A 275 year ice core record from Akademii Nauk ice cap, Severnaya Zemlya, Russian Arctic.

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dc.contributor.author Fritzsche, Diedrich
dc.contributor.author Schütt, Rainer
dc.contributor.author Meyer, Hanno
dc.contributor.author Miller, Heinz
dc.contributor.author Wilhelms, Frank
dc.contributor.author Opel, Thomas
dc.contributor.author Savatyugin, Lev M
dc.coverage.spatial LATITUDE: 80.516660 * LONGITUDE: 94.816660 * DATE/TIME START: 1999-05-01T00:00:00 * DATE/TIME END: 1999-05-01T00:00:00 * MINIMUM DEPTH, ice/snow: 0.7 m * MAXIMUM DEPTH, ice/snow: 136.5 m
dc.date.accessioned 2019-11-24T03:17:34Z
dc.date.available 2019-11-24T03:17:34Z
dc.date.issued 2006-09-15
dc.identifier https://doi.pangaea.de/10.1594/PANGAEA.511330
dc.identifier https://doi.org/10.1594/PANGAEA.511330
dc.identifier.citation Fritzsche, Diedrich; Schütt, Rainer; Meyer, Hanno; Miller, Heinz; Wilhelms, Frank; Opel, Thomas; Savatyugin, Lev M (2005): A 275 year ice core record from Akademii Nauk ice cap, Severnaya Zemlya, Russian Arctic. Annals of Glaciology, 42, 361-366, https://doi.org/10.3189/172756405781812862
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/7485
dc.description.abstract Between 1999 and 2001, a 724 m long ice core was drilled on Akademii Nauk, the largest glacier on Severnaya Zemlya, Russian Arctic. The drilling site is located near the summit. The core is characterized by high melt-layer content. The melt layers are caused by melting and even by rain during the summer. We present high-resolution data of density, electrical conductivity (dielectrical profiling), stable water isotopes and melt-layer content for the upper 136 m (120 m w.e.) of the ice core. The dating by isotopic cycles and electrical conductivity peak identification suggests that this core section covers approximately the past 275 years. Singularities of volcanogenic and anthropogenic origin provide well-defined additional time markers. Long-term temperatures inferred from 12 year running mean averages of d18O reach their lowest level in the entire record around 1790. Thereafter the d18O values indicate a continuously increasing mean temperature on the Akademii Nauk ice cap until 1935, interrupted only by minor cooling episodes. The 20th century is found to be the warmest period in this record.
dc.format text/tab-separated-values, 676 data points
dc.language.iso en
dc.publisher PANGAEA
dc.rights CC-BY-3.0: Creative Commons Attribution 3.0 Unported
dc.rights Access constraints: unrestricted
dc.source Supplement to: Fritzsche, Diedrich; Schütt, Rainer; Meyer, Hanno; Miller, Heinz; Wilhelms, Frank; Opel, Thomas; Savatyugin, Lev M (2005): A 275 year ice core record from Akademii Nauk ice cap, Severnaya Zemlya, Russian Arctic. Annals of Glaciology, 42, 361-366, https://doi.org/10.3189/172756405781812862
dc.subject Age
dc.subject AGE
dc.subject Age model, layer counting
dc.subject Akademii Nauk, Severnaya Zemlya, Russian Arctic
dc.subject AWI_PerDyn
dc.subject calculated average/mean values
dc.subject DEPTH, ice/snow
dc.subject Depth water equivalent
dc.subject ICEDRILL
dc.subject Ice drill
dc.subject Permafrost Research (Periglacial Dynamics) @ AWI
dc.subject SZ_1999/2001
dc.subject SZ99
dc.subject δ18O
dc.subject δ18O, water
dc.title A 275 year ice core record from Akademii Nauk ice cap, Severnaya Zemlya, Russian Arctic.
dc.title.alternative Age model and stable oxygen isotope mean values of ice core SZ99 from Akademii Nauk ice cap on Severnaya Zemlya
dc.type Dataset


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