Surface mass balance and stable oxygen isotope ratios from shallow firn cores on Fimbulisen, East Antarctica
Source at https://doi.org/10.3189/2012AoG60A102 . The mass balance of Antarctica is one of the crucial factors for determining sea-level change in a warming climate. The marginal zones of the continent, namely the ice shelves, are most sensitive to climate change. During the 2009/10 austral summer a...
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Online Access: | https://hdl.handle.net/10037/16740 https://doi.org/10.3189/2012AoG60A102 |
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ftunivtroemsoe:oai:munin.uit.no:10037/16740 2023-05-15T13:29:14+02:00 Surface mass balance and stable oxygen isotope ratios from shallow firn cores on Fimbulisen, East Antarctica Schlosser, E Anschütz, Helgard Isaksson, E. Martma, T Divine, Dmitry V Nøst, O.-A. 2012 https://hdl.handle.net/10037/16740 https://doi.org/10.3189/2012AoG60A102 eng eng Cambridge University Press Annals of Glaciology Schlosser E, Anschütz H, Isaksson E, Martma T, Divine Dv, Nost. Surface mass balance and stable oxygen isotope ratios from shallow firn cores on Fimbulisen, East Antarctica. Annals of Glaciology. 2012;53(60):70-78 FRIDAID 1020605 doi:10.3189/2012AoG60A102 0260-3055 1727-5644 https://hdl.handle.net/10037/16740 openAccess VDP::Mathematics and natural science: 400::Geosciences: 450::Quaternary geology glaciology: 465 VDP::Matematikk og Naturvitenskap: 400::Geofag: 450::Kvartærgeologi glasiologi: 465 Journal article Tidsskriftartikkel Peer reviewed 2012 ftunivtroemsoe https://doi.org/10.3189/2012AoG60A102 2021-06-25T17:56:56Z Source at https://doi.org/10.3189/2012AoG60A102 . The mass balance of Antarctica is one of the crucial factors for determining sea-level change in a warming climate. The marginal zones of the continent, namely the ice shelves, are most sensitive to climate change. During the 2009/10 austral summer an extensive glaciological field campaign was carried out on Fimbulisen, an ice shelf in East Antarctica, to investigate its recent surface mass balance. Shallow (10–18 m) firn cores were drilled and accumulation rates and stable-isotope ratios determined. For firn-core dating, two different methods were compared: (1) seasonal variations of stable oxygen isotope ratios (δ 18 O), and (2) dielectric profiling, including using the volcanic eruptions of Pinatubo, Philippines (1991), and El Chichόn, Mexico (1982), as time markers. The mean annual accumulation for the period 1992–2009 ranges from 298 to 349 mmw.e. a –1 . The interannual variability at the drilling sites is >30%. Accumulation rates show a weak decreasing trend during the past 20–30 years, which is statistically significant only for one of the cores. Stable-isotope ratios were compared to the snowfall temperature of Neumayer station. Neither the temperatures nor the δ 18 O values show any trend for the investigated time period. Article in Journal/Newspaper Annals of Glaciology Antarc* Antarctica East Antarctica Ice Shelf Ice Shelves University of Tromsø: Munin Open Research Archive Austral East Antarctica Fimbulisen ENVELOPE(-0.500,-0.500,-70.750,-70.750) Neumayer Neumayer Station Annals of Glaciology 53 60 70 78 |
institution |
Open Polar |
collection |
University of Tromsø: Munin Open Research Archive |
op_collection_id |
ftunivtroemsoe |
language |
English |
topic |
VDP::Mathematics and natural science: 400::Geosciences: 450::Quaternary geology glaciology: 465 VDP::Matematikk og Naturvitenskap: 400::Geofag: 450::Kvartærgeologi glasiologi: 465 |
spellingShingle |
VDP::Mathematics and natural science: 400::Geosciences: 450::Quaternary geology glaciology: 465 VDP::Matematikk og Naturvitenskap: 400::Geofag: 450::Kvartærgeologi glasiologi: 465 Schlosser, E Anschütz, Helgard Isaksson, E. Martma, T Divine, Dmitry V Nøst, O.-A. Surface mass balance and stable oxygen isotope ratios from shallow firn cores on Fimbulisen, East Antarctica |
topic_facet |
VDP::Mathematics and natural science: 400::Geosciences: 450::Quaternary geology glaciology: 465 VDP::Matematikk og Naturvitenskap: 400::Geofag: 450::Kvartærgeologi glasiologi: 465 |
description |
Source at https://doi.org/10.3189/2012AoG60A102 . The mass balance of Antarctica is one of the crucial factors for determining sea-level change in a warming climate. The marginal zones of the continent, namely the ice shelves, are most sensitive to climate change. During the 2009/10 austral summer an extensive glaciological field campaign was carried out on Fimbulisen, an ice shelf in East Antarctica, to investigate its recent surface mass balance. Shallow (10–18 m) firn cores were drilled and accumulation rates and stable-isotope ratios determined. For firn-core dating, two different methods were compared: (1) seasonal variations of stable oxygen isotope ratios (δ 18 O), and (2) dielectric profiling, including using the volcanic eruptions of Pinatubo, Philippines (1991), and El Chichόn, Mexico (1982), as time markers. The mean annual accumulation for the period 1992–2009 ranges from 298 to 349 mmw.e. a –1 . The interannual variability at the drilling sites is >30%. Accumulation rates show a weak decreasing trend during the past 20–30 years, which is statistically significant only for one of the cores. Stable-isotope ratios were compared to the snowfall temperature of Neumayer station. Neither the temperatures nor the δ 18 O values show any trend for the investigated time period. |
format |
Article in Journal/Newspaper |
author |
Schlosser, E Anschütz, Helgard Isaksson, E. Martma, T Divine, Dmitry V Nøst, O.-A. |
author_facet |
Schlosser, E Anschütz, Helgard Isaksson, E. Martma, T Divine, Dmitry V Nøst, O.-A. |
author_sort |
Schlosser, E |
title |
Surface mass balance and stable oxygen isotope ratios from shallow firn cores on Fimbulisen, East Antarctica |
title_short |
Surface mass balance and stable oxygen isotope ratios from shallow firn cores on Fimbulisen, East Antarctica |
title_full |
Surface mass balance and stable oxygen isotope ratios from shallow firn cores on Fimbulisen, East Antarctica |
title_fullStr |
Surface mass balance and stable oxygen isotope ratios from shallow firn cores on Fimbulisen, East Antarctica |
title_full_unstemmed |
Surface mass balance and stable oxygen isotope ratios from shallow firn cores on Fimbulisen, East Antarctica |
title_sort |
surface mass balance and stable oxygen isotope ratios from shallow firn cores on fimbulisen, east antarctica |
publisher |
Cambridge University Press |
publishDate |
2012 |
url |
https://hdl.handle.net/10037/16740 https://doi.org/10.3189/2012AoG60A102 |
long_lat |
ENVELOPE(-0.500,-0.500,-70.750,-70.750) |
geographic |
Austral East Antarctica Fimbulisen Neumayer Neumayer Station |
geographic_facet |
Austral East Antarctica Fimbulisen Neumayer Neumayer Station |
genre |
Annals of Glaciology Antarc* Antarctica East Antarctica Ice Shelf Ice Shelves |
genre_facet |
Annals of Glaciology Antarc* Antarctica East Antarctica Ice Shelf Ice Shelves |
op_relation |
Annals of Glaciology Schlosser E, Anschütz H, Isaksson E, Martma T, Divine Dv, Nost. Surface mass balance and stable oxygen isotope ratios from shallow firn cores on Fimbulisen, East Antarctica. Annals of Glaciology. 2012;53(60):70-78 FRIDAID 1020605 doi:10.3189/2012AoG60A102 0260-3055 1727-5644 https://hdl.handle.net/10037/16740 |
op_rights |
openAccess |
op_doi |
https://doi.org/10.3189/2012AoG60A102 |
container_title |
Annals of Glaciology |
container_volume |
53 |
container_issue |
60 |
container_start_page |
70 |
op_container_end_page |
78 |
_version_ |
1765999424351240192 |