Isotope values of fresh snow samples and daily temperature from Neumayer station in the period 1981-2000 ...

The relationship between d18O and air temperature at Neumayer station, Ekströmisen, Antarctica, was investigated using fresh-snow samples from the time period 1981-2000. A trajectory model that calculated 5 day-backward trajectories was used to study the influence of different synoptic weather situa...

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Bibliographic Details
Main Authors: Schlosser, Elisabeth, Reijmer, Carleen H, Oerter, Hans, Graf, Wolfgang
Format: Dataset
Language:English
Published: PANGAEA 2003
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.119750
https://doi.pangaea.de/10.1594/PANGAEA.119750
id ftdatacite:10.1594/pangaea.119750
record_format openpolar
spelling ftdatacite:10.1594/pangaea.119750 2023-06-11T04:07:13+02:00 Isotope values of fresh snow samples and daily temperature from Neumayer station in the period 1981-2000 ... Schlosser, Elisabeth Reijmer, Carleen H Oerter, Hans Graf, Wolfgang 2003 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.119750 https://doi.pangaea.de/10.1594/PANGAEA.119750 en eng PANGAEA https://dx.doi.org/10.3189/172756404781814276 https://dx.doi.org/10.3189/002214308784408991 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 DATE/TIME δ Deuterium δ18O, water Deuterium excess Temperature, air Research station Calculated Neumayer_based NEUMAYER III Glaciology @ AWI AWI_Glac Supplementary Dataset Dataset dataset 2003 ftdatacite https://doi.org/10.1594/pangaea.11975010.3189/17275640478181427610.3189/002214308784408991 2023-06-01T11:44:30Z The relationship between d18O and air temperature at Neumayer station, Ekströmisen, Antarctica, was investigated using fresh-snow samples from the time period 1981-2000. A trajectory model that calculated 5 day-backward trajectories was used to study the influence of different synoptic weather situations and thus of different moisture sources on this correlation. Generally a high correlation between air temperature and d18O was found, but the quality of the d18O-T relationship varied with the different trajectory classes. Additionally, the sea-ice coverage on the travel path of the moist air was considered. The amount of open ocean water underneath the trajectory has a large influence on the d18O-T relationship. For trajectories that lead completely above open water, no significant correlation between d18O and T was found, because mixing with air masses containing additionally evaporated water vapour from the ocean influences the isotope ratio of precipitation. A very high correlation, however, was found for ... : Isotope measurements 1981-1999 by GSF, 2000 by AWI. ... Dataset Antarc* Antarctica Sea ice 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 DATE/TIME
δ Deuterium
δ18O, water
Deuterium excess
Temperature, air
Research station
Calculated
Neumayer_based
NEUMAYER III
Glaciology @ AWI AWI_Glac
spellingShingle DATE/TIME
δ Deuterium
δ18O, water
Deuterium excess
Temperature, air
Research station
Calculated
Neumayer_based
NEUMAYER III
Glaciology @ AWI AWI_Glac
Schlosser, Elisabeth
Reijmer, Carleen H
Oerter, Hans
Graf, Wolfgang
Isotope values of fresh snow samples and daily temperature from Neumayer station in the period 1981-2000 ...
topic_facet DATE/TIME
δ Deuterium
δ18O, water
Deuterium excess
Temperature, air
Research station
Calculated
Neumayer_based
NEUMAYER III
Glaciology @ AWI AWI_Glac
description The relationship between d18O and air temperature at Neumayer station, Ekströmisen, Antarctica, was investigated using fresh-snow samples from the time period 1981-2000. A trajectory model that calculated 5 day-backward trajectories was used to study the influence of different synoptic weather situations and thus of different moisture sources on this correlation. Generally a high correlation between air temperature and d18O was found, but the quality of the d18O-T relationship varied with the different trajectory classes. Additionally, the sea-ice coverage on the travel path of the moist air was considered. The amount of open ocean water underneath the trajectory has a large influence on the d18O-T relationship. For trajectories that lead completely above open water, no significant correlation between d18O and T was found, because mixing with air masses containing additionally evaporated water vapour from the ocean influences the isotope ratio of precipitation. A very high correlation, however, was found for ... : Isotope measurements 1981-1999 by GSF, 2000 by AWI. ...
format Dataset
author Schlosser, Elisabeth
Reijmer, Carleen H
Oerter, Hans
Graf, Wolfgang
author_facet Schlosser, Elisabeth
Reijmer, Carleen H
Oerter, Hans
Graf, Wolfgang
author_sort Schlosser, Elisabeth
title Isotope values of fresh snow samples and daily temperature from Neumayer station in the period 1981-2000 ...
title_short Isotope values of fresh snow samples and daily temperature from Neumayer station in the period 1981-2000 ...
title_full Isotope values of fresh snow samples and daily temperature from Neumayer station in the period 1981-2000 ...
title_fullStr Isotope values of fresh snow samples and daily temperature from Neumayer station in the period 1981-2000 ...
title_full_unstemmed Isotope values of fresh snow samples and daily temperature from Neumayer station in the period 1981-2000 ...
title_sort isotope values of fresh snow samples and daily temperature from neumayer station in the period 1981-2000 ...
publisher PANGAEA
publishDate 2003
url https://dx.doi.org/10.1594/pangaea.119750
https://doi.pangaea.de/10.1594/PANGAEA.119750
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
Sea ice
genre_facet Antarc*
Antarctica
Sea ice
op_relation https://dx.doi.org/10.3189/172756404781814276
https://dx.doi.org/10.3189/002214308784408991
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.11975010.3189/17275640478181427610.3189/002214308784408991
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