagwort(e): Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK
    Materialart: Dataset
    Format: application/zip, 3 datasets
    Standort Signatur Erwartet Verfügbarkeit
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  • 26
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    A reconstruction of atmospheric carbon dioxide and its stable carbon isotopic composition from the penultimate glacial maximum to the glacial inception (2013)
    PANGAEA
    In:  Supplement to: Schneider, Robert; Schmitt, Jochen; Koehler, Peter; Joos, Fortunat; Fischer, Hubertus (2013): A reconstruction of atmospheric carbon dioxide and its stable carbon isotopic composition from the penultimate glacial maximum to the glacial inception. Climate of the Past, 9(6), 2507-2523, https://doi.org/10.5194/cp-9-2507-2013
    Details
    Publikationsdatum: 2024-05-31
    Beschreibung: The reconstruction of the stable carbon isotope evolution in atmospheric CO2 (d13Catm ), as archived in Antarctic ice cores, bears the potential to disentangle the contributions of the different carbon cycle fluxes causing past CO2 variations. Here we present a new record of d13Catm before, during and after the Marine Isotope Stage 5.5 (155 000 to 105 000 years BP). The record was derived with a well established sublimation method using ice from the EPICA Dome C (EDC) and the Talos Dome ice cores in East Antarctica. We find a 0.4 permil shift to heavier values between the mean d13Catm level in the Penultimate (~ 140 000 years BP) and Last Glacial Maximum (~ 22 000 years BP), which can be explained by either (i) changes in the isotopic composition or (ii) intensity of the carbon input fluxes to the combined ocean/atmosphere carbon reservoir or (iii) by long-term peat buildup. Our isotopic data suggest that the carbon cycle evolution along Termination II and the subsequent interglacial was controlled by essentially the same processes as during the last 24 000 years, but with different phasing and magnitudes. Furthermore, a 5000 years lag in the CO2 decline relative to EDC temperatures is confirmed during the glacial inception at the end of MIS 5.5 (120 000 years BP). Based on our isotopic data this lag can be explained by terrestrial carbon release and carbonate compensation.
    Schlagwort(e): EPICA; European Project for Ice Coring in Antarctica; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK
    Materialart: Dataset
    Format: application/zip, 2 datasets
    Standort Signatur Erwartet Verfügbarkeit
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  • 27
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    Unbekannt
    Sea surface temperatures during Marine Isotope Stage (MIS) 11 (2013)
    PANGAEA
    In:  Supplement to: Milker, Yvonne; Rachmayani, Rima; Weinkauf, Manuel F G; Prange, Matthias; Raitzsch, Markus; Schulz, Michael; Kucera, Michal (2013): Global and regional sea surface temperature trends during Marine Isotope Stage 11. Climate of the Past, 9(5), 2231-2252, https://doi.org/10.5194/cp-9-2231-2013
    Details
    Publikationsdatum: 2024-05-31
    Beschreibung: The Marine Isotope Stage (MIS) 11 (424-374 ka) was characterized by a protracted deglaciation and an unusually long climatic optimum. It remains unclear to what degree the climate development during this interglacial reflects the unusually weak orbital forcing or greenhouse gas trends. Previously, arguments about the duration and timing of the MIS11 climatic optimum and about the pace of the deglacial warming were based on a small number of key records, which appear to show regional differences. In order to obtain a global signal of climate evolution during MIS11, we compiled a database of 78 sea surface temperature (SST) records from 57 sites spanning MIS11, aligned these individually on the basis of benthic (N = 28) or planktonic (N = 31) stable oxygen isotope curves to a common time frame and subjected 48 of them to an empirical orthogonal function (EOF) analysis. The analysis revealed a high commonality among all records, with the principal SST trend explaining almost 49% of the variability. This trend indicates that on the global scale, the surface ocean underwent rapid deglacial warming during Termination V, in pace with carbon dioxide rise, followed by a broad SST optimum centered at ~410 kyr. The second EOF, which explained ~18% of the variability, revealed the existence of a different SST trend, characterized by a delayed onset of the temperature optimum during MIS11 at ~398 kyr, followed by a prolonged warm period lasting beyond 380 kyr. This trend is most consistently manifested in the mid-latitude North Atlantic and Mediterranean Sea and is here attributed to the strength of the Atlantic meridional overturning circulation. A sensitivity analysis indicates that these results are robust to record selection and to age-model uncertainties of up to 3-6 kyr, but more sensitive to SST seasonal attribution and SST uncertainties 〉1 °C. In order to validate the CCSM3 (Community Climate System Model, version 3) predictive potential, the annual and seasonal SST anomalies recorded in a total of 74 proxy records were compared with runs for three time slices representing orbital configuration extremes during the peak interglacial of MIS11. The modeled SST anomalies are characterized by a significantly lower variance compared to the reconstructions. Nevertheless, significant correlations between proxy and model data are found in comparisons on the seasonal basis, indicating that the model captures part of the long-term variability induced by astronomical forcing, which appears to have left a detectable signature in SST trends.
    Schlagwort(e): Center for Marine Environmental Sciences; Deep Sea Drilling Project; DSDP; GeoB; Geosciences, University of Bremen; Integrated Ocean Drilling Program / International Ocean Discovery Program; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; IODP; MARUM; Ocean Drilling Program; ODP
    Materialart: Dataset
    Format: application/zip, 3 datasets
    Standort Signatur Erwartet Verfügbarkeit
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  • 28
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    Age model, stable isotopes, major element proportions and endmember unmixing results from four western tropical Atlantic cores (2014)
    PANGAEA
    In:  Supplement to: Govin, Aline; Chiessi, Cristiano Mazur; Zabel, Matthias; Sawakuchi, André Oliveira; Heslop, David; Hörner, Tanja; Zhang, Yancheng; Mulitza, Stefan (2014): Terrigenous input off northern South America driven by changes in Amazonian climate and the North Brazil Current retroflection during the last 250 ka. Climate of the Past, 10, 843-862, https://doi.org/10.5194/cp-10-843-2014
    Details
    Publikationsdatum: 2024-05-31
    Beschreibung: We investigate changes in the delivery and oceanic transport of Amazon sediments related to terrestrial climate variations over the last 250 ka. We present high-resolution geochemical records from four marine sediment cores located between 5 and 12° N along the northern South American margin. The Amazon River is the sole source of terrigenous material for sites at 5 and 9° N, while the core at 12° N receives a mixture of Amazon and Orinoco detrital particles. Using an endmember unmixing model, we estimated the relative proportions of Amazon Andean material ("%-Andes", at 5 and 9° N) and of Amazon material ("%-Amazon", at 12° N) within the terrigenous fraction. The %-Andes and %-Amazon records exhibit significant precessional variations over the last 250 ka that are more pronounced during interglacials in comparison to glacial periods. High %-Andes values observed during periods of high austral summer insolation reflect the increased delivery of suspended sediments by Andean tributaries and enhanced Amazonian precipitation, in agreement with western Amazonian speleothem records. Increased Amazonian rainfall reflects the intensification of the South American monsoon in response to enhanced land-ocean thermal gradient and moisture convergence. However, low %-Amazon values obtained at 12° N during the same periods seem to contradict the increased delivery of Amazon sediments. We propose that reorganizations in surface ocean currents modulate the northwestward transport of Amazon material. In agreement with published records, the seasonal North Brazil Current retroflection is intensified (or prolonged in duration) during cold substages of the last 250 ka (which correspond to intervals of high DJF or low JJA insolation) and deflects eastward the Amazon sediment and freshwater plume.
    Schlagwort(e): Center for Marine Environmental Sciences; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; MARUM
    Materialart: Dataset
    Format: application/zip, 19 datasets
    Standort Signatur Erwartet Verfügbarkeit
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  • 29
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    (Supplementary Table 1) 230Th/U results for stalagmite Cuba Grande (CG) from Pinar del Rio (2010)
    PANGAEA
    In:  Supplement to: Fensterer, Claudia; Scholz, Denis; Hoffmann, Dirk L; Mangini, Augusto; Pajon, Jesus M (2010): 230Th/U-dating of a late Holocene low uranium speleothem from Cuba. IOP Conference Series: Earth and Environmental Science, 9(1), 012015, https://doi.org/10.1088/1755-1315/9/1/012015
    Details
    Publikationsdatum: 2024-05-31
    Beschreibung: We present 22 U-series ages for a stalagmite from north-western Cuba based on multi-collector inductively coupled plasma mass spectrometry (MC-ICPMS) and thermal ionisation mass spectrometry (TIMS). Our results reveal that the stalagmite continuously grew within the last ~1400a. Low uranium content of the sample and thus, extremely low 230Th concentrations limit the precision and accuracy of 230Th/U-dating by TIMS. Samples measured by MC-ICPMS show a high variability of 232Th content along the growth axis with some sections significantly affected by initial 230Th from a detrital phase. An a-priori bulk earth ratio for (238U/232Th) cannot be used to accurately account for this initial 230Th. Using an age model based on the 230Th/U ages determined on samples with low or negligible 232Th concentration, we find that the (238U/232Th) activity ratio of the detrital phase is an order of magnitude larger than the bulk earth value, indicating the importance of an accurately determined correction factor.
    Schlagwort(e): Age, comment; Age, dated; Age, dated standard deviation; CG; Cuba_Grande; DISTANCE; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; Multi-collector inductively coupled plasma mass spectrometer (MC-ICP-MS); Pinar del Rio (NW Cuba); Speleothem sample; SPS; Thorium-230/Thorium-232 activity ratio; Thorium-230/Thorium-232 activity ratio, standard deviation; Thorium-230/Uranium-238 activity ratio, standard deviation; Thorium-230/Uranium-238 ratio; Thorium-232; Thorium-232, standard deviation; Uranium-234, standard deviation; Uranium-234/Uranium-238 activity ratio; Uranium-238; Uranium-238, standard deviation
    Materialart: Dataset
    Format: text/tab-separated-values, 351 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 30
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    Three time-slice simulations of the Eemian (eem), the mid-Holocene (hol), and a pre-industrial (pri) control run with the coupled atmosphere-ocean-model ECHAM5/MPI-OM (2010)
    PANGAEA
    In:  Supplement to: Fischer, Nils; Jungclaus, Johann H (2010): Effects of orbital forcing on atmosphere and ocean heat transports in Holocene and Eemian climate simulations with a comprehensive Earth system model. Climate of the Past, 6, 155-168, https://doi.org/10.5194/cp-6-155-2010
    Details
    Publikationsdatum: 2024-05-31
    Beschreibung: Orbital forcing does not only exert direct insolation effects, but also alters climate indirectly through feedback mechanisms that modify atmosphere and ocean dynamics and meridional heat and moisture transfers. We investigate the regional effects of these changes by detailed analysis of atmosphere and ocean circulation and heat transports in a coupled atmosphere-ocean-sea ice-biosphere general circulation model (ECHAM5/JSBACH/MPI-OM). We perform long term quasi equilibrium simulations under pre-industrial, mid-Holocene (6000 years before present – yBP), and Eemian (125 000 yBP) orbital boundary conditions. Compared to pre-industrial climate, Eemian and Holocene temperatures show generally warmer conditions at higher and cooler conditions at lower latitudes. Changes in sea-ice cover, ocean heat transports, and atmospheric circulation patterns lead to pronounced regional heterogeneity. Over Europe, the warming is most pronounced over the north-eastern part in accordance with recent reconstructions for the Holocene. We attribute this warming to enhanced ocean circulation in the Nordic Seas and enhanced ocean-atmosphere heat flux over the Barents Shelf in conduction with retreat of sea ice and intensified winter storm tracks over northern Europe.
    Schlagwort(e): Abbreviation; Experiment; File format; File name; File size; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; Parameter; Uniform resource locator/link to model result file; Unit
    Materialart: Dataset
    Format: text/tab-separated-values, 100 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 31
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    Regional ocean model for the Mediterranean, links to model files (2011)
    PANGAEA
    In:  Supplement to: Mikolajewicz, Uwe (2011): Modeling Mediterranean Ocean climate of the Last Glacial Maximum. Climate of the Past, 7, 161-180, https://doi.org/10.5194/cp-7-161-2011
    Details
    Publikationsdatum: 2024-05-31
    Beschreibung: A regional ocean general circulation model of the Mediterranean is used to study the climate of the Last Glacial Maximum. The atmospheric forcing for these simulations has been derived from simulations with an atmospheric general circulation model, which in turn was forced with surface conditions from a coarse resolution earth system model. The model is successful in reproducing the general patterns of reconstructed sea surface temperature anomalies with the strongest cooling in summer in the northwestern Mediterranean and weak cooling in the Levantine, although the model underestimates the extent of the summer cooling in the western Mediterranean. However, there is a strong vertical gradient associated with this pattern of summer cooling, which makes the comparison with reconstructions complicated. The exchange with the Atlantic is decreased to roughly one half of its present value, which can be explained by the shallower Strait of Gibraltar as a consequence of lower global sea level. This reduced exchange causes a strong increase of salinity in the Mediterranean in spite of reduced net evaporation.
    Schlagwort(e): Experiment; File format; File name; File size; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; Parameter; Uniform resource locator/link to model result file; Unit
    Materialart: Dataset
    Format: text/tab-separated-values, 56 data points
    Standort Signatur Erwartet Verfügbarkeit
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    DATEN PANGAEA
  • 32
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    Holocene precipitation change in different monsoon sub-regions (time-slices and transient data) simulated by different global climate models, with links to model results (2014)
    PANGAEA
    In:  Supplement to: Dallmeyer, Anne; Claussen, Martin; Fischer, Nils; Haberkorn, Kerstin; Wagner, Sebastian; Pfeiffer, Madlene; Jin, Liya; Khon, Vyacheslav; Wang, Yujie; Herzschuh, Ulrike (2015): The evolution of sub-monsoon systems in the Afro-Asian monsoon region during the Holocene– comparison of different transient climate model simulations. Climate of the Past, 11(2), 305-326, https://doi.org/10.5194/cp-11-305-2015
    Details
    Publikationsdatum: 2024-05-31
    Beschreibung: The recently proposed global monsoon hypothesis interprets monsoon systems as part of one global-scale atmospheric overturning circulation, implying a connection between the regional monsoon systems and an in-phase behaviour of all northern hemispheric monsoons on annual timescales (Trenberth et al., 2000). Whether this concept can be applied to past climates and variability on longer timescales is still under debate, because the monsoon systems exhibit different regional characteristics such as different seasonality (i.e. onset, peak, and withdrawal). To investigate the interconnection of different monsoon systems during the pre-industrial Holocene, five transient global climate model simulations have been analysed with respect to the rainfall trend and variability in different sub-domains of the Afro-Asian monsoon region. Our analysis suggests that on millennial timescales with varying orbital forcing, the monsoons do not behave as a tightly connected global system. According to the models, the Indian and North African monsoons are coupled, showing similar rainfall trend and moderate correlation in rainfall variability in all models. The East Asian monsoon changes independently during the Holocene. The dissimilarities in the seasonality of the monsoon sub-systems lead to a stronger response of the North African and Indian monsoon systems to the Holocene insolation forcing than of the East Asian monsoon and affect the seasonal distribution of Holocene rainfall variations. Within the Indian and North African monsoon domain, precipitation solely changes during the summer months, showing a decreasing Holocene precipitation trend. In the East Asian monsoon region, the precipitation signal is determined by an increasing precipitation trend during spring and a decreasing precipitation change during summer, partly balancing each other. A synthesis of reconstructions and the model results do not reveal an impact of the different seasonality on the timing of the Holocene rainfall optimum in the different sub-monsoon systems. They rather indicate locally inhomogeneous rainfall changes and show, that single palaeo-records should not be used to characterise the rainfall change and monsoon evolution for entire monsoon sub-systems.
    Schlagwort(e): Comment; File content; File format; File name; File size; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; Reference of data; Uniform resource locator/link to file
    Materialart: Dataset
    Format: text/tab-separated-values, 76 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 33
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    Model output of the Greenland Ice Sheet to interglacial climate forcing: MIS 5e versus MIS 11 (2017)
    PANGAEA
    In:  Supplement to: Rachmayani, Rima; Prange, Matthias; Lunt, Daniel J; Stone, Emma J; Schulz, Michael (2017): Sensitivity of the Greenland Ice Sheet to Interglacial Climate Forcing: MIS 5e Versus MIS 11. Paleoceanography, 32(11), 1089-1101, https://doi.org/10.1002/2017PA003149
    Details
    Publikationsdatum: 2024-05-31
    Beschreibung: The Greenland Ice Sheet (GrIS) is thought to have contributed substantially to high global sea levels during the interglacials of Marine Isotope Stage (MIS) 5e and 11. Geological evidence suggests that the mass loss of the GrIS was greater during the peak interglacial of MIS 11 than MIS 5e, despite a weaker boreal summer insolation. We address this conundrum by using the three-dimensional thermomechanical ice-sheet model Glimmer forced by CCSM3 climate model output for MIS 5e and MIS 11 interglacial time slices. Our results suggest a stronger sensitivity of the GrIS to MIS 11 climate forcing than to MIS 5e forcing. Besides stronger greenhouse gas radiative forcing, the greater MIS 11 GrIS mass loss relative to MIS 5e is attributed to a larger oceanic heat transport towards high latitudes by a stronger Atlantic meridional overturning circulation. The vigorous MIS 11 ocean overturning, in turn, is related to a stronger wind-driven salt transport from low to high latitudes promoting North Atlantic Deep Water formation. The orbital insolation forcing, which causes the ocean current anomalies, is discussed.
    Schlagwort(e): Center for Marine Environmental Sciences; File format; File name; File size; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; MARUM; Uniform resource locator/link to file
    Materialart: Dataset
    Format: text/tab-separated-values, 32 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 34
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    Results of the pollen analysis of the Dyanushka peat sediments K7/P2 (2010)
    PANGAEA
    In:  Supplement to: Werner, Kirstin; Tarasov, Pavel E; Andreev, Andrei A; Müller, Stefanie; Kienast, Frank; Zech, Michael; Zech, Wolfgang; Diekmann, Bernhard (2010): A 12.5-kyr history of vegetation dynamics and mire development with evidence of Younger Dryas larch presence in the Verkhoyansk Mountains, East Siberia, Russia. Boreas, 39, 56-68, https://doi.org/10.1111/j.1502-3885.2009.00116.x
    Details
    Publikationsdatum: 2024-05-31
    Beschreibung: A 415cm thick permafrost peat section from the Verkhoyansk Mountains was radiocarbon-dated and studied using palaeobotanical and sedimentological approaches. Accumulation of organic-rich sediment commenced in a former oxbow lake, detached from a Dyanushka River meander during the Younger Dryas stadial, at ~12.5 kyr BP. Pollen data indicate that larch trees, shrub alder and dwarf birch were abundant in the vegetation at that time. Local presence of larch during the Younger Dryas is documented by well-preserved and radiocarbon-dated needles and cones. The early Holocene pollen assemblages reveal high percentages of Artemisia pollen, suggesting the presence of steppe-like communities around the site, possibly in response to a relatively warm and dry climate ~11.4-11.2 kyr BP. Both pollen and plant macrofossil data demonstrate that larch woods were common in the river valley. Remains of charcoal and pollen of Epilobium indicate fire events and mark a hiatus ~11.0-8.7 kyr BP. Changes in peat properties, C31/C27 alkane ratios and radiocarbon dates suggest that two other hiatuses occurred ~8.2-6.9 and ~6.7-0.6 kyr BP. Prior to 0.6 kyr BP, a major fire destroyed the mire surface. The upper 60 cm of the studied section is composed of aeolian sands modified in the uppermost part by the modern soil formation. For the first time, local growth of larch during the Younger Dryas has been verified in the western foreland of the Verkhoyansk Mountains (~170km south of the Arctic Circle), thus increasing our understanding of the quick reforestation of northern Eurasia by the early Holocene.
    Schlagwort(e): AGE; Alnus fruticosa-type; Alnus glutinosa; Apiaceae; Artemisia; Asteraceae; Betula alba-type; Betula nana-type; Botrychium; Botrychium lunaria-type; Brassicaceae; Bryozoa, statoblast; Callitriche; Caryophyllaceae; Chenopodiaceae; Chironomidae remains; Cichoriaceae; Cladocera; Cosmarium; Counting, palynology; Cyperaceae; DEPTH, sediment/rock; Drosera; Ephedra; Epilobium; Equisetum; Ericales; Glomus; Huperzia; Indeterminata; Insect remains; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; Juniperus; K7/P2; Lamiaceae; Larix; Linum; Lycopodium; Lycopodium annotinum; Lycopodium clavatum; Menyanthes trifoliata; Myriophyllum; Neorhabdocoela; Pediastrum; Picea; Pinaceae; Pinus pumila; Poaceae; Podospora-type; Pollen, per unit sediment mass; Pollen, redeposited; Pollen, total; Polygonum bistorta-type; Polygonum lapathifolium-type; Polypodium; Potamogeton; PROFILE; Profile sampling; Ranunculaceae; Riccia; Rosaceae; Rumex; Salix; Sanguisorba officinalis; Saxifraga; Scrofulariaceae; Selaginella rupestris; Siberia, Russia; Sordaria; Sparganium; Sphagnum; Sporormiella; Stomata pinaceae; Tardigrada; Thalictrum; Urtica; Zygospore
    Materialart: Dataset
    Format: text/tab-separated-values, 5400 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 35
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    Raw data from 2009 AD Bonaire coral, sample BON-0-A (2011)
    PANGAEA
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): Attributed to extreme Sr/Ca values of any single year; BON-0-A; CaribClim_Coral_Jan 2009; Center for Marine Environmental Sciences; Diploria strigosa, Strontium/Calcium ratio; Diploria strigosa, δ18O; DISTANCE; DRILL; Drilling/drill rig; Estimated based on subannual extension-rate and tie points; ICP-OES, Perkin-Elmer, Optima 3300R; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; Internal coral chronology; MARUM; Mass spectrometer Finnigan MAT 251; referred samples; Sample ID; Southern Caribbean Sea, Bonaire; Tie point
    Materialart: Dataset
    Format: text/tab-separated-values, 841 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 36
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    Transient Holocene experiments under orbital forcing using the comprehensive global climate model CCSM3 (Community Climate System Model 3) (2011)
    PANGAEA
    In:  Supplement to: Varma, Vidya; Prange, Matthias; Merkel, Ute; Kleinen, Thomas; Lohmann, Gerrit; Pfeiffer, Madlene; Renssen, Hans; Wagner, Axel; Wagner, Sebastian; Schulz, Michael (2012): Holocene evolution of the Southern Hemisphere westerly winds in transient simulations with global climate models. Climate of the Past, 8(2), 391-402, https://doi.org/10.5194/cp-8-391-2012
    Details
    Publikationsdatum: 2024-05-31
    Beschreibung: The Southern Hemisphere Westerly Winds (SWW) have been suggested to exert a critical influence on global climate through wind-driven upwelling of deep water in the Southern Ocean and the potentially resulting atmospheric CO2 variations. The investigation of the temporal and spatial evolution of the SWW along with forcings and feedbacks remains a significant challenge in climate research. In this study, the evolution of the SWW under orbital forcing from the early Holocene (9 kyr BP) to pre-industrial modern times is examined with transient experiments using the comprehensive coupled global climate model CCSM3. Analyses of the model results suggest that the annual and seasonal mean SWW were subject to an overall strengthening and poleward shifting trend during the course of the early-to-late Holocene under the influence of orbital forcing, except for the austral spring season, where the SWW exhibited an opposite trend of shifting towards the equator.
    Schlagwort(e): Center for Marine Environmental Sciences; File format; File name; File size; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; MARUM; Uniform resource locator/link to file
    Materialart: Dataset
    Format: text/tab-separated-values, 20 data points
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  • 37
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    Raw data from 1957 AD Bonaire coral, sample BON-9-B (2011)
    PANGAEA
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): Attributed to extreme Sr/Ca values of any single year; BON-9-B; CaribClim_Coral_2006; Center for Marine Environmental Sciences; Diploria strigosa, Strontium/Calcium ratio; Diploria strigosa, δ18O; DISTANCE; DRILL; Drilling/drill rig; Estimated based on subannual extension-rate and tie points; ICP-OES, Perkin-Elmer, Optima 3300R; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; Internal coral chronology; MARUM; Mass spectrometer Finnigan MAT 251; referred samples; Sample ID; Southern Caribbean Sea, Bonaire; Tie point
    Materialart: Dataset
    Format: text/tab-separated-values, 804 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 38
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    Raw data from 3.79 ka Bonaire coral, sample BON-7-A (2011)
    PANGAEA
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): Attributed to extreme Sr/Ca values of any single year; BON-7-A; CaribClim_Coral_2006; Center for Marine Environmental Sciences; Diploria strigosa, Strontium/Calcium ratio; Diploria strigosa, δ18O; DISTANCE; DRILL; Drilling/drill rig; Estimated based on subannual extension-rate and tie points; ICP-OES, Perkin-Elmer, Optima 3300R; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; Internal coral chronology; MARUM; Mass spectrometer Finnigan MAT 251; referred samples; Sample ID; Southern Caribbean Sea, Bonaire; Tie point
    Materialart: Dataset
    Format: text/tab-separated-values, 1936 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 39
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    Reference list of 269 sources used for exploratory search (2012)
    PANGAEA
    Details
    Publikationsdatum: 2024-05-31
    Beschreibung: Today's digital libraries (DLs) archive vast amounts of information in the form of text, videos, images, data measurements, etc. User access to DL content can rely on similarity between metadata elements, or similarity between the data itself (content-based similarity). We consider the problem of exploratory search in large DLs of time-oriented data. We propose a novel approach for overview-first exploration of data collections based on user-selected metadata properties. In a 2D layout representing entities of the selected property are laid out based on their similarity with respect to the underlying data content. The display is enhanced by compact summarizations of underlying data elements, and forms the basis for exploratory navigation of users in the data space. The approach is proposed as an interface for visual exploration, leading the user to discover interesting relationships between data items relying on content-based similarity between data items and their respective metadata labels. We apply the method on real data sets from the earth observation community, showing its applicability and usefulness.
    Schlagwort(e): Alaska, USA; Antarctica; Australia; AWIPEV; AWIPEV_based; BAR; Barrow; BER; Bermuda; BOU; Boulder; Brasilia; Brasilia City, Distrito Federal, Brazil; Brazil; BRB; CAB; Cabauw; Canada; CAR; Carpentras; Chesapeake Light; CLH; Colorado, United States of America; Cosmonauts Sea; DAR; Darwin; Dronning Maud Land, Antarctica; E13; France; Georg von Neumayer; Germany; GVN; Israel; Japan; KWA; Kwajalein; LIN; Lindenberg; MAN; Momote; Monitoring station; MONS; NAU; Nauru; Nauru Island; Neumayer_based; NEUMAYER III; North Pacific Ocean; NYA; Ny-Ålesund; Ny-Ålesund, Spitsbergen; Oklahoma, United States of America; PAL; Palaiseau, SIRTA Observatory; Papua New Guinea; PAY; Payerne; Petrolina; PTR; REG; Regina; São Martinho da Serra; SBO; Sede Boqer; SMS; South Atlantic Ocean; Southern Great Plains; South Pole; SPO; Switzerland; SYO; Syowa; TAT; Tateno; The Netherlands
    Materialart: Dataset
    Format: 269 datasets
    Standort Signatur Erwartet Verfügbarkeit
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  • 40
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    (Figure 2) Diatom relative abundance of sediment core PS58/254-1 (2012)
    PANGAEA
    In:  Supplement to: Konfirst, Matthew Alan; Scherer, Reed P; Hillenbrand, Claus-Dieter; Kuhn, Gerhard (2012): A marine diatom record from the Amundsen Sea – Insights into oceanographic and climatic response to the Mid-Pleistocene Transition in the West Antarctic sector of the Southern Ocean. Marine Micropaleontology, 92-93, 40-51, https://doi.org/10.1016/j.marmicro.2012.05.001
    Details
    Publikationsdatum: 2024-05-31
    Beschreibung: The goal of this study is to assess the changes that have occurred during the Mid-Pleistocene Transition, an important transitional period in cryosphere evolution, by examining the siliceous microfossil record of sediments collected proximal to a major ice drainage outlet for the West Antarctic Ice Sheet. Core PS58/254 was collected from a sediment drift on the upper continental rise in the Amundsen Sea, directly offshore from Pine Island Bay, one of the three main discharge areas for the West Antarctic Ice Sheet (WAIS). Published data on physical properties, geochemical composition, grain size and clay mineral assemblages are complemented here by a high-resolution record (sample spacing 10 cm) of the siliceous microfossil assemblages (diatoms and silicoflagellates). Between 1200 ka and 621 ka, the assemblage is relatively diverse, with Actinocyclus ingens, Thalassiothrix antarctica and Fragilariopsis kerguelensis dominating the assemblages, but diatom abundance is variable from low to barren. Additionally, the occurrence of A. ingens, Thalassiosira elliptipora and Thalassiosira fasciculata is used to confirm and further refine the existing age model and extend it back to 1200 ka. Species composition during the last ca. 621 ka is dominated by F. kerguelensis, which consistently comprises 80-90% of the assemblage. A clear relationship between diatom abundance and glacial/interglacial variability is apparent after 621 ka, which resembles the glacial-interglacial variability previously observed in other proxy data. A significant change in both sediment composition and diatom assemblages is observed at 621 ka. This change concurs with the last abundant occurrence of A. ingens and the end of the Mid-Pleistocene Transition (MPT, i.e. the onset of modern eccentricity/precession-paced glacial cycles around 650 ka). We suggest that during interglacial periods after 621 ka the Amundsen Sea Low pressure system shifted seasonally southwestwards towards the shelf and thereby increased the advection of relatively warm Circumpolar Deep Water (CDW) onto the Amundsen Sea shelf, which is a major factor for present ice-sheet melting in this part of West Antarctica.
    Schlagwort(e): Accumulation rate, mass; Actinocyclus actinochilus; Actinocyclus ingens; AGE; ANT-XVIII/5a; AWI_Paleo; Azpeitia tabularis; Calculated; Chaetoceros spp.; Counting, diatoms; DEPTH, sediment/rock; Diatoms, marine; Diatoms, reworked; Diatoms, sea ice; Diatoms, total, per unit sediment mass; Diatoms tropical/subtropical; Distephanus speculum; Eucampia antarctica; Fragilariopsis curta; Fragilariopsis kerguelensis; Fragilariopsis separanda; Hemidiscus karstenii; KL; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Piston corer (BGR type); Polarstern; PS58; PS58/254-1; Rhizosolenia spp.; Rouxia antarctica; Rouxia constricta; Southeast Pacific; Thalassionema spp.; Thalassiosira elliptipora; Thalassiosira fasciculata; Thalassiosira gracilis; Thalassiosira lentiginosa; Thalassiosira oestrupii; Thalassiosira oliverana; Thalassiosira tetraoestrupii; Thalassiosira tetraoestrupii var. reimeri; Thalassiothrix antarctica
    Materialart: Dataset
    Format: text/tab-separated-values, 5307 data points
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  • 41
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    Mineral dust deposition in interglacial and glacial climate conditions: model results (2012)
    PANGAEA
    Details
    Publikationsdatum: 2024-05-31
    Beschreibung: The global aerosol/climate model ECHAM5-HAM is used in order to investigate the dust cycle for four interglacial and one glacial climate conditions. The 20-year time-slices are the pre-industrial control (CTRL), mid-Holocene (6000 years BP), last glacial inception (115000 years BP), Eemian (126000 years BP) and Last Glacial Maximum (LGM) (21000 years BP) time intervals. The study is focused on the Antarctic region. The model is able to reproduce the magnitude order of dust deposition globally for the pre-industial and LGM climates. Correlation coefficient of the natural logarithm of the observed and modeled values is 0.78 for the CTRL and 0.81 for the LGM. For the pre-industrial simulation the model overestimates observed values in Antarctica by a factor of about 2-3 due to overestimation of the Australian dust source and too high wet deposition in the Antarctica interior. In the LGM, the model underestimates dust deposition in eastern Antarctica by a factor of about 4-5 due to underestimation of the South American dust source. More records are needed to validate dust deposition for the past interglacial time-slices. The modeled results show that dust deposition in Antarctica in the past interglacial time-slices is higher than in the CTRL simulation. The largest increase of dust deposition in Antarctica is simulated for the LGM, showing about 10-fold increase compared to CTRL.
    Schlagwort(e): Abbreviation; Experiment; File format; File name; File size; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; Parameter; Uniform resource locator/link to model result file; Unit
    Materialart: Dataset
    Format: text/tab-separated-values, 80 data points
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  • 42
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    Results of the coupled atmosphere-land surface model ECHAM5-JSBACH in NetCDF format (2013)
    PANGAEA
    In:  Supplement to: Haese, Barbara; Werner, Martin; Lohmann, Gerrit (2013): Stable water isotopes in the coupled atmosphere–land surface model ECHAM5-JSBACH. Geoscientific Model Development, 6(5), 1463-1480, https://doi.org/10.5194/gmd-6-1463-2013
    Details
    Publikationsdatum: 2024-05-31
    Beschreibung: In this study we present first results of a new model development, ECHAM5-JSBACH-wiso, where we have incorporated the stable water isotopes H218O and HDO as tracers in the hydrological cycle of the coupled atmosphere-land surface model ECHAM5-JSBACH. The ECHAM5-JSBACH-wiso model was run under present-day climate conditions at two different resolutions (T31L19, T63L31). A comparison between ECHAM5-JSBACH-wiso and ECHAM5-wiso shows that the coupling has a strong impact on the simulated temperature and soil wetness. Caused by these changes of temperature and the hydrological cycle, the d18O in precipitation also shows variations from -4 permil up to 4 permil. One of the strongest anomalies is shown over northeast Asia where, due to an increase of temperature, the d18O in precipitation increases as well. In order to analyze the sensitivity of the fractionation processes over land, we compare a set of simulations with various implementations of these processes over the land surface. The simulations allow us to distinguish between no fractionation, fractionation included in the evaporation flux (from bare soil) and also fractionation included in both evaporation and transpiration (from water transport through plants) fluxes. While the isotopic composition of the soil water may change for d18O by up to +8 permil:, the simulated d18O in precipitation shows only slight differences on the order of ±1 permil. The simulated isotopic composition of precipitation fits well with the available observations from the GNIP (Global Network of Isotopes in Precipitation) database.
    Schlagwort(e): File name; File size; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; Uniform resource locator/link to model result file
    Materialart: Dataset
    Format: text/tab-separated-values, 33 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 43
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    Basic measurements of radiation from the Baseline Surface Radiation Network (BSRN) in the years 1992 to 2012, reference list of 6378 datasets (2013)
    PANGAEA
    Details
    Publikationsdatum: 2024-05-31
    Beschreibung: In the framework of the global energy balance, the radiative energy exchanges between Sun, Earth and space are now accurately quantified from new satellite missions. Much less is known about the magnitude of the energy flows within the climate system and at the Earth surface, which cannot be directly measured by satellites. In addition to satellite observations, here we make extensive use of the growing number of surface observations to constrain the global energy balance not only from space, but also from the surface. We combine these observations with the latest modeling efforts performed for the 5th IPCC assessment report to infer best estimates for the global mean surface radiative components. Our analyses favor global mean downward surface solar and thermal radiation values near 185 and 342 Wm**-2, respectively, which are most compatible with surface observations. Combined with an estimated surface absorbed solar radiation and thermal emission of 161 Wm**-2 and 397 Wm**-2, respectively, this leaves 106 Wm**-2 of surface net radiation available for distribution amongst the non-radiative surface energy balance components. The climate models overestimate the downward solar and underestimate the downward thermal radiation, thereby simulating nevertheless an adequate global mean surface net radiation by error compensation. This also suggests that, globally, the simulated surface sensible and latent heat fluxes, around 20 and 85 Wm**-2 on average, state realistic values. The findings of this study are compiled into a new global energy balance diagram, which may be able to reconcile currently disputed inconsistencies between energy and water cycle estimates.
    Schlagwort(e): Alaska, USA; Algeria; Alice Springs; Antarctica; ASP; Australia; AWIPEV; AWIPEV_based; BAR; Barrow; Baseline Surface Radiation Network; BER; Bermuda; BIL; Billings; BON; Bondville; BOS; BOU; Boulder; Brazil; BSRN; CAB; Cabauw; CAM; Camborne; Canada; CAR; Carpentras; Cener; Chesapeake Light; China; CLH; CNR; COC; Cocos (Keeling) Islands; Cocos Island; Colorado, United States of America; Cosmonauts Sea; DAA; DAR; Darwin; Darwin Met Office; De Aar; Desert Rock; DRA; Dronning Maud Land, Antarctica; DWN; E13; Estonia; FLO; Florianopolis; Fort Peck; FPE; France; GCR; Georg von Neumayer; Germany; Goodwin Creek; GVN; Illinois, United States of America; ILO; Ilorin; ISH; Ishigakijima; Israel; IZA; Izaña; Japan; KWA; Kwajalein; LER; Lerwick; LIN; Lindenberg; Macdonnell Ranges, Northern Territory, Australia; MAN; Mississippi, United States of America; Momote; Monitoring station; MONS; Montana, United States of America; NAU; Nauru; Nauru Island; Neumayer_based; NEUMAYER III; Nevada, United States of America; Nigeria; North Pacific Ocean; NYA; Ny-Ålesund; Ny-Ålesund, Spitsbergen; Oklahoma, United States of America; PAL; Palaiseau, SIRTA Observatory; Papua New Guinea; PAY; Payerne; Pennsylvania, United States of America; PSU; REG; Regina; Rock Springs; São Martinho da Serra; Saudi Arabia; SBO; Sede Boqer; Shetland Island, United Kingdom; Sioux Falls; SMS; Solar Village; South Africa; South Atlantic Ocean; South Dakota, United States of America; Southern Great Plains; South Pole; SOV; Spain, Sarriguren, Navarra; SPO; Switzerland; SXF; SYO; Syowa; TAM; Tamanrasset; TAT; Tateno; Tenerife, Spain; The Netherlands; TOR; Toravere; United Kingdom; XIA; Xianghe
    Materialart: Dataset
    Format: 6378 datasets
    Standort Signatur Erwartet Verfügbarkeit
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  • 44
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    ClimSens Project Database (Table 1) (2014)
    PANGAEA
    In:  Supplement to: Mudelsee, Manfred; Lohmann, Gerrit (2015): Climate sensitivity during and between interglacials. In: Michael Schulz and Andre Paul (eds.), Integrated analysis of interglacial climate dynamics (INTERDYNAMIC), SpringerBriefs in Earth System Sciences, ISBN: 978-3-319-00692-5 (Print) 978-3-319-00693-2 (Online), doi:10.1007/978-3-319-00693-2, 19-23, https://doi.org/10.1007/978-3-319-00693-2_4
    Details
    Publikationsdatum: 2024-05-31
    Beschreibung: Studying the climate dynamics of past interglacials (IGs) may help to better assess the anthropogenically influenced dynamics of the current IG, the Holocene. We select IG sections from the longest ice core archive, EPICA Dome C (EDC), which covers the past 800 thousand years, and study as well several long, high-resolution marine sediment records. We analyze records of Antarctic temperature, radiative forcing (greenhouse gases and other factors), and sea-surface temperature (SST). Change-point regressions inform about longer-term climate changes and trends within IGs. Comparing trends in temperature with trends in forcing allows inference of longer-term IG climate sensitivities. Results from many records indicate deviations from a “Holocene climate optimum”. IG sensitivities are found to be comparable to estimates for the instrumental period; warming or cooling phases during Marine Isotope Stage (MIS) 5 or 11 do not show significant differences in climate sensitivity.
    Schlagwort(e): Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK
    Materialart: Dataset
    Format: application/pdf, 93.6 kBytes
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  • 45
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    Nutrients measured on under sea-ice water samples during POLARSTERN cruise ARK-XXVII/3 (IceArc) in 2012 (2014)
    PANGAEA
    In:  Royal Netherlands Institute for Sea Research, Texel
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): Arctic Ocean; ARK-XXVII/3; Comment; Date/time end; Date/time start; DEPTH, water; Device type; Distance, relative, X; Distance, relative, Y; Distance to sea ice bottom; Event label; ICE; Ice station; Ice station #1; Ice station #2; Ice station #3; Ice station #4; Ice station #5; Ice station #6; Ice station #7; Ice station #8; Latitude of event; Longitude of event; Nitrate; Nitrate and Nitrite; Nitrite; Optional event label; Phosphate; Polarstern; PS80/224-1; PS80/237-1; PS80/255-1; PS80/277-1; PS80/323-1; PS80/335-1; PS80/349-1; PS80/360-1; PS80 IceArc; Sample code/label; Silicate
    Materialart: Dataset
    Format: text/tab-separated-values, 296 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 46
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    Monthly Bonaire coral Sr/Ca and oxygen isotope data from 118 kyr ago (coral BON-5-D) (2015)
    PANGAEA
    In:  Supplement to: Felis, Thomas; Giry, Cyril; Scholz, Denis; Lohmann, Gerrit; Pfeiffer, Madlene; Pätzold, Jürgen; Kölling, Martin; Scheffers, Sander R (2015): Tropical Atlantic temperature seasonality at the end of the last interglacial. Nature Communications, 6, 6159, https://doi.org/10.1038/ncomms7159
    Details
    Publikationsdatum: 2024-05-31
    Beschreibung: The end of the last interglacial period, ~118 kyr ago, was characterized by substantial ocean circulation and climate perturbations resulting from instabilities of polar ice sheets. These perturbations are crucial for a better understanding of future climate change. The seasonal temperature changes of the tropical ocean, however, which play an important role in seasonal climate extremes such as hurricanes, floods and droughts at the present day, are not well known for this period that led into the last glacial. Here we present a monthly resolved snapshot of reconstructed sea surface temperature in the tropical North Atlantic Ocean for 117.7±0.8 kyr ago, using coral Sr/Ca and d18O records. We find that temperature seasonality was similar to today, which is consistent with the orbital insolation forcing. Our coral and climate model results suggest that temperature seasonality of the tropical surface ocean is controlled mainly by orbital insolation changes during interglacials.
    Schlagwort(e): BON-5-D; Calculated, see reference(s); CaribClim_Coral_2006; Center for Marine Environmental Sciences; Diploria strigosa, Strontium/Calcium ratio; Diploria strigosa, δ18O; DRILL; Drilling/drill rig; ICP-OES, Perkin-Elmer, Optima 3300R; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; Internal coral chronology; MARUM; Mass spectrometer Finnigan MAT 251; Southern Caribbean Sea, Bonaire
    Materialart: Dataset
    Format: text/tab-separated-values, 720 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 47
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    Marine Isotope Stage (MIS) 11 results of model data with Community Climate System Model version 3 including the Dynamic Global Vegetation Model (CCSM3-DGVM) in NetCDF format at global and regional scale (2014)
    PANGAEA
    In:  Supplement to: Kleinen, Thomas; Hildebrandt, Steffi; Prange, Matthias; Rachmayani, Rima; Müller, Stefanie; Bezrukova, Elena V; Brovkin, Victor; Tarasov, Pavel E (2014): The climate and vegetation of Marine Isotope Stage 11 – Model results and proxy-based reconstructions at global and regional scale. Quaternary International, 348, 247-265, https://doi.org/10.1016/j.quaint.2013.12.028
    Details
    Publikationsdatum: 2024-05-31
    Beschreibung: The climate of Marine Isotope Stage (MIS) 11, the interglacial roughly 400,000 years ago, is investigated for four time slices, 416, 410, 400, and 394 ka. The overall picture is that MIS 11 was a relatively warm interglacial in comparison to preindustrial, with Northern Hemisphere (NH) summer temperatures early in MIS 11 (416-410 ka) warmer than preindustrial, though winters were cooler. Later in MIS 11, especially around 400 ka, conditions were cooler in the NH summer, mainly in the high latitudes. Climate changes simulated by the models were mainly driven by insolation changes, with the exception of two local feedbacks that amplify climate changes. Here, the NH high latitudes, where reductions in sea ice cover lead to a winter warming early in MIS 11, as well as the tropics, where monsoon changes lead to stronger climate variations than one would expect on the basis of latitudinal mean insolation change alone, are especially prominent. The results support a northward expansion of trees at the expense of grasses in the high northern latitudes early during MIS 11, especially in northern Asia and North America.
    Schlagwort(e): Center for Marine Environmental Sciences; File format; File name; File size; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; MARUM; Numerical experiments using the general circulation model CCSM3; Uniform resource locator/link to model result file
    Materialart: Dataset
    Format: text/tab-separated-values, 60 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 48
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    Holocene carbon cycle dynamics, links to model files (2011)
    PANGAEA
    In:  Supplement to: Kleinen, Thomas; Brovkin, Victor; von Bloh, Werner; Archer, David E; Munhoven, Guy (2011): Holocene carbon cycle dynamics. Geophysical Research Letters, 37, L02705, 5 pp, https://doi.org/10.1029/2009GL041391
    Details
    Publikationsdatum: 2024-05-31
    Beschreibung: We are investigating the late Holocene rise in CO2 by performing four experiments with the climate-carbon-cycle model CLIMBER2-LPJ. Apart from the deep sea sediments, important carbon cycle processes considered are carbon uptake or release by the vegetation, carbon uptake by peatlands, and CO 2 release due to shallow water sedimentation of CaCO3. Ice core data of atmospheric CO2 between 8 ka BP and preindustrial climate can only be reproduced if CO2 outgassing due to shallow water sedimentation of CaCO3 is considered. In this case the model displays an increase of nearly 20 ppmv CO2 between 8 ka BP and present day. Model configurations that do not contain this forcing show a slight decrease in atmospheric CO2. We can therefore explain the late Holocene rise in CO2 by invoking natural forcing factors only, and anthropogenic forcing is not required to understand preindustrial CO2 dynamics.
    Schlagwort(e): Experiment; File format; File name; File size; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; Parameter; Uniform resource locator/link to model result file; Unit
    Materialart: Dataset
    Format: text/tab-separated-values, 285 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 49
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    Organic marker compounds in surface sediments from the Nordic Seas (2011)
    PANGAEA
    Details
    Publikationsdatum: 2024-05-31
    Beschreibung: Organic geochemical analyses of marine surface sediments from the continental margins of East Greenland and West Spitsbergen provide for a biomarker-based estimate of recent sea ice conditions in the northern North Atlantic. By means of the sea ice proxy IP25 and phytoplankton derived biomarkers (e.g. brassicasterol, dinosterol) we reconstruct sea ice and sea surface conditions, respectively. The combination of IP25 with a phytoplankton marker (in terms of a phytoplankton marker-IP25 index; PIP25) proves highly valuable to properly interpret the sea ice proxy signal as an under- or overestimation of sea ice coverage can be circumvented. A comparison of this biomarker-based assessment of the sea ice distribution in the study area with (1) modern remote sensing data and (2) numerical modelling results reveals a good agreement between organic geochemical, satellite and modelling observations. The reasonable simulation of modern sea ice conditions by means of a regional ocean-sea ice model demonstrates the feasibility to effectively integrate the complex atmospheric and oceanic circulation features as they prevail in the study area. The good correlation between modelled sea ice parameters and the biomarker-based estimate of sea ice coverage substantiates that linking proxy and model data occurs to be a promising concept in terms of a cross-evaluation. This combinatory approach may provide a first step towards quantitative sea ice reconstructions by means of IP25. Future IP25 studies on marine surface sediments from the Arctic realm, however, are recommended to extend and validate this new attempt of using IP25 in combination with a phytoplankton marker as a quantitative measure for sea ice reconstructions.
    Schlagwort(e): 2,6,10,14-Tetramethyl-7-(3-methylpent-4-enyl)pentadecane, per unit mass total organic carbon; 2,6,10,14-Tetramethyl-7-(3-methylpent-4-enyl)pentadecane per unit sediment mass; 24-Methylcholesta-5,22E-dien-3beta-ol, per unit mass total organic carbon; 24-Methylcholesta-5,22E-dien-3beta-ol per unit sediment mass; 4alpha,23,24-Trimethyl-5alpha-cholest-22E-en-3beta-ol, per unit mass total organic carbon; 4alpha,23,24-Trimethyl-5alpha-cholest-22E-en-3beta-ol per unit sediment mass; ARK-X/2; ARK-XIX/4a; ARK-XVI/1; ARK-XVIII/1; AWI_Paleo; Calculated, see reference(s); DEPTH, sediment/rock; East Greenland Sea; Elevation of event; Event label; Gas chromatography - Mass spectrometry (GC-MS); Giant box corer; GKG; Greenland Sea; HG_II; Hurry Inlet, East Greenland; Iceland Sea; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; Kempe Fjord, East Greenland; Latitude of event; Location of event; Longitude of event; MUC; MultiCorer; n-Alkane C15; n-Alkane C15, per unit mass total organic carbon; n-Alkane C17; n-Alkane C17, per unit mass total organic carbon; n-Alkane C19; n-Alkane C19, per unit mass total organic carbon; North Greenland Sea; OBS; OBS314; Ocean bottom seismometer; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Phytoplankton biomarker Brassicasterol IP25 index; Phytoplankton biomarker Dinosterol IP25 index; Phytoplankton biomarker short-chain n-alkanes IP25 index; Polarstern; PS2630-7; PS2642-2; PS2648-3; PS2651-3; PS2654-6; PS31; PS31/138; PS31/155; PS31/172; PS31/177; PS31/180; PS57/127-1; PS57/130-1; PS57/131-2; PS57/136-2; PS57/137-2; PS57/138-1; PS57/145-1; PS57/166-2; PS57 ARKTIEF; PS62; PS62/002-3; PS62/003-3; PS62/004-2; PS62/012-2; PS62/015-4; PS62/017-1; PS62/020-1; PS62/022-3; PS62/026-3; PS62/027-1; PS62/028-1; PS62/029-2; PS62/038-1; PS62/041-1; PS62/044-1; PS62/046-3; PS62/048-1; PS62/050-1; PS64; PS64/487-1; PS64/488-1; PS64/489-1; PS64/490-1; PS64/504-1; PS64/508-1; PS64/511-1; PS64/516-1; PS64/528-1; PS64/531-1; PS64/573-1; PS64/582-1; PS64/583-1; Short-chain n-alkanes, C15H32+C17H36+C19H40, per unit mass total organic carbon; Short-chain n-alkanes, C15H32+C17H36+C19H40 per unit sediment mass; Ø Fjord, East Greenland
    Materialart: Dataset
    Format: text/tab-separated-values, 748 data points
    Standort Signatur Erwartet Verfügbarkeit
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    DATEN PANGAEA
  • 50
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    Simulated agricultural subsistence, timing of transition, and percentage of immigrant farmers (2011)
    PANGAEA
    In:  Supplement to: Lemmen, Carsten; Gronenborn, Detlef; Wirtz, Kai W (2011): A simulation of the Neolithic transition in Western Eurasia. Journal of Archaeological Science, 38(12), 3459-3470, https://doi.org/10.1016/j.jas.2011.08.008
    Details
    Publikationsdatum: 2024-05-31
    Beschreibung: Farming and herding were introduced to Europe from the Near East and Anatolia; there are, however, considerable arguments about the mechanisms of this transition. Were it the people who moved and either outplaced, or admixed with, the indigenous hunter-gatherer groups? Or was it material and information that moved---the Neolithic Package---consisting of domesticated plants and animals and the knowledge of their use? The latter process is commonly referred to as cultural diffusion and the former as demic diffusion. Despite continuous and partly combined efforts by archaeologists, anthropologists, linguists, palaeontologists and geneticists, a final resolution of the debate has not yet been reached. In the present contribution we interpret results from the Global Land Use and technological Evolution Simulator (GLUES). GLUES is a mathematical model for regional sociocultural development, embedded in the geoenvironmental context, during the Holocene. We demonstrate that the model is able to realistically hindcast the expansion speed and the inhomogeneous space-time evolution of the transition to agropastoralism in western Eurasia. In contrast to models that do not resolve endogenous sociocultural dynamics, our model describes and explains how and why the Neolithic advanced in stages. We uncouple the mechanisms of migration and information exchange and also of migration and the spread of agropastoralism. We find that: (1) An indigenous form of agropastoralism could well have arisen in certain Mediterranean landscapes, but not in Northern and Central Europe, where it depended on imported technology and material. (2) Both demic diffusion by migration and cultural diffusion by trade may explain the western European transition equally well. (3) Migrating farmers apparently contribute less than local adopters to the establishment of agropastoralism. Our study thus underlines the importance of adoption of introduced technologies and economies by resident foragers.
    Schlagwort(e): GLUES_LBK; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; Model; Model version 1.1.18; western Eurasia
    Materialart: Dataset
    Format: application/gzip, 141 kBytes
    Standort Signatur Erwartet Verfügbarkeit
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  • 51
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    Raw data from 6.22 ka Bonaire coral, sample BON-3-E (2011)
    PANGAEA
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): Attributed to extreme Sr/Ca values of any single year; BON-3-E; CaribClim_Coral_2006; Center for Marine Environmental Sciences; Diploria strigosa, Strontium/Calcium ratio; Diploria strigosa, δ18O; DISTANCE; DRILL; Drilling/drill rig; Estimated based on subannual extension-rate and tie points; ICP-OES, Perkin-Elmer, Optima 3300R; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; Internal coral chronology; MARUM; Mass spectrometer Finnigan MAT 251; referred samples; Sample ID; Southern Caribbean Sea, Bonaire; Tie point
    Materialart: Dataset
    Format: text/tab-separated-values, 3394 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 52
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    Solar sensitivity experiments for the pre-industrial time period using the comprehensive global climate model CCSM3 (Community Climate System Model 3) (2011)
    PANGAEA
    In:  Supplement to: Varma, Vidya; Prange, Matthias; Lamy, Frank; Merkel, Ute; Schulz, Michael (2011): Solar-forced shifts of the Southern Hemisphere Westerlies during the Holocene. Climate of the Past, 7, 339-347, https://doi.org/10.5194/cp-7-339-2011
    Details
    Publikationsdatum: 2024-05-31
    Beschreibung: The Southern Hemisphere Westerly Winds (SWW) constitute an important zonal circulation that influences large-scale precipitation patterns and ocean circulation. Variations in their intensity and latitudinal position have been suggested to exert a strong influence on the CO2 budget in the Southern Ocean, thus making them a potential factor affecting the global climate. The possible influence of solar forcing on SWW variability during the Holocene is addressed. Solar sensitivity experiments with a comprehensive global climate model (CCSM3) are carried out to study the response of SWW to solar variability. In addition, It is shown that a high-resolution iron record from the Chilean continental slope (41° S), which is interpreted to reflect changes in the position of the SWW, is significantly correlated with reconstructed solar activity during the past 3000 years. Taken together, the proxy and model results suggest that centennial-scale periods of lower (higher) solar activity caused equatorward (southward) shifts of the annual mean SWW.
    Schlagwort(e): Center for Marine Environmental Sciences; File format; File name; File size; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; MARUM; Uniform resource locator/link to file
    Materialart: Dataset
    Format: text/tab-separated-values, 36 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 53
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    Raw data from 3.83 ka Bonaire coral, sample BON-7-B (2011)
    PANGAEA
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): Attributed to extreme Sr/Ca values of any single year; BON-7-B; CaribClim_Coral_2006; Center for Marine Environmental Sciences; Diploria strigosa, Strontium/Calcium ratio; Diploria strigosa, δ18O; DISTANCE; DRILL; Drilling/drill rig; Estimated based on subannual extension-rate and tie points; ICP-OES, Perkin-Elmer, Optima 3300R; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; Internal coral chronology; MARUM; Mass spectrometer Finnigan MAT 251; referred samples; Sample ID; Southern Caribbean Sea, Bonaire; Tie point
    Materialart: Dataset
    Format: text/tab-separated-values, 1772 data points
    Standort Signatur Erwartet Verfügbarkeit
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    DATEN PANGAEA
  • 54
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    Time-oriented earth observation measurements from the Baseline Surface Radiation Network (BSRN) in the years 1992 to 2012, reference list of 6813 datasets (2012)
    PANGAEA
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): Alaska, USA; Algeria; Alice Springs; Antarctica; ASP; Australia; AWIPEV; AWIPEV_based; BAR; Barrow; Baseline Surface Radiation Network; BER; Bermuda; BIL; Billings; BON; Bondville; BOS; BOU; Boulder; Brasilia; Brasilia City, Distrito Federal, Brazil; Brazil; BRB; BSRN; CAB; Cabauw; CAM; Camborne; Canada; CAR; Carpentras; Cener; Chesapeake Light; China; CLH; CNR; COC; Cocos (Keeling) Islands; Cocos Island; Colorado, United States of America; Concordia Station, Dome C; Cosmonauts Sea; DAA; DAR; Darwin; Darwin Met Office; De Aar; Desert Rock; DOM; DRA; Dronning Maud Land, Antarctica; DWN; E13; Ellesmere Island, Canadian Arctic Archipelago; Estonia; EUR; Eureka; FLO; Florianopolis; Fort Peck; FPE; France; FUA; Fukuoka; GCR; Georg von Neumayer; Germany; Goodwin Creek; GVN; Illinois, United States of America; ILO; Ilorin; ISH; Ishigakijima; Israel; IZA; Izaña; Japan; KWA; Kwajalein; LAU; Lauder; LER; Lerwick; LIN; Lindenberg; Macdonnell Ranges, Northern Territory, Australia; MAN; Minamitorishima; Minami-Torishima; Mississippi, United States of America; MNM; Momote; Monitoring station; MONS; Montana, United States of America; NAU; Nauru; Nauru Island; Neumayer_based; NEUMAYER III; Nevada, United States of America; New Zealand; Nigeria; North Pacific Ocean; NYA; Ny-Ålesund; Ny-Ålesund, Spitsbergen; Oklahoma, United States of America; PAL; Palaiseau, SIRTA Observatory; Papua New Guinea; PAY; Payerne; Pennsylvania, United States of America; Petrolina; PSU; PTR; REG; Regina; RLM; Rock Springs; Rolim de Moura; São Martinho da Serra; SAP; Sapporo; Saudi Arabia; SBO; Sede Boqer; Shetland Island, United Kingdom; Siberia, Russia; Sioux Falls; SMS; Solar Village; South Africa; South Atlantic Ocean; South Dakota, United States of America; Southern Great Plains; South Pole; SOV; Spain, Sarriguren, Navarra; SPO; Switzerland; SXF; SYO; Syowa; TAM; Tamanrasset; TAT; Tateno; Tenerife, Spain; The Netherlands; TIK; Tiksi; TOR; Toravere; United Kingdom; XIA; Xianghe
    Materialart: Dataset
    Format: 6787 datasets
    Standort Signatur Erwartet Verfügbarkeit
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  • 55
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    Results of modelled Arctic river discharge trends since 7 ka BP (2011)
    PANGAEA
    In:  Supplement to: Wagner, Axel; Lohmann, Gerrit; Prange, Matthias (2011): Arctic river discharge trends since 7 ka BP. Global and Planetary Change, 79(1-2), 48-60, https://doi.org/10.1016/j.gloplacha.2011.07.006
    Details
    Publikationsdatum: 2024-05-31
    Beschreibung: The Arctic hydrological cycle throughout the Holocene is analyzed based on the results of transient simulations with the coupled atmosphere-ocean circulation model ECHO-G. The results suggest a ~ 2 % increase of mid-Holocene to preindustrial Arctic river discharges for the Eurasian continent. However, rivers of the North America Arctic realm show a moderate runoff decline of approximately 4 to 5 % for the same period. The total river discharge into the Arctic Ocean has remained at an approximately constant preindustrial level since the mid Holocene. The positive discharge trend within Eurasia is caused by a more rapid decrease in local net evaporation compared to a smaller decline in advected moisture and hence precipitation. This effect is neither recognized within the North American Arctic domain nor in the far eastern part of the Eurasian Arctic realm. A detailed comparison of these model findings with a variety of proxy studies is conducted. The collected proxy records show trends of continental surface temperatures and precipitation rates that are consistent with the simulations. A continuation of the transient Holocene runs for the 19th and 20th century with increased greenhouse gases indicates an increase of the total river influx into the Arctic Ocean of up to 7.6 %. The Eurasian river discharges increase by 7.5 %, the North American discharges by up to 8.4 %. The most rapid increases have been detected since the beginning of the 20th century. These results are corroborated by the observed rising of Arctic river discharges during the last century which is attributed to anthropogenic warming. The acceleration of the Arctic hydrological cycle in the 20th century is without precedence in the Holocene.
    Schlagwort(e): -; Code; Date/time end; Date/time start; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; Name; Number of levels; Parameter; Sample code/label; Uniform resource locator/link to model result file; Unit
    Materialart: Dataset
    Format: text/tab-separated-values, 396 data points
    Standort Signatur Erwartet Verfügbarkeit
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    DATEN PANGAEA
  • 56
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    Distribution of planktic foraminifera and stable istopes of sediment core MSM05/5_712-1 (2010)
    PANGAEA
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): Counting; Counting, foraminifera; DEPTH, sediment/rock; Foraminifera, benthic δ13C; Foraminifera, benthic δ18O; Foraminifera, planktic; Foraminifera, planktic, subpolar; Foraminifera, planktic δ13C; Foraminifera, planktic δ18O; Fram Strait; Giant box corer; GKG; Grain size, sieving/settling tube; Ice rafted debris; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; Maria S. Merian; Mass spectrometry; MSM05/5; MSM05/5_712-1; Neogloboquadrina pachyderma sinistral; Size fraction 〉 0.064 mm; Size fraction 1.000-0.063 mm
    Materialart: Dataset
    Format: text/tab-separated-values, 930 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 57
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    Holocene experiment with coupled atmosphere-ocean-model ECHAM5/MPI-OM (2012)
    PANGAEA
    In:  Supplement to: Fischer, Nils; Jungclaus, Johann H (2011): Evolution of the seasonal temperature cycle in a transient Holocene simulation: orbital forcing and sea-ice. Climate of the Past, 7, 1139-1148, https://doi.org/10.5194/cp-7-1139-2011
    Details
    Publikationsdatum: 2024-05-31
    Beschreibung: Changes in the Earth's orbit lead to changes in the seasonal and meridional distribution of insolation. We quantify the influence of orbitally induced changes on the seasonal temperature cycle in a transient simulation of the last 6000 years – from the mid-Holocene to today – using a coupled atmosphere-ocean general circulation model (ECHAM5/MPI-OM) including a land surface model (JSBACH). The seasonal temperature cycle responds directly to the insolation changes almost everywhere. In the Northern Hemisphere, its amplitude decreases according to an increase in winter insolation and a decrease in summer insolation. In the Southern Hemisphere, the opposite is true. Over the Arctic Ocean, decreasing summer insolation leads to an increase in sea-ice cover. The insulating effect of sea ice between the ocean and the atmosphere leads to decreasing heat flux and favors more "continental" conditions over the Arctic Ocean in winter, resulting in strongly decreasing temperatures. Consequently, there are two competing effects: the direct response to insolation changes and a sea-ice insulation effect. The sea-ice insulation effect is stronger, and thus an increase in the amplitude of the seasonal temperature cycle over the Arctic Ocean occurs. This increase is strongest over the Barents Shelf and influences the temperature response over northern Europe. We compare our modeled seasonal temperatures over Europe to paleo reconstructions. We find better agreements in winter temperatures than in summer temperatures and better agreements in northern Europe than in southern Europe, since the model does not reproduce the southern European Holocene summer cooling inferred from the paleo reconstructions. The temperature reconstructions for northern Europe support the notion of the influence of the sea-ice insulation effect on the evolution of the seasonal temperature cycle.
    Schlagwort(e): Abbreviation; File format; File name; File size; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; Parameter; Uniform resource locator/link to model result file; Unit
    Materialart: Dataset
    Format: text/tab-separated-values, 77 data points
    Standort Signatur Erwartet Verfügbarkeit
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    DATEN PANGAEA
  • 58
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    Raw data from 1.84 ka Bonaire coral, sample BON-20-A (2011)
    PANGAEA
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): Attributed to extreme Sr/Ca values of any single year; BON-20-A; CaribClim_Coral_2006; Center for Marine Environmental Sciences; Diploria strigosa, Strontium/Calcium ratio; Diploria strigosa, δ18O; DISTANCE; DRILL; Drilling/drill rig; Estimated based on subannual extension-rate and tie points; ICP-OES, Perkin-Elmer, Optima 3300R; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; Internal coral chronology; MARUM; Mass spectrometer Finnigan MAT 251; referred samples; Sample ID; Southern Caribbean Sea, Bonaire; Tie point
    Materialart: Dataset
    Format: text/tab-separated-values, 482 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 59
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    Simulated transition to agropastoralism in the Indus valley 7500-3000 BC (2013)
    PANGAEA
    In:  Supplement to: Lemmen, Carsten; Khan, Aurangzeb (2013): A simulation of the Neolithic Transition in the Indus Valley. In: L. Giosan, D. Q. Fuller, K. Nicoll, R. K. Flad & P. D. Clift (eds.) Climates, Landscapes, and Civilizations; American Geophysical Union, Geophysical Monograph Series, 198, 107-114, https://doi.org/10.1029/2012GM001217
    Details
    Publikationsdatum: 2024-05-31
    Beschreibung: The Indus Valley Civilization (IVC) was one of the first great civilizations in prehistory. This bronze age civilization flourished from the end of the fourth millennium BC. It disintegrated during the second millennium BC; despite much research effort, this decline is not well understood. Less research has been devoted to the emergence of the IVC, which shows continuous cultural precursors since at least the seventh millennium BC. To understand the decline, we believe it is necessary to investigate the rise of the IVC, i.e., the establishment of agriculture and livestock, dense populations and technological developments 7000-3000 BC. Although much archaeologically typed information is available, our capability to investigate the system is hindered by poorly resolved chronology, and by a lack of field work in the intermediate areas between the Indus valley and Mesopotamia. We thus employ a complementary numerical simulation to develop a consistent picture of technology, agropastoralism and population developments in the IVC domain. Results from this Global Land Use and technological Evolution Simulator show that there is (1) fair agreement between the simulated timing of the agricultural transition and radiocarbon dates from early agricultural sites, but the transition is simulated first in India then Pakistan; (2) an independent agropas- toralism developing on the Indian subcontinent; and (3) a positive relationship between archeological artifact richness and simulated population density which remains to be quantified.
    Schlagwort(e): Archaeosociomodeling; Baluchistan; GLUES; GLUES_IVC; Harappa; Indus Valley; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; Mehrgarh; Model; Neolithic; Version 1.1.19; western Eurasia
    Materialart: Dataset
    Format: application/x-gzip, 92.4 kBytes
    Standort Signatur Erwartet Verfügbarkeit
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  • 60
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    Model results in NetCDF format of North African vegetation-precipitation in early and mid-Holocene climate simulated by CCSM3-DGVM// (2015)
    PANGAEA
    In:  Supplement to: Rachmayani, Rima; Prange, Matthias; Schulz, Michael (2015): North African vegetation–precipitation feedback in early and mid-Holocene climate simulations with CCSM3-DGVM. Climate of the Past, 11(2), 175-185, https://doi.org/10.5194/cp-11-175-2015
    Details
    Publikationsdatum: 2024-05-31
    Beschreibung: The present study analyses the sign, strength, and working mechanism of the vegetation-precipitation feedback over North Africa in middle (6 ka BP) and early Holocene (9 ka BP) simulations using the comprehensive coupled climate-vegetation model CCSM3-DGVM (Community Climate System Model version 3 and a dynamic global vegetation model). The coupled model simulates enhanced summer rainfall and a northward migration of the West African monsoon trough along with an expansion of the vegetation cover for the early and middle Holocene compared to the pre-industrial period. It is shown that dynamic vegetation enhances the orbitally triggered summer precipitation anomaly by approximately 20% in the Sahara-Sahel region (10-25° N, 20° W-30° E) in both the early and mid-Holocene experiments compared to their fixed-vegetation counterparts. The primary vegetation-rainfall feedback identified here operates through surface latent heat flux anomalies by canopy evaporation and transpiration and their effect on the mid-tropospheric African easterly jet, whereas the effects of vegetation changes on surface albedo and local water recycling play a negligible role. Even though CCSM3-DGVM simulates a positive vegetation-precipitation feedback in the North African region, this feedback is not strong enough to produce multiple equilibrium climate-ecosystem states on a regional scale.
    Schlagwort(e): Center for Marine Environmental Sciences; Description; File format; File name; File size; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; MARUM; Model; Sahara-Sahel_region; Uniform resource locator/link to model result file
    Materialart: Dataset
    Format: text/tab-separated-values, 30 data points
    Standort Signatur Erwartet Verfügbarkeit
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    DATEN PANGAEA
  • 61
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    Basic and other measurements of radiation at station Tateno (2001-04) (2010)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, maximum; Diffuse radiation, minimum; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, maximum; Direct radiation, minimum; Direct radiation, standard deviation; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; Japan; Long-wave downward radiation; Long-wave downward radiation, maximum; Long-wave downward radiation, minimum; Long-wave downward radiation, standard deviation; Long-wave upward radiation; Long-wave upward radiation, maximum; Long-wave upward radiation, minimum; Long-wave upward radiation, standard deviation; Monitoring station; MONS; Net radiation; Net radiation, maximum; Net radiation, minimum; Net radiation, standard deviation; Pyranometer, Kipp & Zonen, CM21, SN 950236, WRMC No. 16017; Pyranometer, Kipp & Zonen, CM21, SN 960332, WRMC No. 16015; Pyranometer, Kipp & Zonen, CM21, SN 970423, WRMC No. 16019; Pyrgeometer, Eppley, PIR, SN 29460F3, WRMC No. 16009; Pyrgeometer, Eppley, PIR, SN 31714F3, WRMC No. 16021; Pyrheliometer, Kipp & Zonen, CH1, SN 950093, WRMC No. 16011; Radiometer, EKO, CN-11, SN 87057, WRMC No. 16020; Short-wave downward (GLOBAL) radiation; Short-wave downward (GLOBAL) radiation, maximum; Short-wave downward (GLOBAL) radiation, minimum; Short-wave downward (GLOBAL) radiation, standard deviation; Short-wave upward (REFLEX) radiation; Short-wave upward (REFLEX) radiation, maximum; Short-wave upward (REFLEX) radiation, minimum; Short-wave upward (REFLEX) radiation, standard deviation; Station pressure; TAT; Tateno; Thermometer
    Materialart: Dataset
    Format: text/tab-separated-values, 1211234 data points
    Standort Signatur Erwartet Verfügbarkeit
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    DATEN PANGAEA
  • 62
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    (Table S1) Age determination of sediment core MSM05/5_712-1 (2011)
    PANGAEA
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): Age; Age, 14C AMS; Age, 14C milieu/reservoir corrected; Age, comment; Age, dated; Age, dated standard deviation; Calendar age; Calendar age, standard deviation; Comment; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Fram Strait; Giant box corer; GKG; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; Maria S. Merian; MSM05/5; MSM05/5_712-1; Sample, optional label/labor no
    Materialart: Dataset
    Format: text/tab-separated-values, 38 data points
    Standort Signatur Erwartet Verfügbarkeit
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    DATEN PANGAEA
  • 63
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    Basic and other measurements of radiation at station Tateno (2001-02) (2010)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, maximum; Diffuse radiation, minimum; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, maximum; Direct radiation, minimum; Direct radiation, standard deviation; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; Japan; Long-wave downward radiation; Long-wave downward radiation, maximum; Long-wave downward radiation, minimum; Long-wave downward radiation, standard deviation; Long-wave upward radiation; Long-wave upward radiation, maximum; Long-wave upward radiation, minimum; Long-wave upward radiation, standard deviation; Monitoring station; MONS; Net radiation; Net radiation, maximum; Net radiation, minimum; Net radiation, standard deviation; Pyranometer, Kipp & Zonen, CM21, SN 950236, WRMC No. 16017; Pyranometer, Kipp & Zonen, CM21, SN 960332, WRMC No. 16015; Pyranometer, Kipp & Zonen, CM21, SN 970423, WRMC No. 16019; Pyrgeometer, Eppley, PIR, SN 29460F3, WRMC No. 16009; Pyrgeometer, Eppley, PIR, SN 31714F3, WRMC No. 16021; Pyrheliometer, Kipp & Zonen, CH1, SN 950093, WRMC No. 16011; Radiometer, EKO, CN-11, SN 87057, WRMC No. 16020; Short-wave downward (GLOBAL) radiation; Short-wave downward (GLOBAL) radiation, maximum; Short-wave downward (GLOBAL) radiation, minimum; Short-wave downward (GLOBAL) radiation, standard deviation; Short-wave upward (REFLEX) radiation; Short-wave upward (REFLEX) radiation, maximum; Short-wave upward (REFLEX) radiation, minimum; Short-wave upward (REFLEX) radiation, standard deviation; Station pressure; TAT; Tateno; Thermometer
    Materialart: Dataset
    Format: text/tab-separated-values, 1130358 data points
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
    DATEN PANGAEA
  • 64
    facet.materialart.
    Unbekannt
    Basic and other measurements of radiation at station Tateno (2002-04) (2010)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, maximum; Diffuse radiation, minimum; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, maximum; Direct radiation, minimum; Direct radiation, standard deviation; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; Japan; Long-wave downward radiation; Long-wave downward radiation, maximum; Long-wave downward radiation, minimum; Long-wave downward radiation, standard deviation; Long-wave upward radiation; Long-wave upward radiation, maximum; Long-wave upward radiation, minimum; Long-wave upward radiation, standard deviation; Monitoring station; MONS; Net radiation; Net radiation, maximum; Net radiation, minimum; Net radiation, standard deviation; Pyranometer, Kipp & Zonen, CM21, SN 950236, WRMC No. 16017; Pyranometer, Kipp & Zonen, CM21, SN 960332, WRMC No. 16015; Pyranometer, Kipp & Zonen, CM21, SN 970423, WRMC No. 16019; Pyrgeometer, Eppley, PIR, SN 30700F3, WRMC No. 16010; Pyrgeometer, Eppley, PIR, SN 32205F3, WRMC No. 16022; Pyrheliometer, Kipp & Zonen, CH1, SN 950093, WRMC No. 16011; Radiometer, EKO, CN-11, SN 87057, WRMC No. 16020; Short-wave downward (GLOBAL) radiation; Short-wave downward (GLOBAL) radiation, maximum; Short-wave downward (GLOBAL) radiation, minimum; Short-wave downward (GLOBAL) radiation, standard deviation; Short-wave upward (REFLEX) radiation; Short-wave upward (REFLEX) radiation, maximum; Short-wave upward (REFLEX) radiation, minimum; Short-wave upward (REFLEX) radiation, standard deviation; Station pressure; TAT; Tateno; Thermometer
    Materialart: Dataset
    Format: text/tab-separated-values, 1199786 data points
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
    DATEN PANGAEA
  • 65
    facet.materialart.
    Unbekannt
    Basic and other measurements of radiation at station Tateno (2002-03) (2010)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, maximum; Diffuse radiation, minimum; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, maximum; Direct radiation, minimum; Direct radiation, standard deviation; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; Japan; Long-wave downward radiation; Long-wave downward radiation, maximum; Long-wave downward radiation, minimum; Long-wave downward radiation, standard deviation; Long-wave upward radiation; Long-wave upward radiation, maximum; Long-wave upward radiation, minimum; Long-wave upward radiation, standard deviation; Monitoring station; MONS; Net radiation; Net radiation, maximum; Net radiation, minimum; Net radiation, standard deviation; Pyranometer, Kipp & Zonen, CM21, SN 950236, WRMC No. 16017; Pyranometer, Kipp & Zonen, CM21, SN 960332, WRMC No. 16015; Pyranometer, Kipp & Zonen, CM21, SN 970423, WRMC No. 16019; Pyrgeometer, Eppley, PIR, SN 30700F3, WRMC No. 16010; Pyrgeometer, Eppley, PIR, SN 32205F3, WRMC No. 16022; Pyrheliometer, Kipp & Zonen, CH1, SN 950093, WRMC No. 16011; Radiometer, EKO, CN-11, SN 87057, WRMC No. 16020; Short-wave downward (GLOBAL) radiation; Short-wave downward (GLOBAL) radiation, maximum; Short-wave downward (GLOBAL) radiation, minimum; Short-wave downward (GLOBAL) radiation, standard deviation; Short-wave upward (REFLEX) radiation; Short-wave upward (REFLEX) radiation, maximum; Short-wave upward (REFLEX) radiation, minimum; Short-wave upward (REFLEX) radiation, standard deviation; Station pressure; TAT; Tateno; Thermometer
    Materialart: Dataset
    Format: text/tab-separated-values, 1250648 data points
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
    DATEN PANGAEA
  • 66
    facet.materialart.
    Unbekannt
    Basic and other measurements of radiation at station Tateno (2002-10) (2010)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, maximum; Diffuse radiation, minimum; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, maximum; Direct radiation, minimum; Direct radiation, standard deviation; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; Japan; Long-wave downward radiation; Long-wave downward radiation, maximum; Long-wave downward radiation, minimum; Long-wave downward radiation, standard deviation; Long-wave upward radiation; Long-wave upward radiation, maximum; Long-wave upward radiation, minimum; Long-wave upward radiation, standard deviation; Monitoring station; MONS; Net radiation; Net radiation, maximum; Net radiation, minimum; Net radiation, standard deviation; Pyranometer, Kipp & Zonen, CM21, SN 950236, WRMC No. 16017; Pyranometer, Kipp & Zonen, CM21, SN 960332, WRMC No. 16015; Pyranometer, Kipp & Zonen, CM21, SN 970423, WRMC No. 16019; Pyrgeometer, Eppley, PIR, SN 30700F3, WRMC No. 16010; Pyrgeometer, Eppley, PIR, SN 32205F3, WRMC No. 16022; Pyrheliometer, Kipp & Zonen, CH1, SN 950093, WRMC No. 16011; Radiometer, EKO, CN-11, SN 87057, WRMC No. 16020; Short-wave downward (GLOBAL) radiation; Short-wave downward (GLOBAL) radiation, maximum; Short-wave downward (GLOBAL) radiation, minimum; Short-wave downward (GLOBAL) radiation, standard deviation; Short-wave upward (REFLEX) radiation; Short-wave upward (REFLEX) radiation, maximum; Short-wave upward (REFLEX) radiation, minimum; Short-wave upward (REFLEX) radiation, standard deviation; Station pressure; TAT; Tateno; Thermometer
    Materialart: Dataset
    Format: text/tab-separated-values, 1252089 data points
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
    DATEN PANGAEA
  • 67
    facet.materialart.
    Unbekannt
    Basic and other measurements of radiation at station Tateno (2003-04) (2010)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, maximum; Diffuse radiation, minimum; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, maximum; Direct radiation, minimum; Direct radiation, standard deviation; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; Japan; Long-wave downward radiation; Long-wave downward radiation, maximum; Long-wave downward radiation, minimum; Long-wave downward radiation, standard deviation; Long-wave upward radiation; Long-wave upward radiation, maximum; Long-wave upward radiation, minimum; Long-wave upward radiation, standard deviation; Monitoring station; MONS; Net radiation; Net radiation, maximum; Net radiation, minimum; Net radiation, standard deviation; Pyranometer, Kipp & Zonen, CM21, SN 950236, WRMC No. 16017; Pyranometer, Kipp & Zonen, CM21, SN 960332, WRMC No. 16015; Pyranometer, Kipp & Zonen, CM21, SN 970423, WRMC No. 16019; Pyrgeometer, Eppley, PIR, SN 30700F3, WRMC No. 16010; Pyrgeometer, Eppley, PIR, SN 32205F3, WRMC No. 16022; Pyrheliometer, Kipp & Zonen, CH1, SN 950093, WRMC No. 16011; Radiometer, EKO, CN-11, SN 87057, WRMC No. 16020; Short-wave downward (GLOBAL) radiation; Short-wave downward (GLOBAL) radiation, maximum; Short-wave downward (GLOBAL) radiation, minimum; Short-wave downward (GLOBAL) radiation, standard deviation; Short-wave upward (REFLEX) radiation; Short-wave upward (REFLEX) radiation, maximum; Short-wave upward (REFLEX) radiation, minimum; Short-wave upward (REFLEX) radiation, standard deviation; Station pressure; TAT; Tateno; Thermometer
    Materialart: Dataset
    Format: text/tab-separated-values, 1208164 data points
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
    DATEN PANGAEA
  • 68
    facet.materialart.
    Unbekannt
    Basic and other measurements of radiation at station Tateno (2003-08) (2010)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, maximum; Diffuse radiation, minimum; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, maximum; Direct radiation, minimum; Direct radiation, standard deviation; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; Japan; Long-wave downward radiation; Long-wave downward radiation, maximum; Long-wave downward radiation, minimum; Long-wave downward radiation, standard deviation; Long-wave upward radiation; Long-wave upward radiation, maximum; Long-wave upward radiation, minimum; Long-wave upward radiation, standard deviation; Monitoring station; MONS; Net radiation; Net radiation, maximum; Net radiation, minimum; Net radiation, standard deviation; Pyranometer, Kipp & Zonen, CM21, SN 950236, WRMC No. 16017; Pyranometer, Kipp & Zonen, CM21, SN 960332, WRMC No. 16015; Pyranometer, Kipp & Zonen, CM21, SN 970423, WRMC No. 16019; Pyrgeometer, Eppley, PIR, SN 30700F3, WRMC No. 16010; Pyrgeometer, Eppley, PIR, SN 32205F3, WRMC No. 16022; Pyrheliometer, Kipp & Zonen, CH1, SN 950093, WRMC No. 16011; Radiometer, EKO, CN-11, SN 87057, WRMC No. 16020; Short-wave downward (GLOBAL) radiation; Short-wave downward (GLOBAL) radiation, maximum; Short-wave downward (GLOBAL) radiation, minimum; Short-wave downward (GLOBAL) radiation, standard deviation; Short-wave upward (REFLEX) radiation; Short-wave upward (REFLEX) radiation, maximum; Short-wave upward (REFLEX) radiation, minimum; Short-wave upward (REFLEX) radiation, standard deviation; Station pressure; TAT; Tateno; Thermometer
    Materialart: Dataset
    Format: text/tab-separated-values, 1249072 data points
    Standort Signatur Erwartet Verfügbarkeit
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    DATEN PANGAEA
  • 69
    facet.materialart.
    Unbekannt
    Basic and other measurements of radiation at station Tateno (2010-10) (2011)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, maximum; Diffuse radiation, minimum; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, maximum; Direct radiation, minimum; Direct radiation, standard deviation; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; Japan; Long-wave downward radiation; Long-wave downward radiation, maximum; Long-wave downward radiation, minimum; Long-wave downward radiation, standard deviation; Long-wave upward radiation; Long-wave upward radiation, maximum; Long-wave upward radiation, minimum; Long-wave upward radiation, standard deviation; Monitoring station; MONS; Pyranometer, Kipp & Zonen, CM21, SN 960330, WRMC No. 16013; Pyranometer, Kipp & Zonen, CM21, SN 960331, WRMC No. 16014; Pyranometer, Kipp & Zonen, CM22, SN 010048, WRMC No. 16023; Pyrgeometer, Kipp & Zonen, CG4, SN 010582, WRMC No. 16026; Pyrgeometer, Kipp & Zonen, CG4, SN 030641, WRMC No. 16032; Pyrheliometer, Kipp & Zonen, CH1, SN 950093, WRMC No. 16011; Short-wave downward (GLOBAL) radiation; Short-wave downward (GLOBAL) radiation, maximum; Short-wave downward (GLOBAL) radiation, minimum; Short-wave downward (GLOBAL) radiation, standard deviation; Short-wave upward (REFLEX) radiation; Short-wave upward (REFLEX) radiation, maximum; Short-wave upward (REFLEX) radiation, minimum; Short-wave upward (REFLEX) radiation, standard deviation; Station pressure; TAT; Tateno; Thermometer
    Materialart: Dataset
    Format: text/tab-separated-values, 1073590 data points
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
    DATEN PANGAEA
  • 70
    facet.materialart.
    Unbekannt
    Basic and other measurements of radiation at station Tateno (2004-03) (2011)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, maximum; Diffuse radiation, minimum; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, maximum; Direct radiation, minimum; Direct radiation, standard deviation; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; Japan; Long-wave downward radiation; Long-wave downward radiation, maximum; Long-wave downward radiation, minimum; Long-wave downward radiation, standard deviation; Long-wave upward radiation; Long-wave upward radiation, maximum; Long-wave upward radiation, minimum; Long-wave upward radiation, standard deviation; Monitoring station; MONS; Net radiation; Net radiation, maximum; Net radiation, minimum; Net radiation, standard deviation; Pyranometer, Kipp & Zonen, CM21, SN 960330, WRMC No. 16013; Pyranometer, Kipp & Zonen, CM21, SN 960331, WRMC No. 16014; Pyranometer, Kipp & Zonen, CM22, SN 010048, WRMC No. 16023; Pyrgeometer, Eppley, PIR, SN 30700F3, WRMC No. 16010; Pyrgeometer, Eppley, PIR, SN 32205F3, WRMC No. 16022; Pyrheliometer, Kipp & Zonen, CH1, SN 950093, WRMC No. 16011; Radiometer, EKO, CN-11, SN 87057, WRMC No. 16020; Short-wave downward (GLOBAL) radiation; Short-wave downward (GLOBAL) radiation, maximum; Short-wave downward (GLOBAL) radiation, minimum; Short-wave downward (GLOBAL) radiation, standard deviation; Short-wave upward (REFLEX) radiation; Short-wave upward (REFLEX) radiation, maximum; Short-wave upward (REFLEX) radiation, minimum; Short-wave upward (REFLEX) radiation, standard deviation; Station pressure; TAT; Tateno; Thermometer
    Materialart: Dataset
    Format: text/tab-separated-values, 1249580 data points
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
    DATEN PANGAEA
  • 71
    facet.materialart.
    Unbekannt
    Basic and other measurements of radiation at station Tateno (2004-05) (2011)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, maximum; Diffuse radiation, minimum; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, maximum; Direct radiation, minimum; Direct radiation, standard deviation; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; Japan; Long-wave downward radiation; Long-wave downward radiation, maximum; Long-wave downward radiation, minimum; Long-wave downward radiation, standard deviation; Long-wave upward radiation; Long-wave upward radiation, maximum; Long-wave upward radiation, minimum; Long-wave upward radiation, standard deviation; Monitoring station; MONS; Net radiation; Net radiation, maximum; Net radiation, minimum; Net radiation, standard deviation; Pyranometer, Kipp & Zonen, CM21, SN 960330, WRMC No. 16013; Pyranometer, Kipp & Zonen, CM21, SN 960331, WRMC No. 16014; Pyranometer, Kipp & Zonen, CM22, SN 010048, WRMC No. 16023; Pyrgeometer, Eppley, PIR, SN 30700F3, WRMC No. 16010; Pyrgeometer, Eppley, PIR, SN 32205F3, WRMC No. 16022; Pyrheliometer, Kipp & Zonen, CH1, SN 950093, WRMC No. 16011; Radiometer, EKO, CN-11, SN 87057, WRMC No. 16020; Short-wave downward (GLOBAL) radiation; Short-wave downward (GLOBAL) radiation, maximum; Short-wave downward (GLOBAL) radiation, minimum; Short-wave downward (GLOBAL) radiation, standard deviation; Short-wave upward (REFLEX) radiation; Short-wave upward (REFLEX) radiation, maximum; Short-wave upward (REFLEX) radiation, minimum; Short-wave upward (REFLEX) radiation, standard deviation; Station pressure; TAT; Tateno; Thermometer
    Materialart: Dataset
    Format: text/tab-separated-values, 1208112 data points
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
    DATEN PANGAEA
  • 72
    facet.materialart.
    Unbekannt
    Basic and other measurements of radiation at station Tateno (2010-05) (2010)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, maximum; Diffuse radiation, minimum; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, maximum; Direct radiation, minimum; Direct radiation, standard deviation; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; Japan; Long-wave downward radiation; Long-wave downward radiation, maximum; Long-wave downward radiation, minimum; Long-wave downward radiation, standard deviation; Long-wave upward radiation; Long-wave upward radiation, maximum; Long-wave upward radiation, minimum; Long-wave upward radiation, standard deviation; Monitoring station; MONS; Pyranometer, Kipp & Zonen, CM21, SN 960330, WRMC No. 16013; Pyranometer, Kipp & Zonen, CM21, SN 960331, WRMC No. 16014; Pyranometer, Kipp & Zonen, CM22, SN 010048, WRMC No. 16023; Pyrgeometer, Kipp & Zonen, CG4, SN 010582, WRMC No. 16026; Pyrgeometer, Kipp & Zonen, CG4, SN 030641, WRMC No. 16032; Pyrheliometer, Kipp & Zonen, CH1, SN 950093, WRMC No. 16011; Short-wave downward (GLOBAL) radiation; Short-wave downward (GLOBAL) radiation, maximum; Short-wave downward (GLOBAL) radiation, minimum; Short-wave downward (GLOBAL) radiation, standard deviation; Short-wave upward (REFLEX) radiation; Short-wave upward (REFLEX) radiation, maximum; Short-wave upward (REFLEX) radiation, minimum; Short-wave upward (REFLEX) radiation, standard deviation; Station pressure; TAT; Tateno; Thermometer
    Materialart: Dataset
    Format: text/tab-separated-values, 1073588 data points
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
    DATEN PANGAEA
  • 73
    facet.materialart.
    Unbekannt
    Basic and other measurements of radiation at station Tateno (2010-08) (2010)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, maximum; Diffuse radiation, minimum; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, maximum; Direct radiation, minimum; Direct radiation, standard deviation; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; Japan; Long-wave downward radiation; Long-wave downward radiation, maximum; Long-wave downward radiation, minimum; Long-wave downward radiation, standard deviation; Long-wave upward radiation; Long-wave upward radiation, maximum; Long-wave upward radiation, minimum; Long-wave upward radiation, standard deviation; Monitoring station; MONS; Pyranometer, Kipp & Zonen, CM21, SN 960330, WRMC No. 16013; Pyranometer, Kipp & Zonen, CM21, SN 960331, WRMC No. 16014; Pyranometer, Kipp & Zonen, CM22, SN 010048, WRMC No. 16023; Pyrgeometer, Kipp & Zonen, CG4, SN 010582, WRMC No. 16026; Pyrgeometer, Kipp & Zonen, CG4, SN 030641, WRMC No. 16032; Pyrheliometer, Kipp & Zonen, CH1, SN 950093, WRMC No. 16011; Short-wave downward (GLOBAL) radiation; Short-wave downward (GLOBAL) radiation, maximum; Short-wave downward (GLOBAL) radiation, minimum; Short-wave downward (GLOBAL) radiation, standard deviation; Short-wave upward (REFLEX) radiation; Short-wave upward (REFLEX) radiation, maximum; Short-wave upward (REFLEX) radiation, minimum; Short-wave upward (REFLEX) radiation, standard deviation; Station pressure; TAT; Tateno; Thermometer
    Materialart: Dataset
    Format: text/tab-separated-values, 1073592 data points
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
    DATEN PANGAEA
  • 74
    facet.materialart.
    Unbekannt
    (Figure 6) Sr/Ca and stable isotope records across a single thecal wall of coral sample BON-9-A (2010)
    PANGAEA
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): BON-9-A; CaribClim_Coral_2006; Center for Marine Environmental Sciences; Diploria strigosa, Strontium/Calcium ratio; Diploria strigosa, δ13C; Diploria strigosa, δ18O; DISTANCE; DRILL; Drilling/drill rig; ICP-OES, Perkin-Elmer, Optima 3300R; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; MARUM; Mass spectrometer Finnigan MAT 251; Southern Caribbean Sea, Bonaire; x
    Materialart: Dataset
    Format: text/tab-separated-values, 433 data points
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
    DATEN PANGAEA
  • 75
    facet.materialart.
    Unbekannt
    (Figure 7) Sr/Ca and stable isotope anomalies across the thecal wall of three different Diploria strigosa coral colonies (2010)
    PANGAEA
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): BON-9-A; Calculated; CaribClim_Coral_2006; Center for Marine Environmental Sciences; Comment; Diploria strigosa, δ13C; Diploria strigosa, δ18O; DISTANCE; DRILL; Drilling/drill rig; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; MARUM; Southern Caribbean Sea, Bonaire; Standard error; Strontium/Calcium ratio
    Materialart: Dataset
    Format: text/tab-separated-values, 101 data points
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
    DATEN PANGAEA
  • 76
    facet.materialart.
    Unbekannt
    Physical oceanography at CTD station MSM05/5_713-1 (2011)
    PANGAEA
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): CTD, Sea-Bird SBE 911plus; CTD/Rosette; CTD-RO; DEPTH, water; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; Maria S. Merian; MSM05/5; MSM05/5_713-1; North Greenland Sea; Salinity; Temperature, water
    Materialart: Dataset
    Format: text/tab-separated-values, 1198 data points
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
    DATEN PANGAEA
  • 77
    facet.materialart.
    Unbekannt
    Basic and other measurements of radiation at station Tateno (2004-10) (2011)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, maximum; Diffuse radiation, minimum; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, maximum; Direct radiation, minimum; Direct radiation, standard deviation; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; Japan; Long-wave downward radiation; Long-wave downward radiation, maximum; Long-wave downward radiation, minimum; Long-wave downward radiation, standard deviation; Long-wave upward radiation; Long-wave upward radiation, maximum; Long-wave upward radiation, minimum; Long-wave upward radiation, standard deviation; Monitoring station; MONS; Net radiation; Net radiation, maximum; Net radiation, minimum; Net radiation, standard deviation; Pyranometer, Kipp & Zonen, CM21, SN 960330, WRMC No. 16013; Pyranometer, Kipp & Zonen, CM21, SN 960331, WRMC No. 16014; Pyranometer, Kipp & Zonen, CM21, SN 970366, WRMC No. 16024; Pyrgeometer, Eppley, PIR, SN 30700F3, WRMC No. 16010; Pyrgeometer, Eppley, PIR, SN 31714F3, WRMC No. 16021; Pyrheliometer, Kipp & Zonen, CH1, SN 950093, WRMC No. 16011; Radiometer, EKO, CN-11, SN 87057, WRMC No. 16020; Short-wave downward (GLOBAL) radiation; Short-wave downward (GLOBAL) radiation, maximum; Short-wave downward (GLOBAL) radiation, minimum; Short-wave downward (GLOBAL) radiation, standard deviation; Short-wave upward (REFLEX) radiation; Short-wave upward (REFLEX) radiation, maximum; Short-wave upward (REFLEX) radiation, minimum; Short-wave upward (REFLEX) radiation, standard deviation; Station pressure; TAT; Tateno; Thermometer
    Materialart: Dataset
    Format: text/tab-separated-values, 1252120 data points
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
    DATEN PANGAEA
  • 78
    facet.materialart.
    Unbekannt
    Basic and other measurements of radiation at station Tateno (2005-03) (2011)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, maximum; Diffuse radiation, minimum; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, maximum; Direct radiation, minimum; Direct radiation, standard deviation; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; Japan; Long-wave downward radiation; Long-wave downward radiation, maximum; Long-wave downward radiation, minimum; Long-wave downward radiation, standard deviation; Long-wave upward radiation; Long-wave upward radiation, maximum; Long-wave upward radiation, minimum; Long-wave upward radiation, standard deviation; Monitoring station; MONS; Net radiation; Net radiation, maximum; Net radiation, minimum; Net radiation, standard deviation; Pyranometer, Kipp & Zonen, CM21, SN 960330, WRMC No. 16013; Pyranometer, Kipp & Zonen, CM21, SN 960331, WRMC No. 16014; Pyranometer, Kipp & Zonen, CM22, SN 010048, WRMC No. 16023; Pyrgeometer, Eppley, PIR, SN 30700F3, WRMC No. 16010; Pyrgeometer, Eppley, PIR, SN 31714F3, WRMC No. 16021; Pyrheliometer, Kipp & Zonen, CH1, SN 950093, WRMC No. 16011; Radiometer, EKO, CN-11, SN 87057, WRMC No. 16020; Short-wave downward (GLOBAL) radiation; Short-wave downward (GLOBAL) radiation, maximum; Short-wave downward (GLOBAL) radiation, minimum; Short-wave downward (GLOBAL) radiation, standard deviation; Short-wave upward (REFLEX) radiation; Short-wave upward (REFLEX) radiation, maximum; Short-wave upward (REFLEX) radiation, minimum; Short-wave upward (REFLEX) radiation, standard deviation; Station pressure; TAT; Tateno; Thermometer
    Materialart: Dataset
    Format: text/tab-separated-values, 1206275 data points
    Standort Signatur Erwartet Verfügbarkeit
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    DATEN PANGAEA
  • 79
    facet.materialart.
    Unbekannt
    Basic and other measurements of radiation at station Tateno (2005-07) (2011)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, maximum; Diffuse radiation, minimum; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, maximum; Direct radiation, minimum; Direct radiation, standard deviation; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; Japan; Long-wave downward radiation; Long-wave downward radiation, maximum; Long-wave downward radiation, minimum; Long-wave downward radiation, standard deviation; Long-wave upward radiation; Long-wave upward radiation, maximum; Long-wave upward radiation, minimum; Long-wave upward radiation, standard deviation; Monitoring station; MONS; Net radiation; Net radiation, maximum; Net radiation, minimum; Net radiation, standard deviation; Pyranometer, Kipp & Zonen, CM21, SN 960330, WRMC No. 16013; Pyranometer, Kipp & Zonen, CM21, SN 960331, WRMC No. 16014; Pyranometer, Kipp & Zonen, CM22, SN 010048, WRMC No. 16023; Pyrgeometer, Eppley, PIR, SN 30700F3, WRMC No. 16010; Pyrgeometer, Eppley, PIR, SN 31714F3, WRMC No. 16021; Pyrheliometer, Kipp & Zonen, CH1, SN 950093, WRMC No. 16011; Radiometer, EKO, CN-11, SN 87057, WRMC No. 16020; Short-wave downward (GLOBAL) radiation; Short-wave downward (GLOBAL) radiation, maximum; Short-wave downward (GLOBAL) radiation, minimum; Short-wave downward (GLOBAL) radiation, standard deviation; Short-wave upward (REFLEX) radiation; Short-wave upward (REFLEX) radiation, maximum; Short-wave upward (REFLEX) radiation, minimum; Short-wave upward (REFLEX) radiation, standard deviation; Station pressure; TAT; Tateno; Thermometer
    Materialart: Dataset
    Format: text/tab-separated-values, 1252128 data points
    Standort Signatur Erwartet Verfügbarkeit
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    DATEN PANGAEA
  • 80
    facet.materialart.
    Unbekannt
    Basic and other measurements of radiation at station Tateno (2005-10) (2011)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, maximum; Diffuse radiation, minimum; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, maximum; Direct radiation, minimum; Direct radiation, standard deviation; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; Japan; Long-wave downward radiation; Long-wave downward radiation, maximum; Long-wave downward radiation, minimum; Long-wave downward radiation, standard deviation; Long-wave upward radiation; Long-wave upward radiation, maximum; Long-wave upward radiation, minimum; Long-wave upward radiation, standard deviation; Monitoring station; MONS; Net radiation; Net radiation, maximum; Net radiation, minimum; Net radiation, standard deviation; Pyranometer, Kipp & Zonen, CM21, SN 960331, WRMC No. 16014; Pyranometer, Kipp & Zonen, CM21, SN 960332, WRMC No. 16015; Pyranometer, Kipp & Zonen, CM22, SN 010048, WRMC No. 16023; Pyrgeometer, Eppley, PIR, SN 29460F3, WRMC No. 16009; Pyrgeometer, Eppley, PIR, SN 31714F3, WRMC No. 16021; Pyrheliometer, Kipp & Zonen, CH1, SN 950093, WRMC No. 16011; Radiometer, EKO, CN-11, SN 87057, WRMC No. 16020; Short-wave downward (GLOBAL) radiation; Short-wave downward (GLOBAL) radiation, maximum; Short-wave downward (GLOBAL) radiation, minimum; Short-wave downward (GLOBAL) radiation, standard deviation; Short-wave upward (REFLEX) radiation; Short-wave upward (REFLEX) radiation, maximum; Short-wave upward (REFLEX) radiation, minimum; Short-wave upward (REFLEX) radiation, standard deviation; Station pressure; TAT; Tateno; Thermometer
    Materialart: Dataset
    Format: text/tab-separated-values, 1238624 data points
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
    DATEN PANGAEA
  • 81
    facet.materialart.
    Unbekannt
    Basic and other measurements of radiation at station Tateno (2006-02) (2011)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, maximum; Diffuse radiation, minimum; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, maximum; Direct radiation, minimum; Direct radiation, standard deviation; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; Japan; Long-wave downward radiation; Long-wave downward radiation, maximum; Long-wave downward radiation, minimum; Long-wave downward radiation, standard deviation; Long-wave upward radiation; Long-wave upward radiation, maximum; Long-wave upward radiation, minimum; Long-wave upward radiation, standard deviation; Monitoring station; MONS; Net radiation; Net radiation, maximum; Net radiation, minimum; Net radiation, standard deviation; Pyranometer, Kipp & Zonen, CM21, SN 960331, WRMC No. 16014; Pyranometer, Kipp & Zonen, CM21, SN 960332, WRMC No. 16015; Pyranometer, Kipp & Zonen, CM22, SN 010048, WRMC No. 16023; Pyrgeometer, Eppley, PIR, SN 29460F3, WRMC No. 16009; Pyrgeometer, Eppley, PIR, SN 31714F3, WRMC No. 16021; Pyrheliometer, Kipp & Zonen, CH1, SN 950093, WRMC No. 16011; Radiometer, EKO, CN-11, SN 87057, WRMC No. 16020; Short-wave downward (GLOBAL) radiation; Short-wave downward (GLOBAL) radiation, maximum; Short-wave downward (GLOBAL) radiation, minimum; Short-wave downward (GLOBAL) radiation, standard deviation; Short-wave upward (REFLEX) radiation; Short-wave upward (REFLEX) radiation, maximum; Short-wave upward (REFLEX) radiation, minimum; Short-wave upward (REFLEX) radiation, standard deviation; Station pressure; TAT; Tateno; Thermometer
    Materialart: Dataset
    Format: text/tab-separated-values, 1130128 data points
    Standort Signatur Erwartet Verfügbarkeit
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    DATEN PANGAEA
  • 82
    facet.materialart.
    Unbekannt
    Basic and other measurements of radiation at station Tateno (2006-03) (2011)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, maximum; Diffuse radiation, minimum; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, maximum; Direct radiation, minimum; Direct radiation, standard deviation; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; Japan; Long-wave downward radiation; Long-wave downward radiation, maximum; Long-wave downward radiation, minimum; Long-wave downward radiation, standard deviation; Long-wave upward radiation; Long-wave upward radiation, maximum; Long-wave upward radiation, minimum; Long-wave upward radiation, standard deviation; Monitoring station; MONS; Net radiation; Net radiation, maximum; Net radiation, minimum; Net radiation, standard deviation; Pyranometer, Kipp & Zonen, CM21, SN 960331, WRMC No. 16014; Pyranometer, Kipp & Zonen, CM21, SN 960332, WRMC No. 16015; Pyranometer, Kipp & Zonen, CM22, SN 010048, WRMC No. 16023; Pyrgeometer, Eppley, PIR, SN 29460F3, WRMC No. 16009; Pyrgeometer, Eppley, PIR, SN 31714F3, WRMC No. 16021; Pyrheliometer, Kipp & Zonen, CH1, SN 950093, WRMC No. 16011; Radiometer, EKO, CN-11, SN 87057, WRMC No. 16020; Short-wave downward (GLOBAL) radiation; Short-wave downward (GLOBAL) radiation, maximum; Short-wave downward (GLOBAL) radiation, minimum; Short-wave downward (GLOBAL) radiation, standard deviation; Short-wave upward (REFLEX) radiation; Short-wave upward (REFLEX) radiation, maximum; Short-wave upward (REFLEX) radiation, minimum; Short-wave upward (REFLEX) radiation, standard deviation; Station pressure; TAT; Tateno; Thermometer
    Materialart: Dataset
    Format: text/tab-separated-values, 1251532 data points
    Standort Signatur Erwartet Verfügbarkeit
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    DATEN PANGAEA
  • 83
    facet.materialart.
    Unbekannt
    Basic and other measurements of radiation at station Tateno (2010-09) (2010)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, maximum; Diffuse radiation, minimum; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, maximum; Direct radiation, minimum; Direct radiation, standard deviation; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; Japan; Long-wave downward radiation; Long-wave downward radiation, maximum; Long-wave downward radiation, minimum; Long-wave downward radiation, standard deviation; Long-wave upward radiation; Long-wave upward radiation, maximum; Long-wave upward radiation, minimum; Long-wave upward radiation, standard deviation; Monitoring station; MONS; Pyranometer, Kipp & Zonen, CM21, SN 960330, WRMC No. 16013; Pyranometer, Kipp & Zonen, CM21, SN 960331, WRMC No. 16014; Pyranometer, Kipp & Zonen, CM22, SN 010048, WRMC No. 16023; Pyrgeometer, Kipp & Zonen, CG4, SN 010582, WRMC No. 16026; Pyrgeometer, Kipp & Zonen, CG4, SN 030641, WRMC No. 16032; Pyrheliometer, Kipp & Zonen, CH1, SN 950093, WRMC No. 16011; Short-wave downward (GLOBAL) radiation; Short-wave downward (GLOBAL) radiation, maximum; Short-wave downward (GLOBAL) radiation, minimum; Short-wave downward (GLOBAL) radiation, standard deviation; Short-wave upward (REFLEX) radiation; Short-wave upward (REFLEX) radiation, maximum; Short-wave upward (REFLEX) radiation, minimum; Short-wave upward (REFLEX) radiation, standard deviation; Station pressure; TAT; Tateno; Thermometer
    Materialart: Dataset
    Format: text/tab-separated-values, 1038760 data points
    Standort Signatur Erwartet Verfügbarkeit
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    DATEN PANGAEA
  • 84
    facet.materialart.
    Unbekannt
    Physical oceanography at CTD station JM06-WP-02 (2011)
    PANGAEA
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): CTD, Sea-Bird SBE 911plus; CTD/Rosette; CTD-RO; DEPTH, water; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; Jan Mayen; JM06-WP; JM06-WP-02; Salinity; Temperature, water; WarmPast 2006
    Materialart: Dataset
    Format: text/tab-separated-values, 1198 data points
    Standort Signatur Erwartet Verfügbarkeit
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    DATEN PANGAEA
  • 85
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    Unbekannt
    Chemical composition of surface sediment samples from the Eastern Mediterranean Sea (2010)
    PANGAEA
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): 101; 101-105; 106-111; 107; 111; 112-116; 116; 117-122; 118; 123-126; 137-139; 140-142; 143-148; 149-154; 155-162; 163-170; 171-179; 180-187; 188-194; 560; 561; 562; 563; 564; 565; 566; 569; 570; 571; 572; 573; 574; 575; 576; 577; 578; 579; 580; 581; 582; 584; 585; 586; 589; 590; 592; 594; 596; 599; 601; 602; 604; 666; 667; 668; 670; 671; 672; 673; 674; 676; 677; 678; 680; 681; 682; 683; 684; 685; 686; 687; 689; 690; 691; 692; 693; 694; 695; 696; 697; 699; 700; 701; 702; 703; 704; 705; 706; 707; 708; 709; 710; 712; 713; 714; 716; 717; 718; 719; 80; 82; 85; Alkenone, unsaturation index UK37; Aluminium; Amino acid, total hydrolysable; Amino acid analyser, Biochrom 30; Amino acids/hexosamines ratio; Barium; Calcium; Calcium carbonate; Carbon, inorganic, total; Carbon, organic, total; Carbon, total; Copper; Cyprus; Degradation index of amino acids (Dauwe et al., 1999); DEPTH, sediment/rock; Eastern Mediterranean, Continental slope off Israel; Element analyser CNS, Carlo Erba NA1500; Elevation of event; Eratosthenes Seamount; Event label; Gargano Promontory; Gas chromatography, Fisions 8000; GeoB10701-4; GeoB10702-3; GeoB10703-3; GeoB10704-3; GeoB10705-3; GeoB10706-3; GeoB10707-4; GeoB10708-3; GeoB10710-4; GeoB10711-3; GeoB10712-3; GeoB10713-3; GeoB10714-3; GeoB10715-3; GeoB10716-3; GeoB10717-3; GeoB10718-3; GeoB10719-3; GeoB10720-5; GeoB10721-3; GeoB10722-3; GeoB10723-3; GeoB10724-3; GeoB10725-3; GeoB10726-3; GeoB10727-3; GeoB10728-3; GeoB10729-4; GeoB10730-3; GeoB10731-3; GeoB10732-3; GeoB10733-3; GeoB10734-3; GeoB10735-3; GeoB10736-3; GeoB10737-3; GeoB10738-3; GeoB10739-3; GeoB10740-3; GeoB10741-3; GeoB10742-3; GeoB10743-3; GeoB10744-3; GeoB10746-3; GeoB10747-3; GeoB10748-3; GeoB10749-3; GeoB7704-1; GeoB7705-1; GeoB7706-2; GeoB7714-1; GeoB7718-1; GeoB7720-1; GeoB7723-2; GeoB7725-2; Globigerinoides ruber, δ13C; Globigerinoides ruber, δ18O; Gravity corer (Kiel type); Greece; Gulf of Manfredonia; Gulf of Taranto; Haifa; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; Iron; Latitude of event; Lead; Longitude of event; Lybia; M40/4; M40/4_MUC65; M40/4_MUC66; M40/4_MUC67; M40/4_MUC68; M40/4_MUC69; M40/4_MUC70; M40/4_MUC71; M40/4_MUC72; M40/4_MUC73; M40/4_MUC74; M40/4_MUC75; M40/4_MUC76-2; M40/4_MUC76-3; M40/4_MUC77A; M40/4_MUC77B; M40/4_MUC78-2; M40/4_MUC79; M40/4_MUC81; M40/4_MUC82; M40/4_MUC84; M40/4_MUC85; M40/4_MUC86; M40/4_MUC87; M40/4_MUC88; M40/4_MUC89; M40/4_MUC90; M40/4_MUC91; M40/4_SL80; M51/3; M51/3_560-1; M51/3_561-4; M51/3_562-5; M51/3_563-5; M51/3_564-2; M51/3_565-1; M51/3_566-3; M51/3_569-3; M51/3_570-2; M51/3_571; M51/3_572-2; M51/3_573; M51/3_574-2; M51/3_575-6; M51/3_576-3; M51/3_577-1; M51/3_578; M51/3_579; M51/3_580; M51/3_581; M51/3_582; M51/3_584; M51/3_585; M51/3_586; M51/3_589; M51/3_590; M51/3_592; M51/3_594; M51/3_596; M51/3_599; M51/3_601-3; M51/3_602; M51/3_604; M52/2; M71/3; M71/3_H01; M71/3_H02; M71/3_H03; M71/3_H04; M71/3_H05; M71/3_H06; M71/3_H07; M71/3_H11; M71/3_H12; M71/3_Her01; M71/3_Her03; M71/3_ler01; M71/3_Rho02; M71/3_Sk01; Magnesium; Malta; Manganese; Mass spectrometer Finnigan MAT 252; Mass spectrometer VG Prism; Meteor (1986); MUC; MultiCorer; Nile Fan; Nitrogen, total; Phosphorus; POS339; Poseidon; Potassium; Reactivity index of amino acids (Jennerjahn & Ittekkot, 1997); Rubidium; Sample ID; Silicon; SL; Sodium; Strait of Otranto; Strontium; Sulfur, total; Titanium; Turkey; X-ray fluorescence spectrometer (Panalytical MagixPRO); Zinc; Zirconium; Zyprus; δ15N
    Materialart: Dataset
    Format: text/tab-separated-values, 3130 data points
    Standort Signatur Erwartet Verfügbarkeit
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    DATEN PANGAEA
  • 86
    facet.materialart.
    Unbekannt
    Raw data from 1912 AD Bonaire coral, sample BON-9-A (2011)
    PANGAEA
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): Attributed to extreme Sr/Ca values of any single year; BON-9-A; CaribClim_Coral_2006; Center for Marine Environmental Sciences; Diploria strigosa, Strontium/Calcium ratio; Diploria strigosa, δ18O; DISTANCE; DRILL; Drilling/drill rig; Estimated based on subannual extension-rate and tie points; ICP-OES, Perkin-Elmer, Optima 3300R; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; Internal coral chronology; MARUM; Mass spectrometer Finnigan MAT 251; referred samples; Sample ID; Southern Caribbean Sea, Bonaire; Tie point
    Materialart: Dataset
    Format: text/tab-separated-values, 1548 data points
    Standort Signatur Erwartet Verfügbarkeit
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    DATEN PANGAEA
  • 87
    facet.materialart.
    Unbekannt
    Distribution of planktic foraminifera and calculated sea surface temperature of sediment core MSM05/5_712-1 (2011)
    PANGAEA
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): Accumulation rate, planktic foraminifera by number; Age; AGE; Calculated; Counting, foraminifera, planktic; Counting 100-250 µm fraction; Counting 150-250 µm fraction; Density, dry bulk; DEPTH, sediment/rock; Foraminifera, planktic, subpolar; Fram Strait; Giant box corer; GKG; Globigerina bulloides; Globigerinita sp.; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; Maria S. Merian; MSM05/5; MSM05/5_712-1; Neogloboquadrina pachyderma dextral; Neogloboquadrina pachyderma sinistral; Sea surface temperature, summer; Turborotalita quinqueloba
    Materialart: Dataset
    Format: text/tab-separated-values, 1242 data points
    Standort Signatur Erwartet Verfügbarkeit
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    DATEN PANGAEA
  • 88
    facet.materialart.
    Unbekannt
    Basic and other measurements of radiation at station Tateno (2001-01) (2010)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, maximum; Diffuse radiation, minimum; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, maximum; Direct radiation, minimum; Direct radiation, standard deviation; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; Japan; Long-wave downward radiation; Long-wave downward radiation, maximum; Long-wave downward radiation, minimum; Long-wave downward radiation, standard deviation; Long-wave upward radiation; Long-wave upward radiation, maximum; Long-wave upward radiation, minimum; Long-wave upward radiation, standard deviation; Monitoring station; MONS; Net radiation; Net radiation, maximum; Net radiation, minimum; Net radiation, standard deviation; Pyranometer, Kipp & Zonen, CM21, SN 950236, WRMC No. 16017; Pyranometer, Kipp & Zonen, CM21, SN 960332, WRMC No. 16015; Pyranometer, Kipp & Zonen, CM21, SN 970423, WRMC No. 16019; Pyrgeometer, Eppley, PIR, SN 29460F3, WRMC No. 16009; Pyrgeometer, Eppley, PIR, SN 32205F3, WRMC No. 16022; Pyrheliometer, Kipp & Zonen, CH1, SN 950093, WRMC No. 16011; Radiometer, EKO, CN-11, SN 87057, WRMC No. 16020; Short-wave downward (GLOBAL) radiation; Short-wave downward (GLOBAL) radiation, maximum; Short-wave downward (GLOBAL) radiation, minimum; Short-wave downward (GLOBAL) radiation, standard deviation; Short-wave upward (REFLEX) radiation; Short-wave upward (REFLEX) radiation, maximum; Short-wave upward (REFLEX) radiation, minimum; Short-wave upward (REFLEX) radiation, standard deviation; Station pressure; TAT; Tateno; Thermometer
    Materialart: Dataset
    Format: text/tab-separated-values, 1246717 data points
    Standort Signatur Erwartet Verfügbarkeit
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    DATEN PANGAEA
  • 89
    facet.materialart.
    Unbekannt
    Basic and other measurements of radiation at station Tateno (2001-03) (2010)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, maximum; Diffuse radiation, minimum; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, maximum; Direct radiation, minimum; Direct radiation, standard deviation; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; Japan; Long-wave downward radiation; Long-wave downward radiation, maximum; Long-wave downward radiation, minimum; Long-wave downward radiation, standard deviation; Long-wave upward radiation; Long-wave upward radiation, maximum; Long-wave upward radiation, minimum; Long-wave upward radiation, standard deviation; Monitoring station; MONS; Net radiation; Net radiation, maximum; Net radiation, minimum; Net radiation, standard deviation; Pyranometer, Kipp & Zonen, CM21, SN 950236, WRMC No. 16017; Pyranometer, Kipp & Zonen, CM21, SN 960332, WRMC No. 16015; Pyranometer, Kipp & Zonen, CM21, SN 970423, WRMC No. 16019; Pyrgeometer, Eppley, PIR, SN 29460F3, WRMC No. 16009; Pyrgeometer, Eppley, PIR, SN 31714F3, WRMC No. 16021; Pyrheliometer, Kipp & Zonen, CH1, SN 950093, WRMC No. 16011; Radiometer, EKO, CN-11, SN 87057, WRMC No. 16020; Short-wave downward (GLOBAL) radiation; Short-wave downward (GLOBAL) radiation, maximum; Short-wave downward (GLOBAL) radiation, minimum; Short-wave downward (GLOBAL) radiation, standard deviation; Short-wave upward (REFLEX) radiation; Short-wave upward (REFLEX) radiation, maximum; Short-wave upward (REFLEX) radiation, minimum; Short-wave upward (REFLEX) radiation, standard deviation; Station pressure; TAT; Tateno; Thermometer
    Materialart: Dataset
    Format: text/tab-separated-values, 1246990 data points
    Standort Signatur Erwartet Verfügbarkeit
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    DATEN PANGAEA
  • 90
    facet.materialart.
    Unbekannt
    Basic and other measurements of radiation at station Tateno (2001-05) (2010)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, maximum; Diffuse radiation, minimum; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, maximum; Direct radiation, minimum; Direct radiation, standard deviation; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; Japan; Long-wave downward radiation; Long-wave downward radiation, maximum; Long-wave downward radiation, minimum; Long-wave downward radiation, standard deviation; Long-wave upward radiation; Long-wave upward radiation, maximum; Long-wave upward radiation, minimum; Long-wave upward radiation, standard deviation; Monitoring station; MONS; Net radiation; Net radiation, maximum; Net radiation, minimum; Net radiation, standard deviation; Pyranometer, Kipp & Zonen, CM21, SN 950236, WRMC No. 16017; Pyranometer, Kipp & Zonen, CM21, SN 960332, WRMC No. 16015; Pyranometer, Kipp & Zonen, CM21, SN 970423, WRMC No. 16019; Pyrgeometer, Eppley, PIR, SN 29460F3, WRMC No. 16009; Pyrgeometer, Eppley, PIR, SN 31714F3, WRMC No. 16021; Pyrheliometer, Kipp & Zonen, CH1, SN 950093, WRMC No. 16011; Radiometer, EKO, CN-11, SN 87057, WRMC No. 16020; Short-wave downward (GLOBAL) radiation; Short-wave downward (GLOBAL) radiation, maximum; Short-wave downward (GLOBAL) radiation, minimum; Short-wave downward (GLOBAL) radiation, standard deviation; Short-wave upward (REFLEX) radiation; Short-wave upward (REFLEX) radiation, maximum; Short-wave upward (REFLEX) radiation, minimum; Short-wave upward (REFLEX) radiation, standard deviation; Station pressure; TAT; Tateno; Thermometer
    Materialart: Dataset
    Format: text/tab-separated-values, 1241096 data points
    Standort Signatur Erwartet Verfügbarkeit
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    DATEN PANGAEA
  • 91
    facet.materialart.
    Unbekannt
    Basic and other measurements of radiation at station Tateno (2004-06) (2011)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, maximum; Diffuse radiation, minimum; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, maximum; Direct radiation, minimum; Direct radiation, standard deviation; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; Japan; Long-wave downward radiation; Long-wave downward radiation, maximum; Long-wave downward radiation, minimum; Long-wave downward radiation, standard deviation; Long-wave upward radiation; Long-wave upward radiation, maximum; Long-wave upward radiation, minimum; Long-wave upward radiation, standard deviation; Monitoring station; MONS; Net radiation; Net radiation, maximum; Net radiation, minimum; Net radiation, standard deviation; Pyranometer, Kipp & Zonen, CM21, SN 960330, WRMC No. 16013; Pyranometer, Kipp & Zonen, CM21, SN 960331, WRMC No. 16014; Pyranometer, Kipp & Zonen, CM22, SN 010048, WRMC No. 16023; Pyrgeometer, Eppley, PIR, SN 30700F3, WRMC No. 16010; Pyrgeometer, Eppley, PIR, SN 32205F3, WRMC No. 16022; Pyrheliometer, Kipp & Zonen, CH1, SN 950093, WRMC No. 16011; Radiometer, EKO, CN-11, SN 87057, WRMC No. 16020; Short-wave downward (GLOBAL) radiation; Short-wave downward (GLOBAL) radiation, maximum; Short-wave downward (GLOBAL) radiation, minimum; Short-wave downward (GLOBAL) radiation, standard deviation; Short-wave upward (REFLEX) radiation; Short-wave upward (REFLEX) radiation, maximum; Short-wave upward (REFLEX) radiation, minimum; Short-wave upward (REFLEX) radiation, standard deviation; Station pressure; TAT; Tateno; Thermometer
    Materialart: Dataset
    Format: text/tab-separated-values, 1192212 data points
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
    DATEN PANGAEA
  • 92
    facet.materialart.
    Unbekannt
    Basic and other measurements of radiation at station Tateno (2004-09) (2011)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, maximum; Diffuse radiation, minimum; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, maximum; Direct radiation, minimum; Direct radiation, standard deviation; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; Japan; Long-wave downward radiation; Long-wave downward radiation, maximum; Long-wave downward radiation, minimum; Long-wave downward radiation, standard deviation; Long-wave upward radiation; Long-wave upward radiation, maximum; Long-wave upward radiation, minimum; Long-wave upward radiation, standard deviation; Monitoring station; MONS; Net radiation; Net radiation, maximum; Net radiation, minimum; Net radiation, standard deviation; Pyranometer, Kipp & Zonen, CM21, SN 960330, WRMC No. 16013; Pyranometer, Kipp & Zonen, CM21, SN 960331, WRMC No. 16014; Pyranometer, Kipp & Zonen, CM22, SN 010048, WRMC No. 16023; Pyrgeometer, Eppley, PIR, SN 30700F3, WRMC No. 16010; Pyrgeometer, Eppley, PIR, SN 31714F3, WRMC No. 16021; Pyrheliometer, Kipp & Zonen, CH1, SN 950093, WRMC No. 16011; Radiometer, EKO, CN-11, SN 87057, WRMC No. 16020; Short-wave downward (GLOBAL) radiation; Short-wave downward (GLOBAL) radiation, maximum; Short-wave downward (GLOBAL) radiation, minimum; Short-wave downward (GLOBAL) radiation, standard deviation; Short-wave upward (REFLEX) radiation; Short-wave upward (REFLEX) radiation, maximum; Short-wave upward (REFLEX) radiation, minimum; Short-wave upward (REFLEX) radiation, standard deviation; Station pressure; TAT; Tateno; Thermometer
    Materialart: Dataset
    Format: text/tab-separated-values, 1210684 data points
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
    DATEN PANGAEA
  • 93
    facet.materialart.
    Unbekannt
    Basic and other measurements of radiation at station Tateno (2005-01) (2011)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, maximum; Diffuse radiation, minimum; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, maximum; Direct radiation, minimum; Direct radiation, standard deviation; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; Japan; Long-wave downward radiation; Long-wave downward radiation, maximum; Long-wave downward radiation, minimum; Long-wave downward radiation, standard deviation; Long-wave upward radiation; Long-wave upward radiation, maximum; Long-wave upward radiation, minimum; Long-wave upward radiation, standard deviation; Monitoring station; MONS; Net radiation; Net radiation, maximum; Net radiation, minimum; Net radiation, standard deviation; Pyranometer, Kipp & Zonen, CM21, SN 960330, WRMC No. 16013; Pyranometer, Kipp & Zonen, CM21, SN 960331, WRMC No. 16014; Pyranometer, Kipp & Zonen, CM22, SN 010048, WRMC No. 16023; Pyrgeometer, Eppley, PIR, SN 30700F3, WRMC No. 16010; Pyrgeometer, Eppley, PIR, SN 31714F3, WRMC No. 16021; Pyrheliometer, Kipp & Zonen, CH1, SN 950093, WRMC No. 16011; Radiometer, EKO, CN-11, SN 87057, WRMC No. 16020; Short-wave downward (GLOBAL) radiation; Short-wave downward (GLOBAL) radiation, maximum; Short-wave downward (GLOBAL) radiation, minimum; Short-wave downward (GLOBAL) radiation, standard deviation; Short-wave upward (REFLEX) radiation; Short-wave upward (REFLEX) radiation, maximum; Short-wave upward (REFLEX) radiation, minimum; Short-wave upward (REFLEX) radiation, standard deviation; Station pressure; TAT; Tateno; Thermometer
    Materialart: Dataset
    Format: text/tab-separated-values, 1252124 data points
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
    DATEN PANGAEA
  • 94
    facet.materialart.
    Unbekannt
    Basic and other measurements of radiation at station Tateno (2005-04) (2011)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, maximum; Diffuse radiation, minimum; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, maximum; Direct radiation, minimum; Direct radiation, standard deviation; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; Japan; Long-wave downward radiation; Long-wave downward radiation, maximum; Long-wave downward radiation, minimum; Long-wave downward radiation, standard deviation; Long-wave upward radiation; Long-wave upward radiation, maximum; Long-wave upward radiation, minimum; Long-wave upward radiation, standard deviation; Monitoring station; MONS; Net radiation; Net radiation, maximum; Net radiation, minimum; Net radiation, standard deviation; Pyranometer, Kipp & Zonen, CM21, SN 960330, WRMC No. 16013; Pyranometer, Kipp & Zonen, CM21, SN 960331, WRMC No. 16014; Pyranometer, Kipp & Zonen, CM22, SN 010048, WRMC No. 16023; Pyrgeometer, Eppley, PIR, SN 30700F3, WRMC No. 16010; Pyrgeometer, Eppley, PIR, SN 31714F3, WRMC No. 16021; Pyrheliometer, Kipp & Zonen, CH1, SN 950093, WRMC No. 16011; Radiometer, EKO, CN-11, SN 87057, WRMC No. 16020; Short-wave downward (GLOBAL) radiation; Short-wave downward (GLOBAL) radiation, maximum; Short-wave downward (GLOBAL) radiation, minimum; Short-wave downward (GLOBAL) radiation, standard deviation; Short-wave upward (REFLEX) radiation; Short-wave upward (REFLEX) radiation, maximum; Short-wave upward (REFLEX) radiation, minimum; Short-wave upward (REFLEX) radiation, standard deviation; Station pressure; TAT; Tateno; Thermometer
    Materialart: Dataset
    Format: text/tab-separated-values, 1175968 data points
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
    DATEN PANGAEA
  • 95
    facet.materialart.
    Unbekannt
    Basic and other measurements of radiation at station Tateno (2005-06) (2011)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, maximum; Diffuse radiation, minimum; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, maximum; Direct radiation, minimum; Direct radiation, standard deviation; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; Japan; Long-wave downward radiation; Long-wave downward radiation, maximum; Long-wave downward radiation, minimum; Long-wave downward radiation, standard deviation; Long-wave upward radiation; Long-wave upward radiation, maximum; Long-wave upward radiation, minimum; Long-wave upward radiation, standard deviation; Monitoring station; MONS; Net radiation; Net radiation, maximum; Net radiation, minimum; Net radiation, standard deviation; Pyranometer, Kipp & Zonen, CM21, SN 960330, WRMC No. 16013; Pyranometer, Kipp & Zonen, CM21, SN 960331, WRMC No. 16014; Pyranometer, Kipp & Zonen, CM22, SN 010048, WRMC No. 16023; Pyrgeometer, Eppley, PIR, SN 30700F3, WRMC No. 16010; Pyrgeometer, Eppley, PIR, SN 31714F3, WRMC No. 16021; Pyrheliometer, Kipp & Zonen, CH1, SN 950093, WRMC No. 16011; Radiometer, EKO, CN-11, SN 87057, WRMC No. 16020; Short-wave downward (GLOBAL) radiation; Short-wave downward (GLOBAL) radiation, maximum; Short-wave downward (GLOBAL) radiation, minimum; Short-wave downward (GLOBAL) radiation, standard deviation; Short-wave upward (REFLEX) radiation; Short-wave upward (REFLEX) radiation, maximum; Short-wave upward (REFLEX) radiation, minimum; Short-wave upward (REFLEX) radiation, standard deviation; Station pressure; TAT; Tateno; Thermometer
    Materialart: Dataset
    Format: text/tab-separated-values, 1202928 data points
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
    DATEN PANGAEA
  • 96
    facet.materialart.
    Unbekannt
    Basic and other measurements of radiation at station Tateno (2005-11) (2011)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, maximum; Diffuse radiation, minimum; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, maximum; Direct radiation, minimum; Direct radiation, standard deviation; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; Japan; Long-wave downward radiation; Long-wave downward radiation, maximum; Long-wave downward radiation, minimum; Long-wave downward radiation, standard deviation; Long-wave upward radiation; Long-wave upward radiation, maximum; Long-wave upward radiation, minimum; Long-wave upward radiation, standard deviation; Monitoring station; MONS; Net radiation; Net radiation, maximum; Net radiation, minimum; Net radiation, standard deviation; Pyranometer, Kipp & Zonen, CM21, SN 960331, WRMC No. 16014; Pyranometer, Kipp & Zonen, CM21, SN 960332, WRMC No. 16015; Pyranometer, Kipp & Zonen, CM22, SN 010048, WRMC No. 16023; Pyrgeometer, Eppley, PIR, SN 29460F3, WRMC No. 16009; Pyrgeometer, Eppley, PIR, SN 31714F3, WRMC No. 16021; Pyrheliometer, Kipp & Zonen, CH1, SN 950093, WRMC No. 16011; Radiometer, EKO, CN-11, SN 87057, WRMC No. 16020; Short-wave downward (GLOBAL) radiation; Short-wave downward (GLOBAL) radiation, maximum; Short-wave downward (GLOBAL) radiation, minimum; Short-wave downward (GLOBAL) radiation, standard deviation; Short-wave upward (REFLEX) radiation; Short-wave upward (REFLEX) radiation, maximum; Short-wave upward (REFLEX) radiation, minimum; Short-wave upward (REFLEX) radiation, standard deviation; Station pressure; TAT; Tateno; Thermometer
    Materialart: Dataset
    Format: text/tab-separated-values, 1211652 data points
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
    DATEN PANGAEA
  • 97
    facet.materialart.
    Unbekannt
    Basic and other measurements of radiation at station Tateno (2006-06) (2011)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, maximum; Diffuse radiation, minimum; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, maximum; Direct radiation, minimum; Direct radiation, standard deviation; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; Japan; Long-wave downward radiation; Long-wave downward radiation, maximum; Long-wave downward radiation, minimum; Long-wave downward radiation, standard deviation; Long-wave upward radiation; Long-wave upward radiation, maximum; Long-wave upward radiation, minimum; Long-wave upward radiation, standard deviation; Monitoring station; MONS; Pyranometer, Kipp & Zonen, CM21, SN 960331, WRMC No. 16014; Pyranometer, Kipp & Zonen, CM21, SN 960332, WRMC No. 16015; Pyranometer, Kipp & Zonen, CM22, SN 010048, WRMC No. 16023; Pyrgeometer, Eppley, PIR, SN 29460F3, WRMC No. 16009; Pyrgeometer, Eppley, PIR, SN 31714F3, WRMC No. 16021; Pyrheliometer, Kipp & Zonen, CH1, SN 950093, WRMC No. 16011; Short-wave downward (GLOBAL) radiation; Short-wave downward (GLOBAL) radiation, maximum; Short-wave downward (GLOBAL) radiation, minimum; Short-wave downward (GLOBAL) radiation, standard deviation; Short-wave upward (REFLEX) radiation; Short-wave upward (REFLEX) radiation, maximum; Short-wave upward (REFLEX) radiation, minimum; Short-wave upward (REFLEX) radiation, standard deviation; Station pressure; TAT; Tateno; Thermometer
    Materialart: Dataset
    Format: text/tab-separated-values, 1036848 data points
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
    DATEN PANGAEA
  • 98
    facet.materialart.
    Unbekannt
    Basic and other measurements of radiation at station Tateno (2007-06) (2011)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, maximum; Diffuse radiation, minimum; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, maximum; Direct radiation, minimum; Direct radiation, standard deviation; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; Japan; Long-wave downward radiation; Long-wave downward radiation, maximum; Long-wave downward radiation, minimum; Long-wave downward radiation, standard deviation; Long-wave upward radiation; Long-wave upward radiation, maximum; Long-wave upward radiation, minimum; Long-wave upward radiation, standard deviation; Monitoring station; MONS; Pyranometer, Kipp & Zonen, CM21, SN 960332, WRMC No. 16015; Pyranometer, Kipp & Zonen, CM21, SN 970366, WRMC No. 16024; Pyranometer, Kipp & Zonen, CM22, SN 010048, WRMC No. 16023; Pyrgeometer, Eppley, PIR, SN 29460F3, WRMC No. 16009; Pyrgeometer, Eppley, PIR, SN 31714F3, WRMC No. 16021; Pyrheliometer, Kipp & Zonen, CH1, SN 950093, WRMC No. 16011; Short-wave downward (GLOBAL) radiation; Short-wave downward (GLOBAL) radiation, maximum; Short-wave downward (GLOBAL) radiation, minimum; Short-wave downward (GLOBAL) radiation, standard deviation; Short-wave upward (REFLEX) radiation; Short-wave upward (REFLEX) radiation, maximum; Short-wave upward (REFLEX) radiation, minimum; Short-wave upward (REFLEX) radiation, standard deviation; Station pressure; TAT; Tateno; Thermometer
    Materialart: Dataset
    Format: text/tab-separated-values, 1038940 data points
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
    DATEN PANGAEA
  • 99
    facet.materialart.
    Unbekannt
    Basic and other measurements of radiation at station Tateno (2008-01) (2011)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, maximum; Diffuse radiation, minimum; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, maximum; Direct radiation, minimum; Direct radiation, standard deviation; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; Japan; Long-wave downward radiation; Long-wave downward radiation, maximum; Long-wave downward radiation, minimum; Long-wave downward radiation, standard deviation; Long-wave upward radiation; Long-wave upward radiation, maximum; Long-wave upward radiation, minimum; Long-wave upward radiation, standard deviation; Monitoring station; MONS; Pyranometer, Kipp & Zonen, CM21, SN 960331, WRMC No. 16014; Pyranometer, Kipp & Zonen, CM21, SN 960332, WRMC No. 16015; Pyranometer, Kipp & Zonen, CM21, SN 970423, WRMC No. 16019; Pyrgeometer, Kipp & Zonen, CG4, SN 010582, WRMC No. 16026; Pyrgeometer, Kipp & Zonen, CG4, SN 030641, WRMC No. 16032; Pyrheliometer, Kipp & Zonen, CH1, SN 950093, WRMC No. 16011; Short-wave downward (GLOBAL) radiation; Short-wave downward (GLOBAL) radiation, maximum; Short-wave downward (GLOBAL) radiation, minimum; Short-wave downward (GLOBAL) radiation, standard deviation; Short-wave upward (REFLEX) radiation; Short-wave upward (REFLEX) radiation, maximum; Short-wave upward (REFLEX) radiation, minimum; Short-wave upward (REFLEX) radiation, standard deviation; Station pressure; TAT; Tateno; Thermometer
    Materialart: Dataset
    Format: text/tab-separated-values, 1073592 data points
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
    DATEN PANGAEA
  • 100
    facet.materialart.
    Unbekannt
    Basic and other measurements of radiation at station Tateno (2008-05) (2011)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publikationsdatum: 2024-05-31
    Schlagwort(e): Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, maximum; Diffuse radiation, minimum; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, maximum; Direct radiation, minimum; Direct radiation, standard deviation; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; Japan; Long-wave downward radiation; Long-wave downward radiation, maximum; Long-wave downward radiation, minimum; Long-wave downward radiation, standard deviation; Long-wave upward radiation; Long-wave upward radiation, maximum; Long-wave upward radiation, minimum; Long-wave upward radiation, standard deviation; Monitoring station; MONS; Pyranometer, Kipp & Zonen, CM21, SN 960331, WRMC No. 16014; Pyranometer, Kipp & Zonen, CM21, SN 960332, WRMC No. 16015; Pyranometer, Kipp & Zonen, CM21, SN 970423, WRMC No. 16019; Pyrgeometer, Kipp & Zonen, CG4, SN 010582, WRMC No. 16026; Pyrgeometer, Kipp & Zonen, CG4, SN 030641, WRMC No. 16032; Pyrheliometer, Kipp & Zonen, CH1, SN 950093, WRMC No. 16011; Short-wave downward (GLOBAL) radiation; Short-wave downward (GLOBAL) radiation, maximum; Short-wave downward (GLOBAL) radiation, minimum; Short-wave downward (GLOBAL) radiation, standard deviation; Short-wave upward (REFLEX) radiation; Short-wave upward (REFLEX) radiation, maximum; Short-wave upward (REFLEX) radiation, minimum; Short-wave upward (REFLEX) radiation, standard deviation; Station pressure; TAT; Tateno; Thermometer
    Materialart: Dataset
    Format: text/tab-separated-values, 1073592 data points
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
    DATEN PANGAEA
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