The northern hemisphere tropospheric response to changes in the gravity‐wave drag scheme in a perpetual January GCM
Abstract The sensitivity of a general‐circulation‐model climatology to changes in the gravity‐wave drag scheme is investigated with particular emphasis being placed upon the northern hemisphere wintertime tropospheric circulation. It is found that by weakening the upper‐level drag, the Ferrel‐cell c...
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crwiley:10.1002/qj.49712051709 2024-06-02T08:02:14+00:00 The northern hemisphere tropospheric response to changes in the gravity‐wave drag scheme in a perpetual January GCM Stephenson, David B. 1994 http://dx.doi.org/10.1002/qj.49712051709 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fqj.49712051709 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/qj.49712051709 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Quarterly Journal of the Royal Meteorological Society volume 120, issue 517, page 699-712 ISSN 0035-9009 1477-870X journal-article 1994 crwiley https://doi.org/10.1002/qj.49712051709 2024-05-03T11:38:26Z Abstract The sensitivity of a general‐circulation‐model climatology to changes in the gravity‐wave drag scheme is investigated with particular emphasis being placed upon the northern hemisphere wintertime tropospheric circulation. It is found that by weakening the upper‐level drag, the Ferrel‐cell circulation intensifies to the north, resulting in a greater than 10 K cooling in the region of the arctic tropopause. The poleward side of the northern hemisphere sub‐tropical jet intensifies in the region of 60–70°N, and a poleward shift is observed in the eddy meridional momentum flux. A large part of the response is zonally asymmetric, with the Aleutian and Icelandic lows becoming shallower with weakened upper‐level gravity‐wave drag. By comparing the results of a gravity‐wave drag scheme having a wave‐breaking vertical profile with those of a simple uniform drag‐profile scheme it appears that the tropospheric response to weakened upper‐level drag depends very little upon the choice of vertical drag profile in the troposphere. Article in Journal/Newspaper Arctic Wiley Online Library Arctic Quarterly Journal of the Royal Meteorological Society 120 517 699 712 |
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Wiley Online Library |
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crwiley |
language |
English |
description |
Abstract The sensitivity of a general‐circulation‐model climatology to changes in the gravity‐wave drag scheme is investigated with particular emphasis being placed upon the northern hemisphere wintertime tropospheric circulation. It is found that by weakening the upper‐level drag, the Ferrel‐cell circulation intensifies to the north, resulting in a greater than 10 K cooling in the region of the arctic tropopause. The poleward side of the northern hemisphere sub‐tropical jet intensifies in the region of 60–70°N, and a poleward shift is observed in the eddy meridional momentum flux. A large part of the response is zonally asymmetric, with the Aleutian and Icelandic lows becoming shallower with weakened upper‐level gravity‐wave drag. By comparing the results of a gravity‐wave drag scheme having a wave‐breaking vertical profile with those of a simple uniform drag‐profile scheme it appears that the tropospheric response to weakened upper‐level drag depends very little upon the choice of vertical drag profile in the troposphere. |
format |
Article in Journal/Newspaper |
author |
Stephenson, David B. |
spellingShingle |
Stephenson, David B. The northern hemisphere tropospheric response to changes in the gravity‐wave drag scheme in a perpetual January GCM |
author_facet |
Stephenson, David B. |
author_sort |
Stephenson, David B. |
title |
The northern hemisphere tropospheric response to changes in the gravity‐wave drag scheme in a perpetual January GCM |
title_short |
The northern hemisphere tropospheric response to changes in the gravity‐wave drag scheme in a perpetual January GCM |
title_full |
The northern hemisphere tropospheric response to changes in the gravity‐wave drag scheme in a perpetual January GCM |
title_fullStr |
The northern hemisphere tropospheric response to changes in the gravity‐wave drag scheme in a perpetual January GCM |
title_full_unstemmed |
The northern hemisphere tropospheric response to changes in the gravity‐wave drag scheme in a perpetual January GCM |
title_sort |
northern hemisphere tropospheric response to changes in the gravity‐wave drag scheme in a perpetual january gcm |
publisher |
Wiley |
publishDate |
1994 |
url |
http://dx.doi.org/10.1002/qj.49712051709 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fqj.49712051709 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/qj.49712051709 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic |
genre_facet |
Arctic |
op_source |
Quarterly Journal of the Royal Meteorological Society volume 120, issue 517, page 699-712 ISSN 0035-9009 1477-870X |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1002/qj.49712051709 |
container_title |
Quarterly Journal of the Royal Meteorological Society |
container_volume |
120 |
container_issue |
517 |
container_start_page |
699 |
op_container_end_page |
712 |
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1800746744827346944 |