Distinct modes of internal variability in the Global Meridional Overturning Circulation associated with the Southern Hemisphere westerly winds
The internal variability of the global meridional overturning circulation (GMOC) in long-term integration of the Earth system model COSMOS is examined in this study. Two distinct modes of the GMOC, which are closely linked to the Southern Hemisphere westerly winds (SWW) anomalies, are found on multi...
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2012
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ftawi:oai:epic.awi.de:26034 2024-09-15T18:37:05+00:00 Distinct modes of internal variability in the Global Meridional Overturning Circulation associated with the Southern Hemisphere westerly winds Wei, Wei Lohmann, Gerrit Dima, Mihai 2012 https://epic.awi.de/id/eprint/26034/ https://doi.org/10.1175/JPO-D-11-038.1 https://hdl.handle.net/10013/epic.39278 unknown AMER METEOROLOGICAL SOC Wei, W. , Lohmann, G. orcid:0000-0003-2089-733X and Dima, M. (2012) Distinct modes of internal variability in the Global Meridional Overturning Circulation associated with the Southern Hemisphere westerly winds , Journal of Physical Oceanography, (42), pp. 785-801 . doi:10.1175/JPO-D-11-038.1 <https://doi.org/10.1175/JPO-D-11-038.1> , hdl:10013/epic.39278 EPIC3Journal of Physical Oceanography, AMER METEOROLOGICAL SOC, (42), pp. 785-801, ISSN: 0022-3670 Article isiRev 2012 ftawi https://doi.org/10.1175/JPO-D-11-038.1 2024-06-24T04:03:41Z The internal variability of the global meridional overturning circulation (GMOC) in long-term integration of the Earth system model COSMOS is examined in this study. Two distinct modes of the GMOC, which are closely linked to the Southern Hemisphere westerly winds (SWW) anomalies, are found on multidecadal and centennial time scales. The dominant mode is characterized by Southern Ocean dynamics: strengthening and poleward shift of the SWW associated with a positive phase of the Southern Annualar mode yield Ekman-induced northward mass transport, including a zonally asymmetric response in the Southern Ocean sea surface temperature, and a cooling in the tropical Pacific Ocean due to large-scale upwelling. The second mode projects mainly onto the Atlantic meridional overturning circulation (AMOC). It is driven by a combination of SWW variation and buoyancy forcing. Based on the relationship between the two modes together with the wind perturbation experiments, we emphasize that the full AMOC response to the SWW change takes several centuries in our model. The sea surface temperature in Northern Hemisphere high latitudes is significantly affected in this mode, showing a large-scale warming. Our results from a mid-Holocene experiment imply that both modes are independent from the climate background conditions in the Holocene. Finally, we argue that the natural modes of GMOC are important to understand trends in ocean circulation, with consequences for heat and carbon budgets for past, present and future climate. Article in Journal/Newspaper Southern Ocean Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) Journal of Physical Oceanography 42 5 785 801 |
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Open Polar |
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Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
op_collection_id |
ftawi |
language |
unknown |
description |
The internal variability of the global meridional overturning circulation (GMOC) in long-term integration of the Earth system model COSMOS is examined in this study. Two distinct modes of the GMOC, which are closely linked to the Southern Hemisphere westerly winds (SWW) anomalies, are found on multidecadal and centennial time scales. The dominant mode is characterized by Southern Ocean dynamics: strengthening and poleward shift of the SWW associated with a positive phase of the Southern Annualar mode yield Ekman-induced northward mass transport, including a zonally asymmetric response in the Southern Ocean sea surface temperature, and a cooling in the tropical Pacific Ocean due to large-scale upwelling. The second mode projects mainly onto the Atlantic meridional overturning circulation (AMOC). It is driven by a combination of SWW variation and buoyancy forcing. Based on the relationship between the two modes together with the wind perturbation experiments, we emphasize that the full AMOC response to the SWW change takes several centuries in our model. The sea surface temperature in Northern Hemisphere high latitudes is significantly affected in this mode, showing a large-scale warming. Our results from a mid-Holocene experiment imply that both modes are independent from the climate background conditions in the Holocene. Finally, we argue that the natural modes of GMOC are important to understand trends in ocean circulation, with consequences for heat and carbon budgets for past, present and future climate. |
format |
Article in Journal/Newspaper |
author |
Wei, Wei Lohmann, Gerrit Dima, Mihai |
spellingShingle |
Wei, Wei Lohmann, Gerrit Dima, Mihai Distinct modes of internal variability in the Global Meridional Overturning Circulation associated with the Southern Hemisphere westerly winds |
author_facet |
Wei, Wei Lohmann, Gerrit Dima, Mihai |
author_sort |
Wei, Wei |
title |
Distinct modes of internal variability in the Global Meridional Overturning Circulation associated with the Southern Hemisphere westerly winds |
title_short |
Distinct modes of internal variability in the Global Meridional Overturning Circulation associated with the Southern Hemisphere westerly winds |
title_full |
Distinct modes of internal variability in the Global Meridional Overturning Circulation associated with the Southern Hemisphere westerly winds |
title_fullStr |
Distinct modes of internal variability in the Global Meridional Overturning Circulation associated with the Southern Hemisphere westerly winds |
title_full_unstemmed |
Distinct modes of internal variability in the Global Meridional Overturning Circulation associated with the Southern Hemisphere westerly winds |
title_sort |
distinct modes of internal variability in the global meridional overturning circulation associated with the southern hemisphere westerly winds |
publisher |
AMER METEOROLOGICAL SOC |
publishDate |
2012 |
url |
https://epic.awi.de/id/eprint/26034/ https://doi.org/10.1175/JPO-D-11-038.1 https://hdl.handle.net/10013/epic.39278 |
genre |
Southern Ocean |
genre_facet |
Southern Ocean |
op_source |
EPIC3Journal of Physical Oceanography, AMER METEOROLOGICAL SOC, (42), pp. 785-801, ISSN: 0022-3670 |
op_relation |
Wei, W. , Lohmann, G. orcid:0000-0003-2089-733X and Dima, M. (2012) Distinct modes of internal variability in the Global Meridional Overturning Circulation associated with the Southern Hemisphere westerly winds , Journal of Physical Oceanography, (42), pp. 785-801 . doi:10.1175/JPO-D-11-038.1 <https://doi.org/10.1175/JPO-D-11-038.1> , hdl:10013/epic.39278 |
op_doi |
https://doi.org/10.1175/JPO-D-11-038.1 |
container_title |
Journal of Physical Oceanography |
container_volume |
42 |
container_issue |
5 |
container_start_page |
785 |
op_container_end_page |
801 |
_version_ |
1810481422136246272 |