The storm tracks and the energy cycle of the Southern Hemisphere: sensitivity to sea-ice boundary conditions

The effect of sea-ice on various aspects of the Southern Hemisphere (SH) extratropical climate is examined. Two simulations using the LMD GCM are performed: a control run with the observed sea-ice distribution and an anomaly run in which all SH sea-ice is replaced by open ocean. When sea-ice is remo...

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Published in:Annales Geophysicae
Main Authors: Menéndez, C. G., Serafini, V., Treut, H.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.1007/s00585-999-1478-2
https://angeo.copernicus.org/articles/17/1478/1999/
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spelling ftcopernicus:oai:publications.copernicus.org:angeo34505 2023-05-15T13:36:36+02:00 The storm tracks and the energy cycle of the Southern Hemisphere: sensitivity to sea-ice boundary conditions Menéndez, C. G. Serafini, V. Treut, H. 2018-09-27 application/pdf https://doi.org/10.1007/s00585-999-1478-2 https://angeo.copernicus.org/articles/17/1478/1999/ eng eng doi:10.1007/s00585-999-1478-2 https://angeo.copernicus.org/articles/17/1478/1999/ eISSN: 1432-0576 Text 2018 ftcopernicus https://doi.org/10.1007/s00585-999-1478-2 2020-07-20T16:28:00Z The effect of sea-ice on various aspects of the Southern Hemisphere (SH) extratropical climate is examined. Two simulations using the LMD GCM are performed: a control run with the observed sea-ice distribution and an anomaly run in which all SH sea-ice is replaced by open ocean. When sea-ice is removed, the mean sea level pressure displays anomalies predominantly negatives near the Antarctic coast. In general, the meridional temperature gradient is reduced over most of the Southern Ocean, the polar jet is weaker and the sea level pressure rises equatorward of the control ice edge. The high frequency filtered standard deviation of both the sea level pressure and the 300-hPa geopotential height decreases over the southern Pacific and southwestern Atlantic oceans, especially to the north of the ice edge (as prescribed in the control). In contrast, over the Indian Ocean the perturbed simulation exhibits less variability equatorward of about 50°S and increased variability to the south. The zonal averages of the zonal and eddy potential and kinetic energies were evaluated. The effect of removing sea-ice is to diminish the available potential energy of the mean zonal flow, the available potential energy of the perturbations, the kinetic energy of the growing disturbances and the kinetic energy of the mean zonal flow over most of the Southern Ocean. The zonally averaged intensity of the subpolar trough and the rate of the baroclinic energy conversions are also weaker. Key words. Air-sea interactions · Meteorology and atmospheric dynamics (climatology; ocean · atmosphere interactions) Text Antarc* Antarctic Sea ice Southern Ocean Copernicus Publications: E-Journals Antarctic Indian Pacific Southern Ocean The Antarctic Annales Geophysicae 17 11 1478 1492
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description The effect of sea-ice on various aspects of the Southern Hemisphere (SH) extratropical climate is examined. Two simulations using the LMD GCM are performed: a control run with the observed sea-ice distribution and an anomaly run in which all SH sea-ice is replaced by open ocean. When sea-ice is removed, the mean sea level pressure displays anomalies predominantly negatives near the Antarctic coast. In general, the meridional temperature gradient is reduced over most of the Southern Ocean, the polar jet is weaker and the sea level pressure rises equatorward of the control ice edge. The high frequency filtered standard deviation of both the sea level pressure and the 300-hPa geopotential height decreases over the southern Pacific and southwestern Atlantic oceans, especially to the north of the ice edge (as prescribed in the control). In contrast, over the Indian Ocean the perturbed simulation exhibits less variability equatorward of about 50°S and increased variability to the south. The zonal averages of the zonal and eddy potential and kinetic energies were evaluated. The effect of removing sea-ice is to diminish the available potential energy of the mean zonal flow, the available potential energy of the perturbations, the kinetic energy of the growing disturbances and the kinetic energy of the mean zonal flow over most of the Southern Ocean. The zonally averaged intensity of the subpolar trough and the rate of the baroclinic energy conversions are also weaker. Key words. Air-sea interactions · Meteorology and atmospheric dynamics (climatology; ocean · atmosphere interactions)
format Text
author Menéndez, C. G.
Serafini, V.
Treut, H.
spellingShingle Menéndez, C. G.
Serafini, V.
Treut, H.
The storm tracks and the energy cycle of the Southern Hemisphere: sensitivity to sea-ice boundary conditions
author_facet Menéndez, C. G.
Serafini, V.
Treut, H.
author_sort Menéndez, C. G.
title The storm tracks and the energy cycle of the Southern Hemisphere: sensitivity to sea-ice boundary conditions
title_short The storm tracks and the energy cycle of the Southern Hemisphere: sensitivity to sea-ice boundary conditions
title_full The storm tracks and the energy cycle of the Southern Hemisphere: sensitivity to sea-ice boundary conditions
title_fullStr The storm tracks and the energy cycle of the Southern Hemisphere: sensitivity to sea-ice boundary conditions
title_full_unstemmed The storm tracks and the energy cycle of the Southern Hemisphere: sensitivity to sea-ice boundary conditions
title_sort storm tracks and the energy cycle of the southern hemisphere: sensitivity to sea-ice boundary conditions
publishDate 2018
url https://doi.org/10.1007/s00585-999-1478-2
https://angeo.copernicus.org/articles/17/1478/1999/
geographic Antarctic
Indian
Pacific
Southern Ocean
The Antarctic
geographic_facet Antarctic
Indian
Pacific
Southern Ocean
The Antarctic
genre Antarc*
Antarctic
Sea ice
Southern Ocean
genre_facet Antarc*
Antarctic
Sea ice
Southern Ocean
op_source eISSN: 1432-0576
op_relation doi:10.1007/s00585-999-1478-2
https://angeo.copernicus.org/articles/17/1478/1999/
op_doi https://doi.org/10.1007/s00585-999-1478-2
container_title Annales Geophysicae
container_volume 17
container_issue 11
container_start_page 1478
op_container_end_page 1492
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