Beryllium-10 transport to Antarctica: Results from seasonally resolved observations and modeling
Cosmogenic 10Be measured in polar ice cores has important application in the reconstruction of past solar activity. However, the processes controlling its atmospheric transport and deposition to the ice sheets are not fully understood. Here we use the seasonal changes in 10Be concentrations in a 10...
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ftunivtasecite:oai:ecite.utas.edu.au:76821 2023-05-15T14:02:30+02:00 Beryllium-10 transport to Antarctica: Results from seasonally resolved observations and modeling Pedro, JB Heikkila, UE Klekociuk, A Smith, AM van Ommen, TD Curran, MAJ 2011 application/pdf https://doi.org/10.1029/2011JD016530 http://ecite.utas.edu.au/76821 en eng Amer Geophysical Union http://ecite.utas.edu.au/76821/1/Pedro_JGR_2011-observed and modeled 10Be seasonality.pdf http://dx.doi.org/10.1029/2011JD016530 Pedro, JB and Heikkila, UE and Klekociuk, A and Smith, AM and van Ommen, TD and Curran, MAJ, Beryllium-10 transport to Antarctica: Results from seasonally resolved observations and modeling, Journal of Geophysical Research, 116, (D23) Article D23120. ISSN 2156-2202 (2011) [Refereed Article] http://ecite.utas.edu.au/76821 Earth Sciences Physical Geography and Environmental Geoscience Glaciology Refereed Article PeerReviewed 2011 ftunivtasecite https://doi.org/10.1029/2011JD016530 2019-12-13T21:43:03Z Cosmogenic 10Be measured in polar ice cores has important application in the reconstruction of past solar activity. However, the processes controlling its atmospheric transport and deposition to the ice sheets are not fully understood. Here we use the seasonal changes in 10Be concentrations in a 10 year monthly resolved ice core record from the Law Dome site (East Antarctica) in conjunction with ECHAM5-HAM general circulation model (GCM) simulations of 10Be and 7Be deposition as tools to examine this problem. Maximum 10Be concentrations are observed in the ice core during the austral late summer to early autumn (summer-autumn), while minimum concentrations are observed during the austral winter. The GCM simulations, corroborated by earlier observations of 10Be:7Be ratios in Antarctica from the Georg von Neumayer air sampling station, suggest that the 10Be concentration maximum is linked to direct input of stratospheric 10Be from the Antarctic stratosphere to the lower levels of the Antarctic troposphere during the austral summer-autumn. This result contrasts with the modeled transport of 10Be to Greenland, where the seasonal maximum in stratospheric input is seen in the late winter to spring, synchronous with the timing of the seasonal maximum in midlatitude stratosphere to troposphere exchange. Our results suggest that a different combination of processes is responsible for the transport of 10Be to the Antarctic and Greenland ice sheets. Article in Journal/Newspaper Antarc* Antarctic Antarctica East Antarctica Greenland ice core eCite UTAS (University of Tasmania) Antarctic Austral East Antarctica Greenland Law Dome ENVELOPE(112.833,112.833,-66.733,-66.733) Neumayer The Antarctic Journal of Geophysical Research: Atmospheres 116 D23 n/a n/a |
institution |
Open Polar |
collection |
eCite UTAS (University of Tasmania) |
op_collection_id |
ftunivtasecite |
language |
English |
topic |
Earth Sciences Physical Geography and Environmental Geoscience Glaciology |
spellingShingle |
Earth Sciences Physical Geography and Environmental Geoscience Glaciology Pedro, JB Heikkila, UE Klekociuk, A Smith, AM van Ommen, TD Curran, MAJ Beryllium-10 transport to Antarctica: Results from seasonally resolved observations and modeling |
topic_facet |
Earth Sciences Physical Geography and Environmental Geoscience Glaciology |
description |
Cosmogenic 10Be measured in polar ice cores has important application in the reconstruction of past solar activity. However, the processes controlling its atmospheric transport and deposition to the ice sheets are not fully understood. Here we use the seasonal changes in 10Be concentrations in a 10 year monthly resolved ice core record from the Law Dome site (East Antarctica) in conjunction with ECHAM5-HAM general circulation model (GCM) simulations of 10Be and 7Be deposition as tools to examine this problem. Maximum 10Be concentrations are observed in the ice core during the austral late summer to early autumn (summer-autumn), while minimum concentrations are observed during the austral winter. The GCM simulations, corroborated by earlier observations of 10Be:7Be ratios in Antarctica from the Georg von Neumayer air sampling station, suggest that the 10Be concentration maximum is linked to direct input of stratospheric 10Be from the Antarctic stratosphere to the lower levels of the Antarctic troposphere during the austral summer-autumn. This result contrasts with the modeled transport of 10Be to Greenland, where the seasonal maximum in stratospheric input is seen in the late winter to spring, synchronous with the timing of the seasonal maximum in midlatitude stratosphere to troposphere exchange. Our results suggest that a different combination of processes is responsible for the transport of 10Be to the Antarctic and Greenland ice sheets. |
format |
Article in Journal/Newspaper |
author |
Pedro, JB Heikkila, UE Klekociuk, A Smith, AM van Ommen, TD Curran, MAJ |
author_facet |
Pedro, JB Heikkila, UE Klekociuk, A Smith, AM van Ommen, TD Curran, MAJ |
author_sort |
Pedro, JB |
title |
Beryllium-10 transport to Antarctica: Results from seasonally resolved observations and modeling |
title_short |
Beryllium-10 transport to Antarctica: Results from seasonally resolved observations and modeling |
title_full |
Beryllium-10 transport to Antarctica: Results from seasonally resolved observations and modeling |
title_fullStr |
Beryllium-10 transport to Antarctica: Results from seasonally resolved observations and modeling |
title_full_unstemmed |
Beryllium-10 transport to Antarctica: Results from seasonally resolved observations and modeling |
title_sort |
beryllium-10 transport to antarctica: results from seasonally resolved observations and modeling |
publisher |
Amer Geophysical Union |
publishDate |
2011 |
url |
https://doi.org/10.1029/2011JD016530 http://ecite.utas.edu.au/76821 |
long_lat |
ENVELOPE(112.833,112.833,-66.733,-66.733) |
geographic |
Antarctic Austral East Antarctica Greenland Law Dome Neumayer The Antarctic |
geographic_facet |
Antarctic Austral East Antarctica Greenland Law Dome Neumayer The Antarctic |
genre |
Antarc* Antarctic Antarctica East Antarctica Greenland ice core |
genre_facet |
Antarc* Antarctic Antarctica East Antarctica Greenland ice core |
op_relation |
http://ecite.utas.edu.au/76821/1/Pedro_JGR_2011-observed and modeled 10Be seasonality.pdf http://dx.doi.org/10.1029/2011JD016530 Pedro, JB and Heikkila, UE and Klekociuk, A and Smith, AM and van Ommen, TD and Curran, MAJ, Beryllium-10 transport to Antarctica: Results from seasonally resolved observations and modeling, Journal of Geophysical Research, 116, (D23) Article D23120. ISSN 2156-2202 (2011) [Refereed Article] http://ecite.utas.edu.au/76821 |
op_doi |
https://doi.org/10.1029/2011JD016530 |
container_title |
Journal of Geophysical Research: Atmospheres |
container_volume |
116 |
container_issue |
D23 |
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n/a |
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n/a |
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1766272789576155136 |