このアイテムのアクセス数: 129
このアイテムのファイル:
| ファイル | 記述 | サイズ | フォーマット | |
|---|---|---|---|---|
| cgk01200_049.pdf | 659.85 kB | Adobe PDF | 見る/開く |
完全メタデータレコード
| DCフィールド | 値 | 言語 |
|---|---|---|
| dc.contributor.author | OHNISHI, Haruo | en |
| dc.contributor.author | ASAI, Tomio | en |
| dc.date.accessioned | 2013-09-02T04:36:28Z | - |
| dc.date.available | 2013-09-02T04:36:28Z | - |
| dc.date.issued | 1972-12 | - |
| dc.identifier.uri | http://hdl.handle.net/2433/178619 | - |
| dc.description.abstract | Among those which parameterize cumulus convection, the "penetrative moist convection (PMC) scheme" and the "convective adjustment (CA) scheme" are compared with each other by applying them to a simple numerical model. A main difference between them appears in the vertical distribution of warming. The warming in the PMC scheme has characteristics of penetrative convection, whereas that in the CA scheme hardly penetrate into a stable layer. Features found in precipitations and stabilities for perturbations of different wavelengths are discussed as well as for each of the schemes. Some variations of these two schemes are also examined. | en |
| dc.format.mimetype | application/pdf | - |
| dc.language.iso | eng | - |
| dc.publisher | Geophysical Institute, Kyoto University | en |
| dc.subject.ndc | 450 | - |
| dc.title | A COMPARISON OF SOME SCHEMES PARAMETERIZING CUMULUS CONVECTION BY NUMERICAL EXPERIMENTS | en |
| dc.type | departmental bulletin paper | - |
| dc.type.niitype | Departmental Bulletin Paper | - |
| dc.identifier.ncid | AA00617516 | - |
| dc.identifier.jtitle | Contributions of the Geophysical Institute, Kyoto University | en |
| dc.identifier.volume | 12 | - |
| dc.identifier.spage | 49 | - |
| dc.identifier.epage | 62 | - |
| dc.textversion | publisher | - |
| dc.sortkey | 07 | - |
| dcterms.accessRights | open access | - |
| 出現コレクション: | No.12 | |
このリポジトリに保管されているアイテムはすべて著作権により保護されています。