Climatic signals from 76 shallow firn cores in Dronning Maud Land, East Antarctica

The spatial and temporal distribution of SMB and δ18O were investigated utilizing a set of 76 firn cores retrieved by various expeditions during the past three decades in Dronning Maud Land, East Antarctica. It was the first comprehensive study of this unique data set. The large number of cores was...

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Bibliographic Details
Main Author: Altnau, Sebastian
Format: Master Thesis
Language:English
Published: 2014
Subjects:
SAM
Online Access:https://resolver.obvsg.at/urn:nbn:at:at-ubi:1-636
id ftunivinnsbruck:oai:diglib.uibk.ac.at/:148960
record_format openpolar
spelling ftunivinnsbruck:oai:diglib.uibk.ac.at/:148960 2023-10-01T03:51:27+02:00 Climatic signals from 76 shallow firn cores in Dronning Maud Land, East Antarctica Altnau, Sebastian Ostantarktis 38.82 RY 70387 UI:GA:MG 2014 VII, 97 S. text/html image/jpeg graph. Darst., Kt. https://resolver.obvsg.at/urn:nbn:at:at-ubi:1-636 eng eng vignette : https://diglib.uibk.ac.at/titlepage/urn/urn:nbn:at:at-ubi:1-636/128 http://media.obvsg.at/AC11359055-4001 urn:nbn:at:at-ubi:1-636 https://resolver.obvsg.at/urn:nbn:at:at-ubi:1-636 local:990117517690203331 system:AC11359055 InC_1 Massenbilanz Wasser Isotop Dronning Maud Land East Antarctica shallow firn cores stable isotopes surface mass balance signal-to-noise ratio climatic signals SAM Text Thesis MasterThesis 2014 ftunivinnsbruck 2023-09-04T19:45:08Z The spatial and temporal distribution of SMB and δ18O were investigated utilizing a set of 76 firn cores retrieved by various expeditions during the past three decades in Dronning Maud Land, East Antarctica. It was the first comprehensive study of this unique data set. The large number of cores was used to calculate stacked records of SMB and δ18O, which considerably increased the signal-to-noise ratio compared to earlier studies and facilitated the detection of climatic signals. Considerable differences between cores from the interior plateau and the coastal cores were found. Whereas the δ18O of both the plateau and the ice shelf cores exhibit a slight positive trend in both surface mass balance and δ18O over the second half of the 20th century, the SMB has a negative trend in the ice shelf cores, but increases on the plateau in the corresponding period. Comparison with meteorological data from Neumayer Station revealed that for the ice shelf regions atmospheric dynamic effects are more important than thermodynamics, while on the plateau, the temporal variations of SMB and δ18O occur mostly in parallel, thus can be explained by thermodynamic effects. The Southern Annular Mode (SAM) exhibits a positive trend since the mid-1960s, which is assumed to lead to a cooling of East Antarctica. This is not confirmed by the firn core data. Changes in the atmospheric circulation that result in a changed seasonal distribution of precipitation/accumulation could partly explain the observed features in the ice shelf cores. by Sebastian Altnau Innsbruck, Univ., Masterarb., 2014 Master Thesis Antarc* Antarctica Dronning Maud Land East Antarctica Ice Shelf University of Innsbruck: Digital Library (Universitäts- und Landesbibliothek Tirol) Dronning Maud Land East Antarctica Neumayer Neumayer Station
institution Open Polar
collection University of Innsbruck: Digital Library (Universitäts- und Landesbibliothek Tirol)
op_collection_id ftunivinnsbruck
language English
topic Massenbilanz
Wasser
Isotop
Dronning Maud Land
East Antarctica
shallow firn cores
stable isotopes
surface mass balance
signal-to-noise ratio
climatic signals
SAM
spellingShingle Massenbilanz
Wasser
Isotop
Dronning Maud Land
East Antarctica
shallow firn cores
stable isotopes
surface mass balance
signal-to-noise ratio
climatic signals
SAM
Altnau, Sebastian
Climatic signals from 76 shallow firn cores in Dronning Maud Land, East Antarctica
topic_facet Massenbilanz
Wasser
Isotop
Dronning Maud Land
East Antarctica
shallow firn cores
stable isotopes
surface mass balance
signal-to-noise ratio
climatic signals
SAM
description The spatial and temporal distribution of SMB and δ18O were investigated utilizing a set of 76 firn cores retrieved by various expeditions during the past three decades in Dronning Maud Land, East Antarctica. It was the first comprehensive study of this unique data set. The large number of cores was used to calculate stacked records of SMB and δ18O, which considerably increased the signal-to-noise ratio compared to earlier studies and facilitated the detection of climatic signals. Considerable differences between cores from the interior plateau and the coastal cores were found. Whereas the δ18O of both the plateau and the ice shelf cores exhibit a slight positive trend in both surface mass balance and δ18O over the second half of the 20th century, the SMB has a negative trend in the ice shelf cores, but increases on the plateau in the corresponding period. Comparison with meteorological data from Neumayer Station revealed that for the ice shelf regions atmospheric dynamic effects are more important than thermodynamics, while on the plateau, the temporal variations of SMB and δ18O occur mostly in parallel, thus can be explained by thermodynamic effects. The Southern Annular Mode (SAM) exhibits a positive trend since the mid-1960s, which is assumed to lead to a cooling of East Antarctica. This is not confirmed by the firn core data. Changes in the atmospheric circulation that result in a changed seasonal distribution of precipitation/accumulation could partly explain the observed features in the ice shelf cores. by Sebastian Altnau Innsbruck, Univ., Masterarb., 2014
format Master Thesis
author Altnau, Sebastian
author_facet Altnau, Sebastian
author_sort Altnau, Sebastian
title Climatic signals from 76 shallow firn cores in Dronning Maud Land, East Antarctica
title_short Climatic signals from 76 shallow firn cores in Dronning Maud Land, East Antarctica
title_full Climatic signals from 76 shallow firn cores in Dronning Maud Land, East Antarctica
title_fullStr Climatic signals from 76 shallow firn cores in Dronning Maud Land, East Antarctica
title_full_unstemmed Climatic signals from 76 shallow firn cores in Dronning Maud Land, East Antarctica
title_sort climatic signals from 76 shallow firn cores in dronning maud land, east antarctica
publishDate 2014
url https://resolver.obvsg.at/urn:nbn:at:at-ubi:1-636
op_coverage Ostantarktis
38.82
RY 70387
UI:GA:MG
geographic Dronning Maud Land
East Antarctica
Neumayer
Neumayer Station
geographic_facet Dronning Maud Land
East Antarctica
Neumayer
Neumayer Station
genre Antarc*
Antarctica
Dronning Maud Land
East Antarctica
Ice Shelf
genre_facet Antarc*
Antarctica
Dronning Maud Land
East Antarctica
Ice Shelf
op_relation vignette : https://diglib.uibk.ac.at/titlepage/urn/urn:nbn:at:at-ubi:1-636/128
http://media.obvsg.at/AC11359055-4001
urn:nbn:at:at-ubi:1-636
https://resolver.obvsg.at/urn:nbn:at:at-ubi:1-636
local:990117517690203331
system:AC11359055
op_rights InC_1
_version_ 1778535207039664128