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DEVELOPMENT OF MIDDLE ATMOSPHERE GENERAL CIRCULATION MODEL INCLUDING RADIATION PROCESSES

DEVELOPMENT OF MIDDLE ATMOSPHERE GENERAL CIRCULATION MODEL INCLUDING RADIATION PROCESSES
包括辐射过程的中层大气环流模型的开发
批准号:
05452079
负责人:
NIYAHARA Saburo
金额:
$3.84万
依托单位:
依托单位国家:
日本
项目类别:
Grant-in-Aid for General Scientific Research (B)
财政年份:
1993
资助国家:
日本
项目状态:
已结题
起止时间:
1993 至 1995

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中文摘要
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英文摘要
A radiation scheme developed at Center for Climate System and a rediation scheme developed by Fomichev were incorporated in a middle atmosphere general circulation model at Kyushu University.The former scheme is able to treat the short wave and long wave radiations. Some test runs have been done using a tropospheric-lower stratospheric general circulation model, and it has been confirmed that the GCM can simulate a realistic circulation and temperature distribution.Fomichev's scheme is a long wave radiation scheme treating the LTE and non-LTE radiation in the middle atmosphere. In this project, we have introduced this scheme to treat the long wave radiation in the middle atmosphere and lower thermosphere. The results show that zonal wind around the mesopause becomes strong by introducing the realistic radiation process. This means that we need stronger E-P flux divergence (convergence) to close the zonal wind around the mesopause.An ozone chemical transport process was incorporated to the middle atmosphere GCM,and three dimensional ozone simulation has been conducted to investigate ozone variation in the middle atmosphere and resulting general circulation change. By making an artificial ozone hole in the Antarctic region, variations of temperature distribution and general circulation had been investigated. It is found that temperature decreases around the ozone hole, and it increases above the ozone reduction height. This result is consistent with observations. The temperature change is induced by the changes of the polar night jet, planetary wave activity, and the residual circulation induced by the ozone reduction.
期刊论文(18)
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会议论文
S.Miyahara and J.Forbes: "Interactions between diurnal tides and gravity waves in the lower thermosphere" Jour.Atmos.Terr.Phys.56. 1365-1373 (1994)
S.Miyahara 和 J.Forbes:“低热层中日潮汐与重力波之间的相互作用”Jour.Atmos.Terr.Phys.56。
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通讯作者:
S.Miyahara et al.: "Dynamical coupling between the lower and upper atmosphere by tides and gravity waves" Jour.Atmos.Terr.Phys.55. 1039-1053 (1993)
S.Miyahara 等人:“潮汐和重力波导致下层和上层大气之间的动态耦合”Jour.Atmos.Terr.Phys.55。
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S.Miyahara and J.Forbes: "Interactions between diurnal tides and gravity waves in the lower thermosphere" Jour.Atmos.Terr.Phys.(in press). (1994)
S.Miyahara 和 J.Forbes:“低热层中日潮汐与重力波之间的相互作用”Jour.Atmos.Terr.Phys.(正在印刷中)。
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E.M.P.EKANAYAKE: "Background Wind Effect on Propagation of Nonmigrating Diurnal Tides in the Middle Atmosphere" Jour.Atmos.Terr.Phys.(in press).
E.M.P.EKANAYAKE:“背景风对中层大气中非迁移昼潮传播的影响”Jour.Atmos.Terr.Phys.(正在出版)。
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