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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 | |
|---|---|---|---|---|
| sgk00500_073.pdf | 329.15 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 | MITSUTA, Yasushi | en |
| dc.date.accessioned | 2013-08-30T06:34:34Z | - |
| dc.date.available | 2013-08-30T06:34:34Z | - |
| dc.date.issued | 1965-11 | - |
| dc.identifier.issn | 0454-7837 | - |
| dc.identifier.uri | http://hdl.handle.net/2433/178486 | - |
| dc.description.abstract | The results of the test observation of radio isotope snow gauge at Kariyasu Pass in the source region of Kurobe River are discussed. The total winter precipitation at this point is as large as that in summer and does not change year to year as snowfall on lowlands. In case of heavy snow, snowfall distribution on mountains and coast is affected by stability of airflow. Runoff in spring from snowmelting is closely related to rainfall. | en |
| dc.format.mimetype | application/pdf | - |
| dc.language.iso | eng | - |
| dc.publisher | Geophysical Institute, Kyoto University | en |
| dc.subject.ndc | 450 | - |
| dc.title | WINTER PRECIPITATION ON HIGH MOUNTAINS | 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 | 5 | - |
| dc.identifier.spage | 73 | - |
| dc.identifier.epage | 79 | - |
| dc.textversion | publisher | - |
| dc.sortkey | 09 | - |
| dcterms.accessRights | open access | - |
| dc.identifier.pissn | 0454-7837 | - |
| 出現コレクション: | No.5 | |
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