Antarctic iceberg distribution and dissolution from ship-based observations

The Australian Antarctic Program’s iceberg dataset (from ship-based observations), including information from the austral summer seasons 1984/85 to 1999/2000, is examined and used to extend earlier studies. Using ‘snapshots’ of the iceberg population to provide an idea of the iceberg life cycle, the...

Full description

Bibliographic Details
Published in:Journal of Glaciology
Main Authors: Jacka, TH, Giles, AB
Format: Article in Journal/Newspaper
Language:English
Published: International Glaciological Society 2007
Subjects:
Online Access:https://eprints.utas.edu.au/4011/
https://eprints.utas.edu.au/4011/1/4011.pdf
https://doi.org/10.3189/002214307783258521
id ftunivtasmania:oai:eprints.utas.edu.au:4011
record_format openpolar
spelling ftunivtasmania:oai:eprints.utas.edu.au:4011 2023-05-15T13:36:46+02:00 Antarctic iceberg distribution and dissolution from ship-based observations Jacka, TH Giles, AB 2007 application/pdf https://eprints.utas.edu.au/4011/ https://eprints.utas.edu.au/4011/1/4011.pdf https://doi.org/10.3189/002214307783258521 en eng International Glaciological Society https://eprints.utas.edu.au/4011/1/4011.pdf Jacka, TH and Giles, AB 2007 , 'Antarctic iceberg distribution and dissolution from ship-based observations' , Journal of Glaciology, vol. 53, no. 182 , pp. 341-356 , doi:10.3189/002214307783258521 <http://dx.doi.org/10.3189/002214307783258521>. cc_utas 260115 Glaciology Article PeerReviewed 2007 ftunivtasmania https://doi.org/10.3189/002214307783258521 2020-05-30T07:17:53Z The Australian Antarctic Program’s iceberg dataset (from ship-based observations), including information from the austral summer seasons 1984/85 to 1999/2000, is examined and used to extend earlier studies. Using ‘snapshots’ of the iceberg population to provide an idea of the iceberg life cycle, the distribution of icebergs between 60 and 1508 E is discussed in terms of calving regions and ocean currents. Temporal changes are also examined. The discussion leads us to the point where we can define an area, bounded to the north by the maximum sea-ice limit and to the south by the Antarctic Divergence, in which icebergs are confined as they drift eastward. This allows estimation of total dissolution, in terms of iceberg numbers and volume, within 108 longitudinal sectors and, with knowledge of drift speeds, iceberg movement rates and freshwater input across the sector. Iceberg dissolution rates are found to be 0.03–0.05md–1 and the total mass contribution of fresh water to the ocean as the icebergs traverse our 308 of longitude study sector is 32 Gt. This amounts to a contribution equivalent to precipitation of 15.5cm a–1, accounting for 2% of the total iceberg discharge from the Antarctic ice sheet. Article in Journal/Newspaper Antarc* Antarctic Ice Sheet Iceberg* Journal of Glaciology Sea ice University of Tasmania: UTas ePrints Antarctic Austral The Antarctic Journal of Glaciology 53 182 341 356
institution Open Polar
collection University of Tasmania: UTas ePrints
op_collection_id ftunivtasmania
language English
topic 260115 Glaciology
spellingShingle 260115 Glaciology
Jacka, TH
Giles, AB
Antarctic iceberg distribution and dissolution from ship-based observations
topic_facet 260115 Glaciology
description The Australian Antarctic Program’s iceberg dataset (from ship-based observations), including information from the austral summer seasons 1984/85 to 1999/2000, is examined and used to extend earlier studies. Using ‘snapshots’ of the iceberg population to provide an idea of the iceberg life cycle, the distribution of icebergs between 60 and 1508 E is discussed in terms of calving regions and ocean currents. Temporal changes are also examined. The discussion leads us to the point where we can define an area, bounded to the north by the maximum sea-ice limit and to the south by the Antarctic Divergence, in which icebergs are confined as they drift eastward. This allows estimation of total dissolution, in terms of iceberg numbers and volume, within 108 longitudinal sectors and, with knowledge of drift speeds, iceberg movement rates and freshwater input across the sector. Iceberg dissolution rates are found to be 0.03–0.05md–1 and the total mass contribution of fresh water to the ocean as the icebergs traverse our 308 of longitude study sector is 32 Gt. This amounts to a contribution equivalent to precipitation of 15.5cm a–1, accounting for 2% of the total iceberg discharge from the Antarctic ice sheet.
format Article in Journal/Newspaper
author Jacka, TH
Giles, AB
author_facet Jacka, TH
Giles, AB
author_sort Jacka, TH
title Antarctic iceberg distribution and dissolution from ship-based observations
title_short Antarctic iceberg distribution and dissolution from ship-based observations
title_full Antarctic iceberg distribution and dissolution from ship-based observations
title_fullStr Antarctic iceberg distribution and dissolution from ship-based observations
title_full_unstemmed Antarctic iceberg distribution and dissolution from ship-based observations
title_sort antarctic iceberg distribution and dissolution from ship-based observations
publisher International Glaciological Society
publishDate 2007
url https://eprints.utas.edu.au/4011/
https://eprints.utas.edu.au/4011/1/4011.pdf
https://doi.org/10.3189/002214307783258521
geographic Antarctic
Austral
The Antarctic
geographic_facet Antarctic
Austral
The Antarctic
genre Antarc*
Antarctic
Ice Sheet
Iceberg*
Journal of Glaciology
Sea ice
genre_facet Antarc*
Antarctic
Ice Sheet
Iceberg*
Journal of Glaciology
Sea ice
op_relation https://eprints.utas.edu.au/4011/1/4011.pdf
Jacka, TH and Giles, AB 2007 , 'Antarctic iceberg distribution and dissolution from ship-based observations' , Journal of Glaciology, vol. 53, no. 182 , pp. 341-356 , doi:10.3189/002214307783258521 <http://dx.doi.org/10.3189/002214307783258521>.
op_rights cc_utas
op_doi https://doi.org/10.3189/002214307783258521
container_title Journal of Glaciology
container_volume 53
container_issue 182
container_start_page 341
op_container_end_page 356
_version_ 1766083732731592704