The Southern Ocean: A ventilation contributor with multiple sources

The importance of deep and bottom water formed in the Southern Ocean to the ventilation of theworld ocean abyss has been accepted by the oceanographic community. Uncertainties, however,exist about rate and exact location of dense water mass sinking around Antarctica. Based on watermass analysis, the...

Full description

Bibliographic Details
Main Authors: Hellmer, Hartmut, Beckmann, A.
Format: Article in Journal/Newspaper
Language:unknown
Published: 2001
Subjects:
Online Access:https://epic.awi.de/id/eprint/3512/
https://epic.awi.de/id/eprint/3512/1/Hel8888a.pdf
https://hdl.handle.net/10013/epic.14095
https://hdl.handle.net/10013/epic.14095.d001
id ftawi:oai:epic.awi.de:3512
record_format openpolar
spelling ftawi:oai:epic.awi.de:3512 2024-09-15T17:47:07+00:00 The Southern Ocean: A ventilation contributor with multiple sources Hellmer, Hartmut Beckmann, A. 2001 application/pdf https://epic.awi.de/id/eprint/3512/ https://epic.awi.de/id/eprint/3512/1/Hel8888a.pdf https://hdl.handle.net/10013/epic.14095 https://hdl.handle.net/10013/epic.14095.d001 unknown https://epic.awi.de/id/eprint/3512/1/Hel8888a.pdf https://hdl.handle.net/10013/epic.14095.d001 Hellmer, H. orcid:0000-0002-9357-9853 and Beckmann, A. (2001) The Southern Ocean: A ventilation contributor with multiple sources , Geophysical Research Letters, 28 (15), pp. 2927-2930 . hdl:10013/epic.14095 EPIC3Geophysical Research Letters, 28(15), pp. 2927-2930, ISSN: 0094-8276 Article isiRev 2001 ftawi 2024-06-24T03:54:11Z The importance of deep and bottom water formed in the Southern Ocean to the ventilation of theworld ocean abyss has been accepted by the oceanographic community. Uncertainties, however,exist about rate and exact location of dense water mass sinking around Antarctica. Based on watermass analysis, the Weddell Sea in the Atlantic sector has long been identified as being the majorsource for bottom water. The contribution of the Ross Sea in the western Pacific sector, althoughwith similar if not more favorable ingredients for dense bottom water formation, seemed to be minor.Observations and recent tracer analysis indicate that the Indian-Pacific sector might host sourceswhich together can compete with their Atlantic counterpart. Our numerical model results support asplitting of the Atlantic and Indian-Pacific contributions into roughly equal parts but for bottomwaters of different density. The observationally derived formation rate for dense Antarctic BottomWater on the order of 10 Sv (1 Sv = 10^6 m^3/s) is confirmed but doubles if the lighter componentof the Indian-Pacific sector is included. This places southern and northern hemisphere sources asequal contributors to the ventilation of the world ocean. Article in Journal/Newspaper Antarc* Antarctic Antarctica Ross Sea Southern Ocean Weddell Sea Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center)
institution Open Polar
collection Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center)
op_collection_id ftawi
language unknown
description The importance of deep and bottom water formed in the Southern Ocean to the ventilation of theworld ocean abyss has been accepted by the oceanographic community. Uncertainties, however,exist about rate and exact location of dense water mass sinking around Antarctica. Based on watermass analysis, the Weddell Sea in the Atlantic sector has long been identified as being the majorsource for bottom water. The contribution of the Ross Sea in the western Pacific sector, althoughwith similar if not more favorable ingredients for dense bottom water formation, seemed to be minor.Observations and recent tracer analysis indicate that the Indian-Pacific sector might host sourceswhich together can compete with their Atlantic counterpart. Our numerical model results support asplitting of the Atlantic and Indian-Pacific contributions into roughly equal parts but for bottomwaters of different density. The observationally derived formation rate for dense Antarctic BottomWater on the order of 10 Sv (1 Sv = 10^6 m^3/s) is confirmed but doubles if the lighter componentof the Indian-Pacific sector is included. This places southern and northern hemisphere sources asequal contributors to the ventilation of the world ocean.
format Article in Journal/Newspaper
author Hellmer, Hartmut
Beckmann, A.
spellingShingle Hellmer, Hartmut
Beckmann, A.
The Southern Ocean: A ventilation contributor with multiple sources
author_facet Hellmer, Hartmut
Beckmann, A.
author_sort Hellmer, Hartmut
title The Southern Ocean: A ventilation contributor with multiple sources
title_short The Southern Ocean: A ventilation contributor with multiple sources
title_full The Southern Ocean: A ventilation contributor with multiple sources
title_fullStr The Southern Ocean: A ventilation contributor with multiple sources
title_full_unstemmed The Southern Ocean: A ventilation contributor with multiple sources
title_sort southern ocean: a ventilation contributor with multiple sources
publishDate 2001
url https://epic.awi.de/id/eprint/3512/
https://epic.awi.de/id/eprint/3512/1/Hel8888a.pdf
https://hdl.handle.net/10013/epic.14095
https://hdl.handle.net/10013/epic.14095.d001
genre Antarc*
Antarctic
Antarctica
Ross Sea
Southern Ocean
Weddell Sea
genre_facet Antarc*
Antarctic
Antarctica
Ross Sea
Southern Ocean
Weddell Sea
op_source EPIC3Geophysical Research Letters, 28(15), pp. 2927-2930, ISSN: 0094-8276
op_relation https://epic.awi.de/id/eprint/3512/1/Hel8888a.pdf
https://hdl.handle.net/10013/epic.14095.d001
Hellmer, H. orcid:0000-0002-9357-9853 and Beckmann, A. (2001) The Southern Ocean: A ventilation contributor with multiple sources , Geophysical Research Letters, 28 (15), pp. 2927-2930 . hdl:10013/epic.14095
_version_ 1810495764612251648