初春の北海道噴火湾における湾水の流出構造

DOI PDF Web Site Web Site 被引用文献4件 参考文献2件

書誌事項

タイトル別名
  • Outflow of water from Funka Bay, Hokkaido, during early spring.
公開日
1988
DOI
  • 10.1007/bf02302640
公開者
日本海洋学会

この論文をさがす

説明

Observations were made to study the oceanographic structure of the dense water formation and its outflow from Funka Bay, Hokkaido, during early spring. The winter Funka Bay water, which was transformed from the warm water of the Tsugaru Current, due to cooling and deep convection during the winter, flowed from the bay, while forming a frontal structure. The width and inclination of the density front were about 3n. miles and 1.4×10-2, respectively, during the early spring of 1982. These values roughly coincided with calculated values of 2.6n. miles and 1.7×10-2 using the sill flow model proposed by Whitehead et al.(1974). Observed current speeds and directions were also similar to those predicted by the model. The renewal time of bay water with this flow was estimated to be about 51 days, which is consistent with the results of previous studies.

収録刊行物

被引用文献 (4)*注記

もっと見る

参考文献 (2)*注記

もっと見る

詳細情報 詳細情報について

問題の指摘

ページトップへ