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ファイル | 記述 | サイズ | フォーマット | |
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cgk01300_053.pdf | 440.99 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 |
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dc.contributor.author | FUJITA, Masanobu | en |
dc.date.accessioned | 2013-09-02T04:37:24Z | - |
dc.date.available | 2013-09-02T04:37:24Z | - |
dc.date.issued | 1973-12 | - |
dc.identifier.uri | http://hdl.handle.net/2433/178636 | - |
dc.description.abstract | An observation of river water dispersion was carried out in Lake BIWA a few times in 1972. We observed the temperature and electric conductivity as tracers of the river water. The dispersion patterns could be classified in the following three cases. Case 1 : The river water flows into the lake and disperses in the upper layer of the lake water. Case 2: The river water flows parallel to the coast with the longshore currents made by the wind and breaking of the incident waves. Case 3: The river water sinks at the river mouth and disperses along the lake bottom. | en |
dc.format.mimetype | application/pdf | - |
dc.language.iso | eng | - |
dc.publisher | Geophysical Institute, Kyoto University | en |
dc.subject.ndc | 450 | - |
dc.title | DISPRESION PATTERNS OF RIVER WATER IN LAKE BIWA | 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 | 13 | - |
dc.identifier.spage | 53 | - |
dc.identifier.epage | 64 | - |
dc.textversion | publisher | - |
dc.sortkey | 07 | - |
dcterms.accessRights | open access | - |
出現コレクション: | No.13 |

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