The temperature structure of the winter atmosphere at South Pole
[1] Fe/Rayleigh lidar measurements and balloon observa-tions made recently at the geographic South Pole are used to characterize the monthly mean winter temperature profiles from the surface to about 110 km. The measured temperatures during mid-winter in both the stratopause and mesopause regions ar...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.501.2112 2023-05-15T18:21:53+02:00 The temperature structure of the winter atmosphere at South Pole Weilin Pan Chester S. Gardner Raymond G. Roble The Pennsylvania State University CiteSeerX Archives 2002 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.501.2112 http://conrad.csl.uiuc.edu/Research/SouthPole/Pan_GRL2002.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.501.2112 http://conrad.csl.uiuc.edu/Research/SouthPole/Pan_GRL2002.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://conrad.csl.uiuc.edu/Research/SouthPole/Pan_GRL2002.pdf 0315 0325 text 2002 ftciteseerx 2016-01-08T09:08:27Z [1] Fe/Rayleigh lidar measurements and balloon observa-tions made recently at the geographic South Pole are used to characterize the monthly mean winter temperature profiles from the surface to about 110 km. The measured temperatures during mid-winter in both the stratopause and mesopause regions are 20–30 K colder than current model predictions. These differences are caused by weaker than expected compressional heating associated with subsidence over the polar cap. The measured mesopause temperature responds much more rapidly to changes in sunlight than model predictions, which suggests that IR heating by CO2 absorption may also be important to the thermal balance in the mesopause region. INDEX TERMS: 3334 Meteorology Text South pole Unknown South Pole |
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ftciteseerx |
language |
English |
topic |
0315 0325 |
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0315 0325 Weilin Pan Chester S. Gardner Raymond G. Roble The temperature structure of the winter atmosphere at South Pole |
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0315 0325 |
description |
[1] Fe/Rayleigh lidar measurements and balloon observa-tions made recently at the geographic South Pole are used to characterize the monthly mean winter temperature profiles from the surface to about 110 km. The measured temperatures during mid-winter in both the stratopause and mesopause regions are 20–30 K colder than current model predictions. These differences are caused by weaker than expected compressional heating associated with subsidence over the polar cap. The measured mesopause temperature responds much more rapidly to changes in sunlight than model predictions, which suggests that IR heating by CO2 absorption may also be important to the thermal balance in the mesopause region. INDEX TERMS: 3334 Meteorology |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Weilin Pan Chester S. Gardner Raymond G. Roble |
author_facet |
Weilin Pan Chester S. Gardner Raymond G. Roble |
author_sort |
Weilin Pan |
title |
The temperature structure of the winter atmosphere at South Pole |
title_short |
The temperature structure of the winter atmosphere at South Pole |
title_full |
The temperature structure of the winter atmosphere at South Pole |
title_fullStr |
The temperature structure of the winter atmosphere at South Pole |
title_full_unstemmed |
The temperature structure of the winter atmosphere at South Pole |
title_sort |
temperature structure of the winter atmosphere at south pole |
publishDate |
2002 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.501.2112 http://conrad.csl.uiuc.edu/Research/SouthPole/Pan_GRL2002.pdf |
geographic |
South Pole |
geographic_facet |
South Pole |
genre |
South pole |
genre_facet |
South pole |
op_source |
http://conrad.csl.uiuc.edu/Research/SouthPole/Pan_GRL2002.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.501.2112 http://conrad.csl.uiuc.edu/Research/SouthPole/Pan_GRL2002.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766201208861622272 |