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  • 1
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    Unbekannt
    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
    Publikationsdatum: 2024-05-31
    Beschreibung: Central waters of the North Atlantic are fundamental for ventilation of the upper ocean and are also linked to the strength of the Atlantic Meridional Overturning Circulation (AMOC). Here, we show based on benthic foraminiferal Mg/Ca ratios, that during times of enhanced melting from the Laurentide Ice Sheet (LIS) between 9.0-8.5 thousand years before present (ka) the production of central waters weakened the upper AMOC resulting in a cooling over the Northern Hemisphere. Centered at 8.54 ± 0.2 ka and 8.24 ± 0.1 ka our dataset records two ~150-year cooling events in response to the drainage of Lake Agassiz/Ojibway, indicating early slow-down of the upper AMOC in response to the initial freshwater flux into the subpolar gyre (SPG) followed by a more severe weakening of both the upper and lower branches of the AMOC at 8.2 ka. These results highlight the sensitivity of regional North Atlantic climate change to the strength of central-water overturning and exemplify the impact of both gradual and abrupt freshwater fluxes on eastern SPG surface water convection. In light of the possible future increase in Greenland Ice Sheet melting due to global warming these findings may help us to better constrain and possibly predict future North Atlantic climate change.
    Schlagwort(e): BGR; Bundesanstalt für Geowissenschaften und Rohstoffe, Hannover; Center for Marine Environmental Sciences; GeoB6007-2; Gravity corer (Kiel type); Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; M45/5a; MARUM; Meteor (1986); SL
    Materialart: Dataset
    Format: application/zip, 2 datasets
    Standort Signatur Erwartet Verfügbarkeit
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  • 2
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    Unbekannt
    PANGAEA
    In:  Supplement to: Müller, Stefanie; Tarasov, Pavel E; Andreev, Andrei A; Diekmann, Bernhard (2009): Late Glacial to Holocene environments in the present-day coldest region of the Northern Hemisphere inferred from a pollen record of Lake Billyakh, Verkhoyansk Mts, NE Siberia. Climate of the Past, 5, 73-84, https://doi.org/10.5194/cp-5-73-2009
    Publikationsdatum: 2024-05-31
    Beschreibung: In this study a radiocarbon-dated pollen record from Lake Billyakh (65°17'N, 126°47'E; 340 m a.s.l.) in the Verkhoyansk Mountains was used to reconstruct vegetation and climate change since about 15 kyr BP (1 kyr=1000 cal. yr). The pollen record and pollen-based biome reconstruction suggest that open cool steppe and grass and sedge tundra communities with Poaceae, Cyperaceae, Artemisia, Chenopodiaceae, Caryophyllaceae and Selaginella rupestris dominated the area from 15 to 13.5 kyr BP. On the other hand, the constant presence of Larix pollen in quantities comparable to today's values points to the constant presence of boreal deciduous conifer trees in the regional vegetation during the last glaciation. A major spread of shrub tundra communities, including birch (Betula sect. Nanae), alder (Duschekia fruticosa) and willow (Salix) species, is dated to 13.5-12.7 kyr BP, indicating a noticeable increase in precipitation toward the end of the last glaciation, particularly during the Allerød Interstadial. Between 12.7 and 11.4 kyr BP pollen percentages of herbaceous taxa rapidly increased, whereas shrub taxa percentages decreased, suggesting strengthening of the steppe communities associated with the relatively cold and dry Younger Dryas Stadial. However, the pollen data in hand indicate that Younger Dryas climate was less severe than the climate during the earlier interval from 15 to 13.5 kyr BP. The onset of the Holocene is marked in the pollen record by the highest values of shrub and lowest values of herbaceous taxa, suggesting a return of warmer and wetter conditions after 11.4 kyr BP. Percentages of tree taxa increase gradually and reach maximum values after 7 kyr BP, reflecting the spread of boreal cold deciduous and taiga forests in the region. An interval between 7 and 2 kyr BP is noticeable for the highest percentages of Scots spine (Pinus subgen. Diploxylon), spruce (Picea) and fir (Abies) pollen, indicating mid-Holocene spread of boreal forest communities in response to climate amelioration and degradation of the permafrost layer.
    Schlagwort(e): AWI_PerDyn; AWI Arctic Land Expedition; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; Lake Billyakh, Verkhoyansk Mountains, Yakuti, Russia; PCUWI; Permafrost Research (Periglacial Dynamics) @ AWI; PG1756; Piston corer, UWITEC; RU-Land_2005_Verkhoyansk; Yakutia2005
    Materialart: Dataset
    Format: application/zip, 2 datasets
    Standort Signatur Erwartet Verfügbarkeit
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  • 3
    facet.materialart.
    Unbekannt
    PANGAEA
    In:  Supplement to: Demske, Dieter; Tarasov, Pavel E; Wünnemann, Bernd; Riedel, Frank (2009): Late glacial and Holocene vegetation, Indian monsoon and westerly circulation in the Trans-Himalaya recorded in the lacustrine pollen sequence from Tso Kar, Ladakh, NW India. Palaeogeography, Palaeoclimatology, Palaeoecology, 279(3-4), 172-185, https://doi.org/10.1016/j.palaeo.2009.05.008
    Publikationsdatum: 2024-05-31
    Beschreibung: Palynological investigation of a 410 cm long core section from Tso Kar (33°10'N, 78°E, 4527 m a.s.l.), an alpine lake situated in the arid Ladakh area of NW India at the limit of the present-day Indian summer monsoon, was performed in order to reconstruct post-glacial regional vegetation and climate dynamics. The area was covered with alpine desert vegetation from ca. 15.2 to 14 kyr BP (1 kyr=1000 cal. years), reflecting dry and cold conditions. High influx values of long-distance transported Pinus sylvestris type pollen suggest prevailing air flow from the west and northwest. The spread of alpine meadow communities and local aquatic vegetation is a weak sign of climate amelioration after ca. 14 kyr BP. Pollen data (e.g. influx values of Pinus roxburghii type and Quercus) suggest that this was due to a strengthening of the summer monsoon and the reduced activity of westerly winds. The further spread of Artemisia and species-rich meadows occurred in response to improved moisture conditions between ca. 12.9 and 12.5 kyr BP. The subsequent change towards drier desert-steppe vegetation likely indicates more frequent westerly disturbances and associated snowfalls, which favoured the persistence of alpine meadows on edaphically moist sites. The spread of Chenopodiaceae-dominated vegetation associated with an extremely weak monsoon occurred at ca. 12.2-11.8 kyr BP during the Younger Dryas interstadial. A major increase in humidity is inferred from the development of Artemisia-dominated steppe and wet alpine meadows with Gentianaceae after the late glacial/early Holocene transition in response to the strengthening of the summer monsoon. Monsoonal influence reached maximum activity in the Tso Kar region between ca. 10.9 and 9.2 kyr BP. The subsequent development of the alpine meadow, steppe and desert-steppe vegetation points to a moderate reduction in the moisture supply, which can be linked to the weaker summer monsoon and the accompanying enhancement of the winter westerly flow from ca. 9.2 to 4.8 kyr BP. The highest water levels of Tso Kar around 8 kyr BP probably reflect combined effect of both monsoonal and westerly influence in the region. An abrupt shift towards aridity in the Tso Kar region occurred after ca. 4.8 kyr BP, as evidenced by an expansion of Chenopodiaceae-dominated desert-steppe. Low pollen influx values registered ca. 2.8-1.3 kyr BP suggest scarce vegetation cover and unfavourable growing conditions likely associated with a further weakening of the Indian Monsoon.
    Schlagwort(e): Geological profile sampling; GEOPRO; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; Ladakh, NW India, Himalaya; Tso_Kar
    Materialart: Dataset
    Format: application/zip, 2 datasets
    Standort Signatur Erwartet Verfügbarkeit
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  • 4
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    Unbekannt
    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
    Publikationsdatum: 2024-05-31
    Beschreibung: In this study we review a global set of alkenone- and foraminiferal Mg/Ca-derived sea surface temperatures (SST) records from the Holocene and compare them with a suite of published Eemian SST records based on the same approach. For the Holocene, the alkenone SST records belong to the actualized GHOST database (Kim, J.-H., Schneider R.R., 2004). The actualized GHOST database not only confirms the SST changes previously described but also documents the Holocene temperature evolution in new oceanic regions such as the Northwestern Atlantic, the eastern equatorial Pacific, and the Southern Ocean. A comparison of Holocene SST records stemming from the two commonly applied paleothermometry methods reveals contrasting - sometimes divergent - SST evolution, particularly at low latitudes where SST records are abundant enough to infer systematic discrepancies at a regional scale. Opposite SST trends at particular locations could be explained by out-of-phase trends in seasonal insolation during the Holocene. This hypothesis assumes that a strong contrast in the ecological responses of coccolithophores and planktonic foraminifera to winter and summer oceanographic conditions is the ultimate reason for seasonal differences in the origin of the temperature signal provided by these organisms. As a simple test for this hypothesis, Eemian SST records are considered because the Holocene and Eemian time periods experienced comparable changes in orbital configurations, but had a higher magnitude in insolation variance during the Eemian. For several regions, SST changes during both interglacials were of a similar sign, but with higher magnitudes during the Eemian as compared to the Holocene. This observation suggests that the ecological mechanism shaping SST trends during the Holocene was comparable during the penultimate interglacial period. Although this "ecology hypothesis" fails to explain all of the available results, we argue that any other mechanism would fail to satisfactorily explain the observed SST discrepancies among proxies.
    Schlagwort(e): 108-658C; 138-846; 160-967D; 160-969E; 161-977; 162-984; 165-1002C; 165-999A; 167-1012B; 167-1017E; 167-1019C; 175-1078C; 175-1084B; 184-1145C; 2; 202-1233; 202-1240; 202-1242; 225514; 225517; 71; 90b; 96; 96-619; A-7; AD91-17; Alboran Sea; also published as VM28-122; Angola Basin; Arabian Sea; Arctic Ocean; Atlantic Ocean; AUSCAN; Bay of Bengal; BCR; BENEFIT/4; BENGAL FAN; Benguela Current, South Atlantic Ocean; BOFS31/1K; BOFS31#1; Box corer (Reineck); BS79-33; BS79-38; CALYPSO; Calypso Corer; Canarias Sea; Caribbean Sea; Cayman Rise, Caribbean Sea; CD159-12; CD53; CEPAG; CH07-98-GGC19; Charles Darwin; Chatham Rise; CHIPAL; Cocos Ridge; COMPCORE; Composite Core; Congo Fan; D13882; D249; De Soto Canyon; Discovery (1962); DRILL; Drilling/drill rig; Eastern Basin; East Pacific; Emperor Seamounts; Equatorial East Pacific; GC; GeoB1023-5; GeoB3129-1; GeoB3313-1; GeoB3910-2; GeoB4509-2; GeoB4905-4; GeoB5546-2; GeoB5844-2; GeoB5901-2; GeoB6007-2; GeoB6518-1; GeoB7139-2; GeoB7926-2; GEOSCIENCES, MARMARCORE; GeoTü SL71; GGC; GGC-15-1; Giant box corer; Giant gravity corer; Giant piston corer; GIK17748-2; GIK17940-2; GIK17964-1; GIK18252-3; GIK18287-3; GIK23258-2; GINCO 3; GKG; Glomar Challenger; GPC; Gravity corer; Gravity corer (Kiel type); Gulf of Mexico; Hakuho-Maru; HOTLINE, HYGAPE; IMAGES I; IMAGES III - IPHIS; IMAGES IV-IPHIS III; IMAGES IX - PAGE; IMAGES V; IMAGES VIII - MONA; IMAGES VII - WEPAMA; Indian Ocean; Indonesia; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; IOW225514; IOW225517; IOW4509B; James Clark Ross; Joides Resolution; JOPSII-6; JR20000727; JR51; JR51GC-35; JT96-0909PC; KAL; Kasten corer; KH-01-3; KH-01-3-19; KL; KL_Mg; Knorr; KNR176-2; KNR176-JPC32; Kurilen Trench; LAPAZ21P; Leg108; Leg138; Leg160; Leg161; Leg162; Leg165; Leg167; Leg175; Leg184; Leg202; Leg96; Le Suroît; M34/4; M35/1; M35003-4; M39/1; M39/1_08-3; M39008-3; M40/4; M40/4_87-6SL; M40/4_SL67; M40/4_SL71; M40/4_SL78; M40/4_SL78-3; M40/4_SL87; M41/1; M42/4b; M44/1; M44/1_74KL; M44/1_KL71; M44/3; M45/1; M45/5a; M47/3; M53/1; M6/6; M7/2; Marge Ibérique; Marion Dufresne (1972); Marion Dufresne (1995); Marmara Sea; MD01-2334; MD012378; MD01-2378; MD012390; MD01-2390; MD012412; MD01-2412; MD012416; MD01-2416; MD01-2443; MD022529; MD02-2529; MD022575; MD02-2575; MD032611G; MD03-2611G; MD03-2707; MD101; MD106; MD111; MD114; MD122; MD123; MD126; MD127; MD13; MD131; MD77-194; MD79-257; MD85674; MD94-103; MD952011; MD95-2011; MD952015; MD95-2015; MD952042; MD95-2042; MD952043; MD95-2043; MD972120; MD97-2120; MD972121; MD97-2121; MD972125; MD97-2125; MD972141; MD97-2141; MD972151; MD97-2151; MD982162; MD98-2162; MD982165; MD98-2165; MD982170; MD98-2170; MD982176; MD98-2176; MD982181; MD98-2181; MD99-2155; MD99-2251; MD99-2334; ME0005A; ME0005A-24JC; Melville; Meteor (1986); MONITOR MONSUN; NE-Brazilian continental margin; NEMO; Northeast Atlantic; Northeast Brasilian Margin; Northern Red Sea; North Pacific Ocean; North-West African margin; OCE326-GGC26; OCE326-GGC30; off Cameroon; OSIRIS4; OSIRIS III; Pacific Ocean; PAKOMIN; PC; PC-17; PC-2; PC-4; Petr Kottsov; Piston corer; Piston corer (BGR type); Piston corer Meischner large; PL07-39PC; Portuguese Margin; PUCK; RAPID-12-1K; RC11; RC1112; RC11-238; Reykjanes Ridge; RL11; Robert Conrad; Rockall; SCS90-36; SL; SO102/1; SO115; SO115_05; SO115_40; SO136; SO136_011GC; SO139; SO139-74KL; SO156/2; SO80_4; SO80a; SO90; SO90_136KL; SO90_39KG; SO90_93KL; SO93/3; SO93/3_126KL; SO95; Sonne; South Atlantic Ocean; South China Sea; South-East Pacific; Southern Ocean; Southern Okhotsk Sea; South Pacific Ocean; SSDP102; St.14; St.20; SU81-18; SUNDAFLUT; Sunda Shelf; TASQWA; Timor Sea; TN057-21; TR163-19; TR163-22; TY93-905; TY93929/P; U938; V19; V19-27; V19-28; V19-30; V21; V21-30; V28; V28-122; Vema; Victor Hensen; Vietnam shelf; Voring Plateau
    Materialart: Dataset
    Format: application/zip, 133 datasets
    Standort Signatur Erwartet Verfügbarkeit
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  • 5
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    Unbekannt
    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
    Publikationsdatum: 2024-05-31
    Beschreibung: Geochemical tracers incorporated into the skeleton of reef-building corals are ideal proxies for reconstructing environmental parameters of ambient seawater such as temperature and salinity at subseasonal resolution. However, validation concerns of these environmental proxies due to the complex skeleton of some tropical Atlantic corals have hindered such coral-based environmental reconstructions in this region compared to the tropical Pacific. In order to identify complications associated with the complex skeletal architecture of the massive brain coral Diploria strigosa, we performed microsampling experiments along and across individual skeletal elements. We demonstrate that the mesoscale heterogeneity of Sr/Ca, d18O and d13C is a systematic feature of D. strigosa and is linked to different vital effects between skeletal elements. The thecal wall is significantly depleted in Sr, 18O and 13C compared to the adjacent septa and columella and differences between apparent temperature signatures of several degrees are greater for Sr/Ca suggesting that this temperature proxy is more sensitive to skeletal mixing than d18O. Parallel subseasonal microsampling experiments performed along individual skeletal elements of a single corallite of a D. strigosa coral which grew at a rate of 0.65 cm/year allow for investigating potential biases associated with its complex skeletal mesoarchitecture. Highest correlation between Sr/Ca and d18O from skeletal material retrieved from the centre of the thecal wall suggests that microdrilling the theca provides the best environmental signal compared to adjacent microsampling profiles. Moreover, based on monthly-mean climatology, the temperature dependence of Sr/Ca for this profile is comparable to previous calibrations published from faster growing D. strigosa. Based on these results, we conclude that accurate microsampling along the centre of the thecal wall of D. strigosa is a prerequisite for generating robust climate reconstructions from its skeleton.
    Schlagwort(e): BON-9-A; CaribClim_Coral_2006; Center for Marine Environmental Sciences; DRILL; Drilling/drill rig; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; MARUM; Southern Caribbean Sea, Bonaire
    Materialart: Dataset
    Format: application/zip, 3 datasets
    Standort Signatur Erwartet Verfügbarkeit
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  • 6
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    Unbekannt
    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
    Publikationsdatum: 2024-05-31
    Beschreibung: The Arctic is responding more rapidly to global warming than most other areas on our planet. Northward flowing Atlantic Water is the major means of heat advection towards the Arctic and strongly affects the sea ice distribution. Records of its natural variability are critical for the understanding of feedback mechanisms and the future of the Arctic climate system, but continuous historical records reach back only ~150 years. Here, we present a multidecadal scale record of ocean temperature variations during the last 2000 years, derived from marine sediments off Western Svalbard (79°N). We find that early-21st-century temperatures of Atlantic Water entering the Arctic Ocean are unprecedented over the past 2000 years and are presumably linked to the Arctic Amplification of global warming.
    Schlagwort(e): CTD/Rosette; CTD-RO; Fram Strait; Giant box corer; GKG; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; International Polar Year (2007-2008); IPY; Jan Mayen; JM06-WP; JM06-WP-02; Maria S. Merian; MSM05/5; MSM05/5_712-1; MSM05/5_713-1; North Greenland Sea; WarmPast 2006
    Materialart: Dataset
    Format: application/zip, 4 datasets
    Standort Signatur Erwartet Verfügbarkeit
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  • 7
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    Unbekannt
    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
    Publikationsdatum: 2024-05-31
    Beschreibung: The enhanced accumulation of organic matter in Eastern Mediterranean sapropels and their unusually low d15N values have been attributed to either enhanced nutrient availability which led to elevated primary production and carbon sequestration or to enhanced organic matter preservation under anoxic conditions. In order to evaluate these two hypothesis we have determined Ba/Al ratios, amino acid composition, N and organic C concentrations and d15N in sinking particles, surface sediments, eight spatially distributed core records of the youngest sapropel S1 (10-6 ka) and older sapropels (S5, S6) from two locations. These data suggest that (i) temporal and spatial variations in d15N of sedimentary N are driven by different degrees of diagenesis at different sites rather than by changes in N-sources or primary productivity and (ii) present day TOC export production would suffice to create a sapropel like S1 under conditions of deep-water anoxia. This implies that both enhanced TOC accumulation and d15N depletion in sapropels were due to the absence of oxygen in deep waters. Thus preservation plays a major role for the accumulation of organic-rich sediments casting doubt on the need of enhanced primary production for sapropel formation.
    Schlagwort(e): 101; 101-105; 106-111; 107; 111; 112-116; 116; 117-122; 118; 123-126; 137-139; 140-142; 143-148; 149-154; 155-162; 163-170; 171-179; 180-187; 188-194; 560; 561; 562; 563; 564; 565; 566; 569; 570; 571; 572; 573; 574; 575; 576; 577; 578; 579; 580; 581; 582; 584; 585; 586; 589; 590; 592; 594; 596; 599; 601; 602; 604; 666; 667; 668; 670; 671; 672; 673; 674; 676; 677; 678; 680; 681; 682; 683; 684; 685; 686; 687; 689; 690; 691; 692; 693; 694; 695; 696; 697; 699; 700; 701; 702; 703; 704; 705; 706; 707; 708; 709; 710; 712; 713; 714; 716; 717; 718; 719; 80; 82; 85; Cyprus; Eastern Mediterranean, Continental slope off Israel; Eratosthenes Seamount; Gargano Promontory; GeoB10701-4; GeoB10702-3; GeoB10703-3; GeoB10704-3; GeoB10705-3; GeoB10706-3; GeoB10707-4; GeoB10708-3; GeoB10710-4; GeoB10711-3; GeoB10712-3; GeoB10713-3; GeoB10714-3; GeoB10715-3; GeoB10716-3; GeoB10717-3; GeoB10718-3; GeoB10719-3; GeoB10720-5; GeoB10721-3; GeoB10722-3; GeoB10723-3; GeoB10724-3; GeoB10725-3; GeoB10726-3; GeoB10727-3; GeoB10728-3; GeoB10729-4; GeoB10730-3; GeoB10731-3; GeoB10732-3; GeoB10733-3; GeoB10734-3; GeoB10735-3; GeoB10736-3; GeoB10737-3; GeoB10738-3; GeoB10739-3; GeoB10740-3; GeoB10741-3; GeoB10742-3; GeoB10743-3; GeoB10744-3; GeoB10746-3; GeoB10747-3; GeoB10748-3; GeoB10749-3; GeoB7704-1; GeoB7705-1; GeoB7706-2; GeoB7714-1; GeoB7718-1; GeoB7720-1; GeoB7723-2; GeoB7725-2; Gravity corer (Kiel type); Greece; Gulf of Manfredonia; Gulf of Taranto; Haifa; Integrierte Analyse zwischeneiszeitlicher Klimadynamik; INTERDYNAMIK; Lybia; M40/4; M40/4_MUC65; M40/4_MUC66; M40/4_MUC67; M40/4_MUC68; M40/4_MUC69; M40/4_MUC70; M40/4_MUC71; M40/4_MUC72; M40/4_MUC73; M40/4_MUC74; M40/4_MUC75; M40/4_MUC76-2; M40/4_MUC76-3; M40/4_MUC77A; M40/4_MUC77B; M40/4_MUC78-2; M40/4_MUC79; M40/4_MUC81; M40/4_MUC82; M40/4_MUC84; M40/4_MUC85; M40/4_MUC86; M40/4_MUC87; M40/4_MUC88; M40/4_MUC89; M40/4_MUC90; M40/4_MUC91; M40/4_SL80; M51/3; M51/3_560-1; M51/3_561-4; M51/3_562-5; M51/3_563-5; M51/3_564-2; M51/3_565-1; M51/3_566-3; M51/3_569-3; M51/3_570-2; M51/3_571; M51/3_572-2; M51/3_573; M51/3_574-2; M51/3_575-6; M51/3_576-3; M51/3_577-1; M51/3_578; M51/3_579; M51/3_580; M51/3_581; M51/3_582; M51/3_584; M51/3_585; M51/3_586; M51/3_589; M51/3_590; M51/3_592; M51/3_594; M51/3_596; M51/3_599; M51/3_601-3; M51/3_602; M51/3_604; M52/2; M71/3; M71/3_H01; M71/3_H02; M71/3_H03; M71/3_H04; M71/3_H05; M71/3_H06; M71/3_H07; M71/3_H11; M71/3_H12; M71/3_Her01; M71/3_Her03; M71/3_ler01; M71/3_Rho02; M71/3_Sk01; Malta; Meteor (1986); MUC; MultiCorer; Nile Fan; POS339; Poseidon; SL; Strait of Otranto; Turkey; Zyprus
    Materialart: Dataset
    Format: application/zip, 6 datasets
    Standort Signatur Erwartet Verfügbarkeit
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  • 8
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    Unbekannt
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Publikationsdatum: 2024-05-31
    Schlagwort(e): ALTITUDE; Baseline Surface Radiation Network; BSRN; DATE/TIME; Dew/frost point; Japan; Monitoring station; MONS; Pressure, at given altitude; Radiosonde, Meisei, RS291; TAT; Tateno; Temperature, air
    Materialart: Dataset
    Format: text/tab-separated-values, 13187 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 9
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    Unbekannt
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Publikationsdatum: 2024-05-31
    Schlagwort(e): ALTITUDE; Baseline Surface Radiation Network; BSRN; DATE/TIME; Dew/frost point; Japan; Monitoring station; MONS; Pressure, at given altitude; Radiosonde, Meisei, RS291; TAT; Tateno; Temperature, air
    Materialart: Dataset
    Format: text/tab-separated-values, 14023 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 10
    facet.materialart.
    Unbekannt
    PANGAEA
    In:  Aerological Observatory, Japan Meteorological Agency
    Publikationsdatum: 2024-05-31
    Schlagwort(e): ALTITUDE; Baseline Surface Radiation Network; BSRN; DATE/TIME; Dew/frost point; Japan; Monitoring station; MONS; Pressure, at given altitude; Radiosonde, Meisei, RS291; TAT; Tateno; Temperature, air
    Materialart: Dataset
    Format: text/tab-separated-values, 11801 data points
    Standort Signatur Erwartet Verfügbarkeit
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