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| ファイル | 記述 | サイズ | フォーマット | |
|---|---|---|---|---|
| b42p4n370p08.pdf | 269.68 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 | PAN, Tao | en |
| dc.contributor.author | HU, Yinqiao | en |
| dc.contributor.author | LIN, Peishun | en |
| dc.contributor.author | MITSUTA, Yasushi | en |
| dc.date.accessioned | 2010-09-08T08:27:18Z | - |
| dc.date.available | 2010-09-08T08:27:18Z | - |
| dc.date.issued | 1992-12 | - |
| dc.identifier.issn | 0454-7675 | - |
| dc.identifier.uri | http://hdl.handle.net/2433/124991 | - |
| dc.description.abstract | The structure of Planetary Boundary Layer (PBL) in the HEIFE area has been preliminarily studied by Doppler Sodar in August, 1990 at Huayin station. Evolution of the PBL can be described by the Mixed Layer (ML) height increasing rapidly in daytime, and holding for a short time after the nocturnal Stable Boundary Layer (SBL) is formed in the evening. A complete process including formation, growth and disappearance of the Low-Level Jet (LLJ) was observed on August 20, 1990. | en |
| dc.format.mimetype | application/pdf | - |
| dc.language.iso | eng | - |
| dc.publisher | Disaster Prevention Research Institute, Kyoto University | en |
| dc.title | An Analysis on the Vertical Structure of Wind Field Sounded by Doppler Sodar at Huayin | en |
| dc.type | departmental bulletin paper | - |
| dc.type.niitype | Departmental Bulletin Paper | - |
| dc.identifier.ncid | AA00581033 | - |
| dc.identifier.jtitle | Bulletin of the Disaster Prevention Research Institute | en |
| dc.identifier.volume | 42 | - |
| dc.identifier.issue | 4 | - |
| dc.identifier.spage | 115 | - |
| dc.identifier.epage | 124 | - |
| dc.textversion | publisher | - |
| dc.sortkey | 02 | - |
| dcterms.accessRights | open access | - |
| 出現コレクション: | Vol.42 Pt.4 | |
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