Annals of Glaciology 44 2006 429 Covariation of sea ice and methanesulphonic acid in
ABSTRACT. Sea ice plays an important role in ocean–atmosphere heat exchange, global albedo and the marine ecosystem. Knowledge of variation in sea-ice extent is essential in order to understand past climates, and to model possible future climate scenarios. This paper presents results from a short fi...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.430.1275 2023-05-15T13:43:47+02:00 Annals of Glaciology 44 2006 429 Covariation of sea ice and methanesulphonic acid in Wilhelm Ii L East Antarctica Annette F. M. Foster Mark A. J. Curran Barbara T. Smith Tas D. Van Ommen Vin I. Morgan The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.430.1275 http://www.igsoc.org/annals/44/a44a010.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.430.1275 http://www.igsoc.org/annals/44/a44a010.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.igsoc.org/annals/44/a44a010.pdf text ftciteseerx 2016-01-08T04:36:47Z ABSTRACT. Sea ice plays an important role in ocean–atmosphere heat exchange, global albedo and the marine ecosystem. Knowledge of variation in sea-ice extent is essential in order to understand past climates, and to model possible future climate scenarios. This paper presents results from a short firn core spanning 15 years collected from near Mount Brown, Wilhelm II Land, East Antarctica. Variations of methanesulphonic acid (MSA) at Mount Brown were positively correlated with sea-ice extent from the coastal region surrounding Mount Brown (60–1208 E) and from around the entire Antarctic coast (0–3608 E). Previous results from Law Dome identified this MSA–sea-ice relationship and proposed it as an Antarctic sea-ice proxy (Curran and others, 2003), with the strongest results found for the local Law Dome region. Our data provide supporting evidence for the Law Dome proxy (at another site in East Antarctica), but a deeper Mount Brown ice core is required to confirm the sea-ice decline suggested by Curran and others (2003). Results also indicate that this deeper record may also provide a more circum-Antarctic sea-ice proxy. Text Antarc* Antarctic Antarctica East Antarctica ice core Sea ice Wilhelm II Land Unknown Antarctic East Antarctica Law Dome ENVELOPE(112.833,112.833,-66.733,-66.733) Mount Brown ENVELOPE(86.000,86.000,-68.617,-68.617) Wilhelm II Land ENVELOPE(90.000,90.000,-67.000,-67.000) |
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English |
description |
ABSTRACT. Sea ice plays an important role in ocean–atmosphere heat exchange, global albedo and the marine ecosystem. Knowledge of variation in sea-ice extent is essential in order to understand past climates, and to model possible future climate scenarios. This paper presents results from a short firn core spanning 15 years collected from near Mount Brown, Wilhelm II Land, East Antarctica. Variations of methanesulphonic acid (MSA) at Mount Brown were positively correlated with sea-ice extent from the coastal region surrounding Mount Brown (60–1208 E) and from around the entire Antarctic coast (0–3608 E). Previous results from Law Dome identified this MSA–sea-ice relationship and proposed it as an Antarctic sea-ice proxy (Curran and others, 2003), with the strongest results found for the local Law Dome region. Our data provide supporting evidence for the Law Dome proxy (at another site in East Antarctica), but a deeper Mount Brown ice core is required to confirm the sea-ice decline suggested by Curran and others (2003). Results also indicate that this deeper record may also provide a more circum-Antarctic sea-ice proxy. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Wilhelm Ii L East Antarctica Annette F. M. Foster Mark A. J. Curran Barbara T. Smith Tas D. Van Ommen Vin I. Morgan |
spellingShingle |
Wilhelm Ii L East Antarctica Annette F. M. Foster Mark A. J. Curran Barbara T. Smith Tas D. Van Ommen Vin I. Morgan Annals of Glaciology 44 2006 429 Covariation of sea ice and methanesulphonic acid in |
author_facet |
Wilhelm Ii L East Antarctica Annette F. M. Foster Mark A. J. Curran Barbara T. Smith Tas D. Van Ommen Vin I. Morgan |
author_sort |
Wilhelm Ii L |
title |
Annals of Glaciology 44 2006 429 Covariation of sea ice and methanesulphonic acid in |
title_short |
Annals of Glaciology 44 2006 429 Covariation of sea ice and methanesulphonic acid in |
title_full |
Annals of Glaciology 44 2006 429 Covariation of sea ice and methanesulphonic acid in |
title_fullStr |
Annals of Glaciology 44 2006 429 Covariation of sea ice and methanesulphonic acid in |
title_full_unstemmed |
Annals of Glaciology 44 2006 429 Covariation of sea ice and methanesulphonic acid in |
title_sort |
annals of glaciology 44 2006 429 covariation of sea ice and methanesulphonic acid in |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.430.1275 http://www.igsoc.org/annals/44/a44a010.pdf |
long_lat |
ENVELOPE(112.833,112.833,-66.733,-66.733) ENVELOPE(86.000,86.000,-68.617,-68.617) ENVELOPE(90.000,90.000,-67.000,-67.000) |
geographic |
Antarctic East Antarctica Law Dome Mount Brown Wilhelm II Land |
geographic_facet |
Antarctic East Antarctica Law Dome Mount Brown Wilhelm II Land |
genre |
Antarc* Antarctic Antarctica East Antarctica ice core Sea ice Wilhelm II Land |
genre_facet |
Antarc* Antarctic Antarctica East Antarctica ice core Sea ice Wilhelm II Land |
op_source |
http://www.igsoc.org/annals/44/a44a010.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.430.1275 http://www.igsoc.org/annals/44/a44a010.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766193211327381504 |