Quantifying dissolution rates of Antarctic icebergs in open water

Abstract At any one time 130 000 icebergs are afloat in the Southern Ocean; 97% of these are too small to be registered in current satellite-based databases, yet the melting of these small icebergs provides a major input to the Southern Ocean. We use a unique set of visual size observations of 53 00...

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Published in:Annals of Glaciology
Main Authors: Orheim, Olav, Giles, A. Barry, Jacka, T. H. (Jo), Moholdt, Geir
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2023
Subjects:
Online Access:http://dx.doi.org/10.1017/aog.2023.26
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0260305523000265
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spelling crcambridgeupr:10.1017/aog.2023.26 2024-06-09T07:38:27+00:00 Quantifying dissolution rates of Antarctic icebergs in open water Orheim, Olav Giles, A. Barry Jacka, T. H. (Jo) Moholdt, Geir 2023 http://dx.doi.org/10.1017/aog.2023.26 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0260305523000265 en eng Cambridge University Press (CUP) http://creativecommons.org/licenses/by/4.0/ Annals of Glaciology page 1-11 ISSN 0260-3055 1727-5644 journal-article 2023 crcambridgeupr https://doi.org/10.1017/aog.2023.26 2024-05-15T13:07:34Z Abstract At any one time 130 000 icebergs are afloat in the Southern Ocean; 97% of these are too small to be registered in current satellite-based databases, yet the melting of these small icebergs provides a major input to the Southern Ocean. We use a unique set of visual size observations of 53 000 icebergs in the South Atlantic Ocean, the SCAR International Iceberg Database, to derive average iceberg dissolution rates. Fracture into two parts is the dominant dissolution process for tabular icebergs, with an average half-life of 30 days for icebergs <4 km length and 60 days for larger icebergs. Complete shatter producing many icebergs <1 km length is rare. A side attrition rate of 0.23 m d −1 combined with drift speed of 6 km d −1 , or any proportional change in both numbers fits the observed changes in iceberg distribution. The largest injection into the Southern Ocean of fresh water and any iceberg-transported material takes place in a ~2.3 × 10⁶ km 2 zone extending east-northeast from the Antarctic Peninsula to the Greenwich meridian. The iceberg contribution to salinities and temperatures, with maximum contribution north of the Weddell Sea, differs in some regions, from those indicated by tracking large icebergs. Article in Journal/Newspaper Annals of Glaciology Antarc* Antarctic Antarctic Peninsula Iceberg* South Atlantic Ocean Southern Ocean Weddell Sea Cambridge University Press Antarctic Antarctic Peninsula Greenwich Southern Ocean The Antarctic Weddell Weddell Sea Annals of Glaciology 1 11
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description Abstract At any one time 130 000 icebergs are afloat in the Southern Ocean; 97% of these are too small to be registered in current satellite-based databases, yet the melting of these small icebergs provides a major input to the Southern Ocean. We use a unique set of visual size observations of 53 000 icebergs in the South Atlantic Ocean, the SCAR International Iceberg Database, to derive average iceberg dissolution rates. Fracture into two parts is the dominant dissolution process for tabular icebergs, with an average half-life of 30 days for icebergs <4 km length and 60 days for larger icebergs. Complete shatter producing many icebergs <1 km length is rare. A side attrition rate of 0.23 m d −1 combined with drift speed of 6 km d −1 , or any proportional change in both numbers fits the observed changes in iceberg distribution. The largest injection into the Southern Ocean of fresh water and any iceberg-transported material takes place in a ~2.3 × 10⁶ km 2 zone extending east-northeast from the Antarctic Peninsula to the Greenwich meridian. The iceberg contribution to salinities and temperatures, with maximum contribution north of the Weddell Sea, differs in some regions, from those indicated by tracking large icebergs.
format Article in Journal/Newspaper
author Orheim, Olav
Giles, A. Barry
Jacka, T. H. (Jo)
Moholdt, Geir
spellingShingle Orheim, Olav
Giles, A. Barry
Jacka, T. H. (Jo)
Moholdt, Geir
Quantifying dissolution rates of Antarctic icebergs in open water
author_facet Orheim, Olav
Giles, A. Barry
Jacka, T. H. (Jo)
Moholdt, Geir
author_sort Orheim, Olav
title Quantifying dissolution rates of Antarctic icebergs in open water
title_short Quantifying dissolution rates of Antarctic icebergs in open water
title_full Quantifying dissolution rates of Antarctic icebergs in open water
title_fullStr Quantifying dissolution rates of Antarctic icebergs in open water
title_full_unstemmed Quantifying dissolution rates of Antarctic icebergs in open water
title_sort quantifying dissolution rates of antarctic icebergs in open water
publisher Cambridge University Press (CUP)
publishDate 2023
url http://dx.doi.org/10.1017/aog.2023.26
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0260305523000265
geographic Antarctic
Antarctic Peninsula
Greenwich
Southern Ocean
The Antarctic
Weddell
Weddell Sea
geographic_facet Antarctic
Antarctic Peninsula
Greenwich
Southern Ocean
The Antarctic
Weddell
Weddell Sea
genre Annals of Glaciology
Antarc*
Antarctic
Antarctic Peninsula
Iceberg*
South Atlantic Ocean
Southern Ocean
Weddell Sea
genre_facet Annals of Glaciology
Antarc*
Antarctic
Antarctic Peninsula
Iceberg*
South Atlantic Ocean
Southern Ocean
Weddell Sea
op_source Annals of Glaciology
page 1-11
ISSN 0260-3055 1727-5644
op_rights http://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.1017/aog.2023.26
container_title Annals of Glaciology
container_start_page 1
op_container_end_page 11
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