| THE ROLE PLAYED BY THE STRATOSPHERE IN GREENHOUSE EFFECT |
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| 作者姓名： | Guo Caili Li Weiliang Liu Yu |
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| 作者单位： | Chinese Academy of Meteorological Sciences Beijing 100081，Chinese Academy of Meteorological Sciences Beijing 100081，Chinese Academy of Meteorological Sciences Beijing 100081 |
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| 摘 要： | Two one-dimensional radiative-convective models with the same scheme and the different ranges that one is fromsurface to stratopause and the other is from surface to tropopause,have been developed to study the role played by thestratosphere in greenhouse effect.It is shown that the addition of stratospheric response may lead to an increase of 7—50percent in radiative forcing at the tropopause,and an increase of 20—60 percent in surface temperature when the con-centration of the same gas in the two models increases at the same time;and when the same change in radiative forcing atthe tropopause due to the same agent in the two models occurs,the addition of stratospheric response may lead to an in-crease of 5—20 percent in surface temperature;and allowing for the stratospheric adjustment means that the tempera-ture responses to the same flux change due to different causes are in far disagreement.
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| 收稿时间： | 1991/8/12 0:00:00 |
| 修稿时间： | 1992/6/13 0:00:00 |
THE ROLE PLAYED BY THE STRATOSPHERE IN GREENHOUSE EFFECT |
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| Guo Caili,Li Weiliang,Liu Yu.THE ROLE PLAYED BY THE STRATOSPHERE IN GREENHOUSE EFFECT[J].Acta Meteorologica Sinica,1993,7(1):50-60. |
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| Authors: | Guo Caili Li Weiliang and Liu Yu |
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| Institution: | Guo Caili Li Weiliang Liu Yu Chinese Academy of Meteorological Sciences,Beijing 100081 |
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| Abstract: | Two one-dimensional radiative-convective models with the same scheme and the different ranges that one is from surface to stratopause and the other is from surface to tropopause,have been developed to study the role played by the stratosphere in greenhouse effect.It is shown that the addition of stratospheric response may lead to an increase of 7-50 percent in radiative forcing at the tropopause,and an increase of 20-60 percent in surface temperature when the concentration of the same gas in the two models increases at the same time;and when the same change in radiative forcing at the tropopause due to the same agent in the two models occurs,the addition of stratospheric response may lead to an increase of 5-20 percent in surface temperature;and allowing for the stratospheric adjustment means that the temperature responses to the same flux change due to different causes are in far disagreement. |
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| Keywords: | greenhouse effect stratosphere 1-D radiative-convective model temperature response |
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