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  • PANGAEA  (51,121)
  • 2010-2014  (50,456)
  • 1980-1984  (665)
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  • 1
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    (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
    Publication Date: 2024-05-31
    Description: 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.
    Keywords: 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
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 2
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    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
    Publication Date: 2024-05-31
    Description: 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.
    Keywords: 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
    Type: Dataset
    Format: application/zip, 133 datasets
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  • 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
    Publication Date: 2024-05-31
    Description: 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.
    Keywords: 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
    Type: Dataset
    Format: application/zip, 3 datasets
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    DATA 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
    Publication Date: 2024-05-31
    Description: 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.
    Keywords: 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
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 5
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    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
    Publication Date: 2024-05-31
    Description: 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.
    Keywords: 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
    Type: Dataset
    Format: application/zip, 6 datasets
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  • 6
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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
    Publication Date: 2024-05-31
    Description: 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.
    Keywords: Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK
    Type: Dataset
    Format: application/zip, 7 datasets
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  • 7
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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
    Publication Date: 2024-05-31
    Description: 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.
    Keywords: Center for Marine Environmental Sciences; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; MARUM
    Type: Dataset
    Format: application/zip, 9 datasets
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  • 8
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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
    Publication Date: 2024-05-31
    Description: 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.
    Keywords: 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
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 9
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    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
    Publication Date: 2024-05-31
    Description: 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.
    Keywords: Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 10
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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
    Publication Date: 2024-05-31
    Description: 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.
    Keywords: EPICA; European Project for Ice Coring in Antarctica; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 11
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    Reference list of sources used for two experimental data files dataBSRN and dataMixed (2011)
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    Details
    Publication Date: 2024-05-31
    Description: 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.
    Type: Dataset
    Format: 7498 datasets
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  • 12
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    Raw data from 2.35 ka Bonaire coral, sample BON-6-A (2011)
    PANGAEA
    Details
    Publication Date: 2024-05-31
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 3189 data points
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  • 13
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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
    Publication Date: 2024-05-31
    Description: 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.
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 971 data points
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  • 14
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    Raw data from 3.79 ka Bonaire coral, sample BON-7-A (2011)
    PANGAEA
    Details
    Publication Date: 2024-05-31
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 1936 data points
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  • 15
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    Reference list of 269 sources used for exploratory search (2012)
    PANGAEA
    Details
    Publication Date: 2024-05-31
    Description: 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.
    Keywords: 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
    Type: Dataset
    Format: 269 datasets
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  • 16
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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
    Publication Date: 2024-05-31
    Description: 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.
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 5307 data points
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  • 17
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    Mineral dust deposition in interglacial and glacial climate conditions: model results (2012)
    PANGAEA
    Details
    Publication Date: 2024-05-31
    Description: 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.
    Keywords: Abbreviation; Experiment; File format; File name; File size; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; Parameter; Uniform resource locator/link to model result file; Unit
    Type: Dataset
    Format: text/tab-separated-values, 80 data points
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  • 18
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    Basic and other measurements of radiation at station Tateno (2010-09) (2010)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publication Date: 2024-05-31
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 1038760 data points
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  • 19
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    Physical oceanography at CTD station JM06-WP-02 (2011)
    PANGAEA
    Details
    Publication Date: 2024-05-31
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 1198 data points
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  • 20
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    Chemical composition of surface sediment samples from the Eastern Mediterranean Sea (2010)
    PANGAEA
    Details
    Publication Date: 2024-05-31
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 3130 data points
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  • 21
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    Raw data from 1.84 ka Bonaire coral, sample BON-20-A (2011)
    PANGAEA
    Details
    Publication Date: 2024-05-31
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 482 data points
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  • 22
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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
    Publication Date: 2024-05-31
    Description: 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.
    Keywords: Archaeosociomodeling; Baluchistan; GLUES; GLUES_IVC; Harappa; Indus Valley; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; Mehrgarh; Model; Neolithic; Version 1.1.19; western Eurasia
    Type: Dataset
    Format: application/x-gzip, 92.4 kBytes
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  • 23
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    Unknown
    Basic and other measurements of radiation at station Tateno (2009-12) (2010)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publication Date: 2024-05-31
    Keywords: 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 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
    Type: Dataset
    Format: text/tab-separated-values, 1073592 data points
    Location Call Number Expected Availability
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  • 24
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    Unknown
    Basic and other measurements of radiation at station Tateno (2010-01) (2010)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publication Date: 2024-05-31
    Keywords: 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 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
    Type: Dataset
    Format: text/tab-separated-values, 1073592 data points
    Location Call Number Expected Availability
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  • 25
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    Unknown
    Basic and other measurements of radiation at station Tateno (2010-04) (2010)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publication Date: 2024-05-31
    Keywords: 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 970423, WRMC No. 16019; 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
    Type: Dataset
    Format: text/tab-separated-values, 1038960 data points
    Location Call Number Expected Availability
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  • 26
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    Unknown
    Basic and other measurements of radiation at station Tateno (2010-03) (2010)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publication Date: 2024-05-31
    Keywords: 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 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
    Type: Dataset
    Format: text/tab-separated-values, 1073428 data points
    Location Call Number Expected Availability
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  • 27
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    Unknown
    Basic and other measurements of radiation at station Tateno (2010-07) (2010)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publication Date: 2024-05-31
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 1073592 data points
    Location Call Number Expected Availability
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  • 28
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    Basic and other measurements of radiation at station Tateno (2002-02) (2010)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publication Date: 2024-05-31
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 1130771 data points
    Location Call Number Expected Availability
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  • 29
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    Basic and other measurements of radiation at station Tateno (2002-06) (2010)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publication Date: 2024-05-31
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 1157041 data points
    Location Call Number Expected Availability
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  • 30
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    Unknown
    Basic and other measurements of radiation at station Tateno (2002-09) (2010)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publication Date: 2024-05-31
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 1206373 data points
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  • 31
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    Basic and other measurements of radiation at station Tateno (2003-07) (2010)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publication Date: 2024-05-31
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 1208088 data points
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  • 32
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    Basic and other measurements of radiation at station Tateno (2003-11) (2010)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publication Date: 2024-05-31
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 1171634 data points
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  • 33
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    Basic and other measurements of radiation at station Tateno (2003-09) (2010)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publication Date: 2024-05-31
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 1211708 data points
    Location Call Number Expected Availability
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  • 34
    facet.materialart.
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    Basic and other measurements of radiation at station Tateno (2004-01) (2011)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publication Date: 2024-05-31
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 1251827 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 35
    facet.materialart.
    Unknown
    Basic and other measurements of radiation at station Tateno (2004-04) (2011)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publication Date: 2024-05-31
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 1205712 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 36
    facet.materialart.
    Unknown
    Basic and other measurements of radiation at station Tateno (2004-08) (2011)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publication Date: 2024-05-31
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 1252048 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 37
    facet.materialart.
    Unknown
    Basic and other measurements of radiation at station Tateno (2004-12) (2011)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publication Date: 2024-05-31
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 1246552 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 38
    facet.materialart.
    Unknown
    Basic and other measurements of radiation at station Tateno (2005-05) (2011)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publication Date: 2024-05-31
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 1217732 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 39
    facet.materialart.
    Unknown
    Basic and other measurements of radiation at station Tateno (2005-08) (2011)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publication Date: 2024-05-31
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 1125564 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 40
    facet.materialart.
    Unknown
    Basic and other measurements of radiation at station Tateno (2005-12) (2011)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publication Date: 2024-05-31
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 1252064 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 41
    facet.materialart.
    Unknown
    Basic and other measurements of radiation at station Tateno (2006-05) (2011)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publication Date: 2024-05-31
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 1073588 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 42
    facet.materialart.
    Unknown
    Basic and other measurements of radiation at station Tateno (2006-08) (2011)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publication Date: 2024-05-31
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 1073572 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 43
    facet.materialart.
    Unknown
    Basic and other measurements of radiation at station Tateno (2006-11) (2011)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publication Date: 2024-05-31
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 1038960 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 44
    facet.materialart.
    Unknown
    Basic and other measurements of radiation at station Tateno (2007-01) (2011)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publication Date: 2024-05-31
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 1073565 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 45
    facet.materialart.
    Unknown
    Basic and other measurements of radiation at station Tateno (2008-05) (2011)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publication Date: 2024-05-31
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 1073592 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 46
    facet.materialart.
    Unknown
    Basic and other measurements of radiation at station Tateno (2007-05) (2011)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publication Date: 2024-05-31
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 1073592 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 47
    facet.materialart.
    Unknown
    Basic and other measurements of radiation at station Tateno (2007-07) (2011)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publication Date: 2024-05-31
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 1073592 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 48
    facet.materialart.
    Unknown
    Basic and other measurements of radiation at station Tateno (2007-09) (2011)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publication Date: 2024-05-31
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 1038960 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 49
    facet.materialart.
    Unknown
    Basic and other measurements of radiation at station Tateno (2007-11) (2011)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publication Date: 2024-05-31
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 1038923 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 50
    facet.materialart.
    Unknown
    Basic and other measurements of radiation at station Tateno (2007-12) (2011)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publication Date: 2024-05-31
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 1073592 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 51
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    Basic and other measurements of radiation at station Tateno (2008-02) (2011)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publication Date: 2024-05-31
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 1004328 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 52
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    Unknown
    Basic and other measurements of radiation at station Tateno (2008-04) (2011)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publication Date: 2024-05-31
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 1038960 data points
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    DATA PANGAEA
  • 53
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    Distribution of planktic foraminifera and stable istopes of sediment core MSM05/5_712-2 (2013)
    PANGAEA
    Details
    Publication Date: 2024-05-31
    Keywords: Accumulation rate, ice rafted debris by number; Accumulation rate, planktic foraminifera by number; AGE; Calculated; Calculated from mass/volume; Cibicidoides wuellerstorfi, δ13C; Cibicidoides wuellerstorfi, δ18O; Counting 100-250 µm fraction; Density, dry bulk; DEPTH, sediment/rock; Foraminifera, planktic; Fram Strait; Grain size, sieving/settling tube; Ice rafted debris; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; IRD-Counting (Grobe, 1987); KAL; Kasten corer; Maria S. Merian; Mass spectrometry; MSM05/5; MSM05/5_712-2; Neogloboquadrina pachyderma sinistral; Neogloboquadrina pachyderma sinistral, δ13C; Neogloboquadrina pachyderma sinistral, δ18O; Size fraction 1.000-0.063 mm; Turborotalita quinqueloba; Turborotalita quinqueloba, δ13C; Turborotalita quinqueloba, δ18O
    Type: Dataset
    Format: text/tab-separated-values, 1967 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 54
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    Unknown
    (Figure 5) Monthly interpolated coral Sr/Ca record from Bonaire coral BON-7-A, 3.79 ka (2012)
    PANGAEA
    Details
    Publication Date: 2024-05-31
    Keywords: BON-7-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
    Type: Dataset
    Format: text/tab-separated-values, 936 data points
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    DATA PANGAEA
  • 55
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    Unknown
    (Figure 5) Monthly interpolated coral Sr/Ca record from Bonaire coral BON-9-A, 1912 AD (2012)
    PANGAEA
    Details
    Publication Date: 2024-05-31
    Keywords: BON-9-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
    Type: Dataset
    Format: text/tab-separated-values, 746 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 56
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    (Figure 7) Mean coral Sr/Ca seasonality for individual Bonaire corals (2012)
    PANGAEA
    Details
    Publication Date: 2024-05-31
    Keywords: 1-sigma error based on U-series datings; AGE; Age, error; 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; Diploria strigosa, Strontium/Calcium ratio; DRILL; Drilling/drill rig; Error; Event label; ICP-OES, Perkin-Elmer, Optima 3300R; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; MARUM; see reference(s); Southern Caribbean Sea, Bonaire
    Type: Dataset
    Format: text/tab-separated-values, 23 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 57
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    (Figure 8) Seasonal coral Sr/Ca records from 2.35 ka coral sample (2012)
    PANGAEA
    Details
    Publication Date: 2024-05-31
    Keywords: BON-6-A; Calculated, monthly interpolated; 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
    Type: Dataset
    Format: text/tab-separated-values, 1892 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 58
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    Unknown
    Basic and other measurements of radiation at station Tateno (2011-06) (2012)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publication Date: 2024-05-31
    Keywords: 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 970365, WRMC No. 16028; Pyranometer, Kipp & Zonen, CM22, SN 010048, WRMC No. 16023; Pyranometer, Kipp & Zonen, CMP21, SN 100363, WRMC No. 16036; Pyrgeometer, Kipp & Zonen, CG4, SN 010582, WRMC No. 16026; Pyrgeometer, Kipp & Zonen, CGR4, SN 090166, WRMC No. 16039; 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
    Type: Dataset
    Format: text/tab-separated-values, 1038924 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 59
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    Unknown
    Basic and other measurements of radiation at station Tateno (2012-05) (2012)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publication Date: 2024-05-31
    Keywords: 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, CMP21, SN 090229, WRMC No. 16035; Pyranometer, Kipp & Zonen, CMP21, SN 100363, WRMC No. 16036; Pyranometer, Kipp & Zonen, CMP22, SN 090099, WRMC No. 16037; Pyrgeometer, Kipp & Zonen, CGR4, SN 090133, WRMC No. 16038; Pyrgeometer, Kipp & Zonen, CGR4, SN 090166, WRMC No. 16039; Pyrheliometer, Kipp & Zonen, CHP 1, SN 090140, WRMC No. 16034; 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
    Type: Dataset
    Format: text/tab-separated-values, 1073572 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 60
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    Basic and other measurements of radiation at station Tateno (2012-10) (2012)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publication Date: 2024-05-31
    Keywords: 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, CMP21, SN 090229, WRMC No. 16035; Pyranometer, Kipp & Zonen, CMP21, SN 100363, WRMC No. 16036; Pyranometer, Kipp & Zonen, CMP22, SN 090099, WRMC No. 16037; Pyrgeometer, Kipp & Zonen, CGR4, SN 090133, WRMC No. 16038; Pyrgeometer, Kipp & Zonen, CGR4, SN 090166, WRMC No. 16039; Pyrheliometer, Kipp & Zonen, CHP 1, SN 090140, WRMC No. 16034; 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
    Type: Dataset
    Format: text/tab-separated-values, 1073592 data points
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  • 61
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    Age, depth, Uk'37 and estimated sea surface temperature of sediment core GeoB8332-3 (2010)
    PANGAEA
    Details
    Publication Date: 2024-05-31
    Keywords: Age; Alkenone, unsaturation index UK'37; Calculated; Calculated from UK'37 (Müller et al, 1998); Center for Marine Environmental Sciences; DEPTH, sediment/rock; GeoB; GeoB8332-3; Geosciences, University of Bremen; GIK/IfG; Institute for Geosciences, Christian Albrechts University, Kiel; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; M57/1; MARUM; Meteor (1986); MUC; MultiCorer; Sea surface temperature
    Type: Dataset
    Format: text/tab-separated-values, 90 data points
    Location Call Number Expected Availability
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  • 62
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    Basic and other measurements of radiation at station Tateno (2013-01) (2013)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publication Date: 2024-05-31
    Keywords: 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, CMP21, SN 090229, WRMC No. 16035; Pyranometer, Kipp & Zonen, CMP21, SN 100363, WRMC No. 16036; Pyranometer, Kipp & Zonen, CMP22, SN 090099, WRMC No. 16037; Pyrgeometer, Kipp & Zonen, CGR4, SN 090133, WRMC No. 16038; Pyrgeometer, Kipp & Zonen, CGR4, SN 090166, WRMC No. 16039; Pyrheliometer, Kipp & Zonen, CHP 1, SN 100227, WRMC No. 16041; 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
    Type: Dataset
    Format: text/tab-separated-values, 1073588 data points
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  • 63
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    Sortable silt mean of sediment core MSM05/5_712-2 (2013)
    PANGAEA
    Details
    Publication Date: 2024-05-31
    Keywords: AGE; Calculated; Fram Strait; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; KAL; Kasten corer; Maria S. Merian; MSM05/5; MSM05/5_712-2; Sortable-silt mean
    Type: Dataset
    Format: text/tab-separated-values, 201 data points
    Location Call Number Expected Availability
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  • 64
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    Unknown
    Basic and other measurements of radiation at station Tateno (2013-02) (2013)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publication Date: 2024-05-31
    Keywords: 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, CMP21, SN 090229, WRMC No. 16035; Pyranometer, Kipp & Zonen, CMP21, SN 100363, WRMC No. 16036; Pyranometer, Kipp & Zonen, CMP22, SN 090099, WRMC No. 16037; Pyrgeometer, Kipp & Zonen, CGR4, SN 090133, WRMC No. 16038; Pyrgeometer, Kipp & Zonen, CGR4, SN 090166, WRMC No. 16039; Pyrheliometer, Kipp & Zonen, CHP 1, SN 100227, WRMC No. 16041; 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
    Type: Dataset
    Format: text/tab-separated-values, 969696 data points
    Location Call Number Expected Availability
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  • 65
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    Monthly interpolated coral δ¹⁸O record from Bonaire coral BON-6-A, 2.35 ka (2013)
    PANGAEA
    Details
    Publication Date: 2024-05-31
    Keywords: BON-6-A; Calculated, monthly interpolated; CaribClim_Coral_2006; Center for Marine Environmental Sciences; Diploria strigosa, δ18O; DRILL; Drilling/drill rig; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; Internal coral chronology; MARUM; Mass spectrometer Finnigan MAT 251; Southern Caribbean Sea, Bonaire
    Type: Dataset
    Format: text/tab-separated-values, 1622 data points
    Location Call Number Expected Availability
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  • 66
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    Basic and other measurements of radiation at station Tateno (2013-03) (2013)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publication Date: 2024-05-31
    Keywords: 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, CMP21, SN 090231, WRMC No. 4006/86006; Pyranometer, Kipp & Zonen, CMP21, SN 100363, WRMC No. 16036; Pyranometer, Kipp & Zonen, CMP22, SN 090101, WRMC No. 4007; Pyrgeometer, Kipp & Zonen, CGR4, SN 090133, WRMC No. 16038; Pyrgeometer, Kipp & Zonen, CGR4, SN 090166, WRMC No. 16039; Pyrheliometer, Kipp & Zonen, CHP 1, SN 090140, WRMC No. 16034; 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
    Type: Dataset
    Format: text/tab-separated-values, 1073592 data points
    Location Call Number Expected Availability
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  • 67
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    Basic and other measurements of radiation at station Tateno (2013-04) (2013)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publication Date: 2024-05-31
    Keywords: 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, CMP21, SN 090229, WRMC No. 16035; Pyranometer, Kipp & Zonen, CMP21, SN 100363, WRMC No. 16036; Pyranometer, Kipp & Zonen, CMP22, SN 090099, WRMC No. 16037; Pyrgeometer, Kipp & Zonen, CGR4, SN 090133, WRMC No. 16038; Pyrgeometer, Kipp & Zonen, CGR4, SN 090166, WRMC No. 16039; Pyrheliometer, Kipp & Zonen, CHP 1, SN 090140, WRMC No. 16034; 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
    Type: Dataset
    Format: text/tab-separated-values, 1038960 data points
    Location Call Number Expected Availability
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  • 68
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    Diatom abundances in sediment core NBP99-03-MTC18A (2013)
    PANGAEA
    Details
    Publication Date: 2024-05-31
    Keywords: Age; AGE; Antarctic Peninsula; Climate Change: Learning from the past climate; DEPTH, sediment/rock; Diatoms, sea ice; Diatoms, total, per unit sediment mass; MTC18A; MUC; MultiCorer; Nathaniel B. Palmer; NBP9903; NBP9903_MTC18A; Past4Future; Thalassiosira antarctica; Thalassiosira gracilis
    Type: Dataset
    Format: text/tab-separated-values, 276 data points
    Location Call Number Expected Availability
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  • 69
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    Community Climate System Model, version 3 (CCSM3) model data (2013)
    PANGAEA
    Details
    Publication Date: 2024-05-31
    Keywords: Center for Marine Environmental Sciences; Description; File name; File size; File type; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; MARUM; Uniform resource locator/link to model result file
    Type: Dataset
    Format: text/tab-separated-values, 30 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 70
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    Age model and sea surface temperature data used for Empirical Orthogonal Function (EOF) analysis and for proxy-data model comparisons during MIS11 (2013)
    PANGAEA
    Details
    Publication Date: 2024-05-31
    Keywords: Center for Marine Environmental Sciences; Deep Sea Drilling Project; DSDP; GeoB; Geosciences, University of Bremen; GIK/IfG; Institute for Geosciences, Christian Albrechts University, Kiel; Integrated Ocean Drilling Program / International Ocean Discovery Program; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; IODP; MARUM; Ocean Drilling Program; ODP
    Type: Dataset
    Format: 0 Bytes
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  • 71
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    13. 14C-AMS dates from sediment core GeoB3938-1 (2014)
    PANGAEA
    Details
    Publication Date: 2024-05-31
    Keywords: Age, 14C AMS; Age, 14C calibrated, CALIB 6.1.0 (Stuiver et al., 2014) and Marine09 calibration; Age, dated; Age, dated material; Age, dated standard deviation; Atlantic Caribbean Margin; Calendar age; Calendar age, standard error; Center for Marine Environmental Sciences; DEPTH, sediment/rock; GeoB3938-1; Gravity corer (Kiel type); Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; Laboratory code/label; M34/4; MARUM; Meteor (1986); SL
    Type: Dataset
    Format: text/tab-separated-values, 24 data points
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  • 72
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    09. Age model from sediment core GeoB7011-1 (2014)
    PANGAEA
    Details
    Publication Date: 2024-05-31
    Keywords: Age model; Center for Marine Environmental Sciences; DEPTH, sediment/rock; GC; GeoB7011-1; Gravity corer; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; M49/4; MARUM; Meteor (1986); Sedimentation rate
    Type: Dataset
    Format: text/tab-separated-values, 14 data points
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  • 73
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    Basic and other measurements of radiation at station Tateno (2014-04) (2014)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publication Date: 2024-05-31
    Keywords: 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, CMP21, SN 090229, WRMC No. 16035; Pyranometer, Kipp & Zonen, CMP21, SN 100363, WRMC No. 16036; Pyranometer, Kipp & Zonen, CMP22, SN 090099, WRMC No. 16037; Pyrgeometer, Kipp & Zonen, CGR4, SN 090133, WRMC No. 16038; Pyrgeometer, Kipp & Zonen, CGR4, SN 090166, WRMC No. 16039; Pyrheliometer, Kipp & Zonen, CHP 1, SN 090140, WRMC No. 16034; 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
    Type: Dataset
    Format: text/tab-separated-values, 1038952 data points
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  • 74
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    Basic and other measurements of radiation at station Tateno (2014-06) (2014)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publication Date: 2024-05-31
    Keywords: 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, CMP21, SN 090229, WRMC No. 16035; Pyranometer, Kipp & Zonen, CMP21, SN 100363, WRMC No. 16036; Pyranometer, Kipp & Zonen, CMP22, SN 090099, WRMC No. 16037; Pyrgeometer, Kipp & Zonen, CGR4, SN 090133, WRMC No. 16038; Pyrgeometer, Kipp & Zonen, CGR4, SN 090166, WRMC No. 16039; Pyrheliometer, Kipp & Zonen, CHP 1, SN 090140, WRMC No. 16034; 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
    Type: Dataset
    Format: text/tab-separated-values, 1038952 data points
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  • 75
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    14. Age model from sediment core GeoB3938-1 (2014)
    PANGAEA
    Details
    Publication Date: 2024-05-31
    Keywords: Age model; Atlantic Caribbean Margin; Center for Marine Environmental Sciences; DEPTH, sediment/rock; GeoB3938-1; Gravity corer (Kiel type); Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; M34/4; MARUM; Meteor (1986); Method comment; Sedimentation rate; SL
    Type: Dataset
    Format: text/tab-separated-values, 51 data points
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  • 76
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    Basic and other measurements of radiation at station Tateno (1999-12) (2014)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publication Date: 2024-05-31
    Keywords: 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 28849F3, WRMC No. 16008; Pyrgeometer, Eppley, PIR, SN 29460F3, WRMC No. 16009; Pyrheliometer, Kipp & Zonen, CH1, SN 950093, WRMC No. 16011; Radiometer, EKO, CN-11, SN 87058, WRMC No. 16018; 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
    Type: Dataset
    Format: text/tab-separated-values, 1239862 data points
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  • 77
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    Basic and other measurements of radiation at station Tateno (2014-07) (2014)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publication Date: 2024-05-31
    Keywords: 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, CMP21, SN 090229, WRMC No. 16035; Pyranometer, Kipp & Zonen, CMP21, SN 100363, WRMC No. 16036; Pyranometer, Kipp & Zonen, CMP22, SN 090099, WRMC No. 16037; Pyrgeometer, Kipp & Zonen, CGR4, SN 090133, WRMC No. 16038; Pyrgeometer, Kipp & Zonen, CGR4, SN 090166, WRMC No. 16039; Pyrheliometer, Kipp & Zonen, CHP 1, SN 090140, WRMC No. 16034; 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
    Type: Dataset
    Format: text/tab-separated-values, 1073592 data points
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  • 78
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    Basic and other measurements of radiation at station Tateno (2014-09) (2014)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publication Date: 2024-05-31
    Keywords: 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, CMP21, SN 090229, WRMC No. 16035; Pyranometer, Kipp & Zonen, CMP21, SN 100363, WRMC No. 16036; Pyranometer, Kipp & Zonen, CMP22, SN 090099, WRMC No. 16037; Pyrgeometer, Kipp & Zonen, CGR4, SN 090133, WRMC No. 16038; Pyrgeometer, Kipp & Zonen, CGR4, SN 090166, WRMC No. 16039; Pyrheliometer, Kipp & Zonen, CHP 1, SN 090140, WRMC No. 16034; 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
    Type: Dataset
    Format: text/tab-separated-values, 1038960 data points
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  • 79
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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
    Publication Date: 2024-05-31
    Description: 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.
    Keywords: Florida Strait; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; PC; Piston corer; RASTA/GOLDFLOS; SO164; SO164-17-2; Sonne
    Type: Dataset
    Format: application/zip, 5 datasets
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  • 80
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    Planktonic foraminiferal (Globigerinoides ruber) Mg/Ca ratios and SSTs of sediment cores GeoB9501-4 and GeoB9501-5 (2011)
    PANGAEA
    Details
    Publication Date: 2024-05-31
    Description: 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.
    Keywords: 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
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 81
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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
    Publication Date: 2024-05-31
    Description: 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.
    Keywords: 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
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 82
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    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
    Publication Date: 2024-05-31
    Description: 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.
    Keywords: 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
    Type: Dataset
    Format: application/zip, 13 datasets
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  • 83
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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
    Publication Date: 2024-05-31
    Description: 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.
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 351 data points
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  • 84
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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
    Publication Date: 2024-05-31
    Description: 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.
    Keywords: Abbreviation; Experiment; File format; File name; File size; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; Parameter; Uniform resource locator/link to model result file; Unit
    Type: Dataset
    Format: text/tab-separated-values, 100 data points
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  • 85
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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
    Publication Date: 2024-05-31
    Description: 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.
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 960 data points
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  • 86
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    Raw data from 4.27 ka Bonaire coral, sample BON-4-G (2011)
    PANGAEA
    Details
    Publication Date: 2024-05-31
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 1069 data points
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  • 87
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    Unknown
    Raw data from 1957 AD Bonaire coral, sample BON-9-B (2011)
    PANGAEA
    Details
    Publication Date: 2024-05-31
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 804 data points
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  • 88
    facet.materialart.
    Unknown
    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
    Publication Date: 2024-05-31
    Description: 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.
    Keywords: Center for Marine Environmental Sciences; File format; File name; File size; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; MARUM; Uniform resource locator/link to file
    Type: Dataset
    Format: text/tab-separated-values, 36 data points
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  • 89
    facet.materialart.
    Unknown
    Raw data from 3.83 ka Bonaire coral, sample BON-7-B (2011)
    PANGAEA
    Details
    Publication Date: 2024-05-31
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 1772 data points
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  • 90
    facet.materialart.
    Unknown
    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
    Publication Date: 2024-05-31
    Keywords: 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
    Type: Dataset
    Format: 6787 datasets
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  • 91
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    Unknown
    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
    Publication Date: 2024-05-31
    Description: 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.
    Keywords: Comment; File content; File format; File name; File size; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; Reference of data; Uniform resource locator/link to file
    Type: Dataset
    Format: text/tab-separated-values, 76 data points
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  • 92
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    Unknown
    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
    Publication Date: 2024-05-31
    Description: 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.
    Keywords: -; 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
    Type: Dataset
    Format: text/tab-separated-values, 396 data points
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  • 93
    facet.materialart.
    Unknown
    Distribution of planktic foraminifera and stable istopes of sediment core MSM05/5_712-1 (2010)
    PANGAEA
    Details
    Publication Date: 2024-05-31
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 930 data points
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  • 94
    facet.materialart.
    Unknown
    Raw data from 1912 AD Bonaire coral, sample BON-9-A (2011)
    PANGAEA
    Details
    Publication Date: 2024-05-31
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 1548 data points
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  • 95
    facet.materialart.
    Unknown
    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
    Publication Date: 2024-05-31
    Description: 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.
    Keywords: Abbreviation; File format; File name; File size; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; Parameter; Uniform resource locator/link to model result file; Unit
    Type: Dataset
    Format: text/tab-separated-values, 77 data points
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  • 96
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    Unknown
    Basic and other measurements of radiation at station Tateno (2002-04) (2010)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publication Date: 2024-05-31
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 1199786 data points
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  • 97
    facet.materialart.
    Unknown
    Basic and other measurements of radiation at station Tateno (2002-03) (2010)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publication Date: 2024-05-31
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 1250648 data points
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  • 98
    facet.materialart.
    Unknown
    Basic and other measurements of radiation at station Tateno (2002-10) (2010)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publication Date: 2024-05-31
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 1252089 data points
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  • 99
    facet.materialart.
    Unknown
    Basic and other measurements of radiation at station Tateno (2003-04) (2010)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publication Date: 2024-05-31
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 1208164 data points
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  • 100
    facet.materialart.
    Unknown
    Basic and other measurements of radiation at station Tateno (2003-08) (2010)
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Details
    Publication Date: 2024-05-31
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 1249072 data points
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