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| ファイル | 記述 | サイズ | フォーマット | |
|---|---|---|---|---|
| sgk00700_095.pdf | 868.56 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 | SAHASHI, Ken | en |
| dc.date.accessioned | 2013-09-02T04:22:36Z | - |
| dc.date.available | 2013-09-02T04:22:36Z | - |
| dc.date.issued | 1967-12 | - |
| dc.identifier.issn | 0454-7837 | - |
| dc.identifier.uri | http://hdl.handle.net/2433/178541 | - |
| dc.description.abstract | The evaporation rates from the water and soil surfaces are estimated by the eddy-correlation method which is, in principle, the most reasonable one, using a sonic anemometer and a fine thermocouple psychrometer. Cospectral analysis shows that the method seems to be applicable to the estimation of evaporation rate, in spite of rather long averaging time of 1 sec and short sampling duration of 5 min, taken here. The results are compared with those by the aerodynamic method, the heat-balance method and the pan method. It is found that there is a fairly good agreement between the results by the eddy-correlation method and those by Thornthwaite-Holzman's formula. | en |
| dc.format.mimetype | application/pdf | - |
| dc.language.iso | eng | - |
| dc.publisher | Geophysical Institute, Kyoto University | en |
| dc.subject.ndc | 450 | - |
| dc.title | ESTIMATION OF EVAPORATION RATE BY USE OF A SONIC ANEMOMETER | en |
| dc.type | departmental bulletin paper | - |
| dc.type.niitype | Departmental Bulletin Paper | - |
| dc.identifier.ncid | AA00423961 | - |
| dc.identifier.jtitle | Special Contributions of the Geophysical Institute, Kyoto University | en |
| dc.identifier.volume | 7 | - |
| dc.identifier.spage | 95 | - |
| dc.identifier.epage | 109 | - |
| dc.textversion | publisher | - |
| dc.sortkey | 13 | - |
| dcterms.accessRights | open access | - |
| dc.identifier.pissn | 0454-7837 | - |
| 出現コレクション: | No.7 | |
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