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翻訳と辞書　辞書検索 [ 開発暫定版 ] スポンサード リンク Mindanao Eddy ： ウィキペディア英語版 Mindanao Eddy The Mindanao Eddy (7°N, 128°E) is a semi-permanent cold-ring eddy formed in the retroflection area of the Mindanao Current. The Mindanao Eddy is bordered to the north by the North Equatorial Current and to the south by the North Equatorial Counter Current. The eddy has a diameter of 250 km and a cyclonic circulation.〔Aruda, W.Z. Eddies Along Western Boundaries. http://www.im.ufrj.br/~wilton/Papers/Wilton_PhDdiss.pdf〕 The Mindanao Eddy has been identified as potential grounds for fisheries due to upwelling.〔Primavera, K.H., Jacinto, G.S., San Diego-McGlon, M.L., Villanoy, C.L. Water Stability. Nutrient Flux, and Chlorophyll-a Distribution in the Mindanao Eddy. Natural Science. 8: 163-173.〕 == References == 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Mindanao Eddy」の詳細全文を読む スポンサード リンク 翻訳と辞書 : 翻訳のためのインターネットリソース Copyright(C) kotoba.ne.jp 1997-2016. All Rights Reserved.