Comparison of accumulation rates and stable isotope ratios ...

Since 1979/80, glaciological studies have been carried out at Ekströmisen, Antarctica, including accumulation-stake measurements, snow-pit and shallow-firn-core studies. Snowstratigraphy, chemical properties and stable-isotope ratios (d18O) were investigated. This study focuses on three cores taken...

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Main Authors: Schlosser, Elisabeth, Oerter, Hans
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2002
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.690398
https://doi.pangaea.de/10.1594/PANGAEA.690398
id ftdatacite:10.1594/pangaea.690398
record_format openpolar
spelling ftdatacite:10.1594/pangaea.690398 2023-06-11T04:07:02+02:00 Comparison of accumulation rates and stable isotope ratios ... Schlosser, Elisabeth Oerter, Hans 2002 application/zip https://dx.doi.org/10.1594/pangaea.690398 https://doi.pangaea.de/10.1594/PANGAEA.690398 en eng PANGAEA https://dx.doi.org/10.3189/172756402781816915 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Ice drill Stake Firn auger Neumayer_based EPICA_DML3 NEUMAYER III Neumayer Station WMO89002 Glaciology @ AWI AWI_Glac Collection Supplementary Publication Series of Datasets article 2002 ftdatacite https://doi.org/10.1594/pangaea.69039810.3189/172756402781816915 2023-06-01T11:44:30Z Since 1979/80, glaciological studies have been carried out at Ekströmisen, Antarctica, including accumulation-stake measurements, snow-pit and shallow-firn-core studies. Snowstratigraphy, chemical properties and stable-isotope ratios (d18O) were investigated. This study focuses on three cores taken between 1982 and 1998. The 1998 core was dated using dielectric profiling, d18O profiles and stake measurements. Accumulation rates showhigh interannual and spatial variability due to the extreme wind influence. No significant trend was found for the last 50 years; during the first half of the 20th century, accumulation decreased. The high spatial and interannual variability, however, means that trends must be interpreted with care. In spite of the highly irregular accumulation distribution, stable-isotope ratios show little spatial variability. The mean annual d18O values of cores B04 and FB0198 agree fairly well for the time period 1955-82 covered by both cores. d18O values have increased during most of the 20th ... : Supplement to: Schlosser, Elisabeth; Oerter, Hans (2002): Shallow firn cores from Neumayer, Ekströmisen, Antarctica: a comparison of accumulation rates and stable-isotope ratios. Annals of Glaciology, 35, 91-96 ... Article in Journal/Newspaper Antarc* Antarctica DataCite Metadata Store (German National Library of Science and Technology) Ekströmisen ENVELOPE(-8.000,-8.000,-71.000,-71.000) Neumayer Neumayer Station
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Ice drill
Stake
Firn auger
Neumayer_based
EPICA_DML3
NEUMAYER III
Neumayer Station WMO89002
Glaciology @ AWI AWI_Glac
spellingShingle Ice drill
Stake
Firn auger
Neumayer_based
EPICA_DML3
NEUMAYER III
Neumayer Station WMO89002
Glaciology @ AWI AWI_Glac
Schlosser, Elisabeth
Oerter, Hans
Comparison of accumulation rates and stable isotope ratios ...
topic_facet Ice drill
Stake
Firn auger
Neumayer_based
EPICA_DML3
NEUMAYER III
Neumayer Station WMO89002
Glaciology @ AWI AWI_Glac
description Since 1979/80, glaciological studies have been carried out at Ekströmisen, Antarctica, including accumulation-stake measurements, snow-pit and shallow-firn-core studies. Snowstratigraphy, chemical properties and stable-isotope ratios (d18O) were investigated. This study focuses on three cores taken between 1982 and 1998. The 1998 core was dated using dielectric profiling, d18O profiles and stake measurements. Accumulation rates showhigh interannual and spatial variability due to the extreme wind influence. No significant trend was found for the last 50 years; during the first half of the 20th century, accumulation decreased. The high spatial and interannual variability, however, means that trends must be interpreted with care. In spite of the highly irregular accumulation distribution, stable-isotope ratios show little spatial variability. The mean annual d18O values of cores B04 and FB0198 agree fairly well for the time period 1955-82 covered by both cores. d18O values have increased during most of the 20th ... : Supplement to: Schlosser, Elisabeth; Oerter, Hans (2002): Shallow firn cores from Neumayer, Ekströmisen, Antarctica: a comparison of accumulation rates and stable-isotope ratios. Annals of Glaciology, 35, 91-96 ...
format Article in Journal/Newspaper
author Schlosser, Elisabeth
Oerter, Hans
author_facet Schlosser, Elisabeth
Oerter, Hans
author_sort Schlosser, Elisabeth
title Comparison of accumulation rates and stable isotope ratios ...
title_short Comparison of accumulation rates and stable isotope ratios ...
title_full Comparison of accumulation rates and stable isotope ratios ...
title_fullStr Comparison of accumulation rates and stable isotope ratios ...
title_full_unstemmed Comparison of accumulation rates and stable isotope ratios ...
title_sort comparison of accumulation rates and stable isotope ratios ...
publisher PANGAEA
publishDate 2002
url https://dx.doi.org/10.1594/pangaea.690398
https://doi.pangaea.de/10.1594/PANGAEA.690398
long_lat ENVELOPE(-8.000,-8.000,-71.000,-71.000)
geographic Ekströmisen
Neumayer
Neumayer Station
geographic_facet Ekströmisen
Neumayer
Neumayer Station
genre Antarc*
Antarctica
genre_facet Antarc*
Antarctica
op_relation https://dx.doi.org/10.3189/172756402781816915
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.69039810.3189/172756402781816915
_version_ 1768379530415702016