Accumulation rate of the B26_2011 firn core

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Hauptverfasser: Vinther, Bo Møllesøe, Freitag, Johannes, Kipfstuhl, Sepp, Weißbach, Stefanie, Karlsson, Nanna Bjørnholt, Münch, Thomas, Hörhold, Maria
Format: Dataset Open Access
Sprache:en
Veröffentlicht: PANGAEA 2022
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author Vinther, Bo Møllesøe
Freitag, Johannes
Kipfstuhl, Sepp
Weißbach, Stefanie
Karlsson, Nanna Bjørnholt
Münch, Thomas
Hörhold, Maria
author_facet Vinther, Bo Møllesøe
Freitag, Johannes
Kipfstuhl, Sepp
Weißbach, Stefanie
Karlsson, Nanna Bjørnholt
Münch, Thomas
Hörhold, Maria
collection Datos científicos de ciencias marinas y ambientales
contents The firn core array of the North Greenland Traverse (NGT) provides unique climatic information for North Greenland until the mid 1990ies. In order to extend this climate record into more recent time, some of the drill sites were revisited and extension cores were drilled. The record is a composite of snow liners (from the surface to 1.29 m depth) and a consecutive firn core from 1.47 m depth to 30.00 m depth with a diameter of 75 cm. Density was measured by weighing the 55 cm long bags. Stable oxygen isotopes (δ18O) were measured at the Niels Bohr Institute, Copenhagen, Denmark. Using raw, un-calibrated dielectrical profiling (DEP) data from the field (NEEM Set-up), volcanic tie points were derived. Together with the smoothed density data and the isotopic composition the record was dated by layer counting. The annual mean values of δ18O were obtained based on this dating. Based on the density measurements and the dating, the annual accumulation rate in water equivalent depth was derived.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_945666
institution PANGAEA
language en
publishDate 2022
publisher PANGAEA
record_format pangaea
spellingShingle Accumulation rate of the B26_2011 firn core
Vinther, Bo Møllesøe
Freitag, Johannes
Kipfstuhl, Sepp
Weißbach, Stefanie
Karlsson, Nanna Bjørnholt
Münch, Thomas
Hörhold, Maria
Accumulation rate ice, in water equivalent; Age; AGE; AWI_Envi; AWI_Glac; B26_2011; Calculated, annual mean; density; FIRNC; firn core; Firn corer; Glaciology @ AWI; Greenland; NEEM; North Greenland Eemian Ice Drilling; North Greenland Traverse; Polar Terrestrial Environmental Systems @ AWI; stable water isotopes
The firn core array of the North Greenland Traverse (NGT) provides unique climatic information for North Greenland until the mid 1990ies. In order to extend this climate record into more recent time, some of the drill sites were revisited and extension cores were drilled. The record is a composite of snow liners (from the surface to 1.29 m depth) and a consecutive firn core from 1.47 m depth to 30.00 m depth with a diameter of 75 cm. Density was measured by weighing the 55 cm long bags. Stable oxygen isotopes (δ18O) were measured at the Niels Bohr Institute, Copenhagen, Denmark. Using raw, un-calibrated dielectrical profiling (DEP) data from the field (NEEM Set-up), volcanic tie points were derived. Together with the smoothed density data and the isotopic composition the record was dated by layer counting. The annual mean values of δ18O were obtained based on this dating. Based on the density measurements and the dating, the annual accumulation rate in water equivalent depth was derived.
title Accumulation rate of the B26_2011 firn core
topic Accumulation rate ice, in water equivalent; Age; AGE; AWI_Envi; AWI_Glac; B26_2011; Calculated, annual mean; density; FIRNC; firn core; Firn corer; Glaciology @ AWI; Greenland; NEEM; North Greenland Eemian Ice Drilling; North Greenland Traverse; Polar Terrestrial Environmental Systems @ AWI; stable water isotopes
url https://doi.org/10.1594/PANGAEA.945666