RADIATIVELY DETERMINED TEMPERATURE IN THE MIDDLE ATMOSPHERE IN THE POLAR REGION
Radiatively determined temperature, i. e., time-marched temperature under the absence of dynamical warming, in the middle atmosphere is investigated for various conditions. The model used in this study extends from the surface to the middle mesosphere at about 70km. First, the temperature change dur...
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ftnipr:oai:nipr.repo.nii.ac.jp:00003656 2023-07-02T03:33:34+02:00 RADIATIVELY DETERMINED TEMPERATURE IN THE MIDDLE ATMOSPHERE IN THE POLAR REGION シバタ キヨタカ Kiyotaka SHIBATA 1991-05 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3656 http://id.nii.ac.jp/1291/00003656/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3656&item_no=1&attribute_id=18&file_no=1 en eng ABSTRACT Meteorological Research Institute National Institute of Polar Research https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3656 http://id.nii.ac.jp/1291/00003656/ AA10756213 Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology, 4, 122-123(1991-05) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3656&item_no=1&attribute_id=18&file_no=1 Departmental Bulletin Paper P(論文) 1991 ftnipr 2023-06-10T19:38:20Z Radiatively determined temperature, i. e., time-marched temperature under the absence of dynamical warming, in the middle atmosphere is investigated for various conditions. The model used in this study extends from the surface to the middle mesosphere at about 70km. First, the temperature change during the polar night is studied. For a clear atmosphere, the surface temperature of which is calculated from the radiation heat budget, temperature decreases uniformly with respect to height except for the first 20 days. The decrease rate becomes very small as temperature becomes low, and hence even the lowest temperature at the surface cannot reach 100K for the polar night. When the surface temperature is prescribed to have the climatological value, the temperature in the stratosphere and mesosphere decreases in a similar way. However, there appears a relatively high temperature region from about 150mb to 30mb. This is because CO_2 and O_3 absorb longwave radiation from the warm surface. Second, the temperature change is studied after the sun reappears. It is found that according to the intensity of warming, the stratosphere can be separated into 3 regions : upper (P<10mb), middle (10mb<P<100mb), lower (100mb<P). The temperature in the upper and middle stratosphere is restored to the climatological value in a rather short time, 1 to 2 months. On the other hand, the temperature in the lower stratosphere rises far more slowly and remains much lower than the climatological value. This suggests that the dynamical warming plays a crucial role in the lower stratosphere. Report Polar meteorology and glaciology polar night Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology National Institute of Polar Research Repository, Japan |
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Open Polar |
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National Institute of Polar Research Repository, Japan |
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ftnipr |
language |
English |
description |
Radiatively determined temperature, i. e., time-marched temperature under the absence of dynamical warming, in the middle atmosphere is investigated for various conditions. The model used in this study extends from the surface to the middle mesosphere at about 70km. First, the temperature change during the polar night is studied. For a clear atmosphere, the surface temperature of which is calculated from the radiation heat budget, temperature decreases uniformly with respect to height except for the first 20 days. The decrease rate becomes very small as temperature becomes low, and hence even the lowest temperature at the surface cannot reach 100K for the polar night. When the surface temperature is prescribed to have the climatological value, the temperature in the stratosphere and mesosphere decreases in a similar way. However, there appears a relatively high temperature region from about 150mb to 30mb. This is because CO_2 and O_3 absorb longwave radiation from the warm surface. Second, the temperature change is studied after the sun reappears. It is found that according to the intensity of warming, the stratosphere can be separated into 3 regions : upper (P<10mb), middle (10mb<P<100mb), lower (100mb<P). The temperature in the upper and middle stratosphere is restored to the climatological value in a rather short time, 1 to 2 months. On the other hand, the temperature in the lower stratosphere rises far more slowly and remains much lower than the climatological value. This suggests that the dynamical warming plays a crucial role in the lower stratosphere. |
format |
Report |
author |
シバタ キヨタカ Kiyotaka SHIBATA |
spellingShingle |
シバタ キヨタカ Kiyotaka SHIBATA RADIATIVELY DETERMINED TEMPERATURE IN THE MIDDLE ATMOSPHERE IN THE POLAR REGION |
author_facet |
シバタ キヨタカ Kiyotaka SHIBATA |
author_sort |
シバタ キヨタカ |
title |
RADIATIVELY DETERMINED TEMPERATURE IN THE MIDDLE ATMOSPHERE IN THE POLAR REGION |
title_short |
RADIATIVELY DETERMINED TEMPERATURE IN THE MIDDLE ATMOSPHERE IN THE POLAR REGION |
title_full |
RADIATIVELY DETERMINED TEMPERATURE IN THE MIDDLE ATMOSPHERE IN THE POLAR REGION |
title_fullStr |
RADIATIVELY DETERMINED TEMPERATURE IN THE MIDDLE ATMOSPHERE IN THE POLAR REGION |
title_full_unstemmed |
RADIATIVELY DETERMINED TEMPERATURE IN THE MIDDLE ATMOSPHERE IN THE POLAR REGION |
title_sort |
radiatively determined temperature in the middle atmosphere in the polar region |
publisher |
ABSTRACT |
publishDate |
1991 |
url |
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3656 http://id.nii.ac.jp/1291/00003656/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3656&item_no=1&attribute_id=18&file_no=1 |
genre |
Polar meteorology and glaciology polar night Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology |
genre_facet |
Polar meteorology and glaciology polar night Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology |
op_relation |
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3656 http://id.nii.ac.jp/1291/00003656/ AA10756213 Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology, 4, 122-123(1991-05) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3656&item_no=1&attribute_id=18&file_no=1 |
_version_ |
1770273561652494336 |