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ファイル | 記述 | サイズ | フォーマット | |
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a18b0p45.pdf | 376.2 kB | Adobe PDF | 見る/開く |
タイトル: | ひうち灘の海面における熱収支 |
その他のタイトル: | HEAT BALANCE AT THE SEA SURFACE OVER HIUCHINADA IN SETO INLAND SEA |
著者: | 田中, 正昭 中島, 暢太郎 |
著者名の別形: | TANAKA, Masaaki NAKAJIMA, Chotaro |
発行日: | 1-Apr-1975 |
出版者: | 京都大学防災研究所 |
誌名: | 京都大学防災研究所年報. B |
巻: | 18 |
号: | B |
開始ページ: | 589 |
終了ページ: | 595 |
抄録: | In order to investigate the heat balance at the sea surface over Hiuchinada in SetoInland Sea, observations of Sea-surface temperature, radiation and precipitation were madeat Uoshima Island located in the central part of Hiuchinada from Oct. 1972 to Oct. 1973.The seasonal variation of observed radiation is likely to the sine curve with a period of ayear and maximum value appears in July and minimum one in December. That of observedsea-surface temperature is also likely to the sine curve, but phase of the variation of sea-surface temperature lags about 2. 5 months behind that of radiation.Calculated average annual values of the heat balance terms were as follows; net short--wave radiation QA: 270 ly/day, net long-wave radiation QB: 130 ly/day, latent heat transferQe: 105 ly/day, sensible heat transfer Qh: 25 ly/day. Then, gains and losses of energy atthe sea surface must balance at Hiuchinada through the year. |
URI: | http://hdl.handle.net/2433/69974 |
関連リンク: | http://www.dpri.kyoto-u.ac.jp/nenpo/nenpo.html |
出現コレクション: | No.18 B |
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