| タイトル | 21 Layer troposphere-stratosphere climate model |
| 本文（外部サイト） | http://hdl.handle.net/2060/19850013561 |
| 著者（英） | Russell, G.; Suozzo, R.; Rind, D.; Lacis, A.; Hansen, J. |
| 著者所属（英） | NASA Goddard Space Flight Center |
| 発行日 | 1984-12-01 |
| 言語 | eng |
| 内容記述 | The global climate model is extended through the stratosphere by increasing the vertical resolution and raising the rigid model top to the 0.01 mb (75 km) level. The inclusion of a realistic stratosphere is necessary for the investigation of the climate effects of stratospheric perturbations, such as changes of ozone, aerosols or solar ultraviolet irradiance, as well as for studying the effect on the stratosphere of tropospheric climate changes. The observed temperature and wind patterns throughout the troposphere and stratosphere are simulated. In addition to the excess planetary wave amplitude in the upper stratosphere, other model deficiences include the Northern Hemisphere lower stratospheric temperatures being 5 to 10 C too cold in winter at high latitudes and the temperature at 50 to 60 km altitude near the equator are too cold. Methods of correcting these deficiencies are discussed. |
| NASA分類 | METEOROLOGY AND CLIMATOLOGY |
| レポートNO | 85N21871
NAS 1.15:86183
GNC84-027
NASA-TM-86183 |
| 権利 | No Copyright |
| URI | https://repository.exst.jaxa.jp/dspace/handle/a-is/156881 |
