| タイトル | Jovian meterology: Large-scale moist convection without a lower boundary |
| 本文（外部サイト） | http://hdl.handle.net/2060/19760009916 |
| 著者（英） | Gierasch, P. J. |
| 著者所属（英） | Cornell Univ. |
| 発行日 | 1975-11-01 |
| 言語 | eng |
| 内容記述 | It is proposed that Jupiter's cloud bands represent large scale convection whose character is determined by the phase change of water at a level where the temperature is about 275K. It is argued that there are three important layers in the atmosphere: a tropopause layer where emission to space occurs; an intermediate layer between the tropopause and the water cloud base; and the deep layer below the water cloud. All arguments are only semi-quantitative. It is pointed out that these ingredients are essential to Jovian meteorology. |
| NASA分類 | LUNAR AND PLANETARY EXPLORATION |
| レポートNO | 76N17004
NASA-CR-146353
CRSR-616 |
| 権利 | No Copyright |
| URI | https://repository.exst.jaxa.jp/dspace/handle/a-is/187223 |
