太平洋温帯の地域移動のメカニズム:ENSOへの影響

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Updated: Jul 11, 2026

Evolution of Staircase Structures in Diffusive Convection
07:28

Evolution of Staircase Structures in Diffusive Convection

Published on: September 5, 2018

Picaut1, Ioualalen, Menkes

  • 1J. Picaut, M. Ioualalen, T. Delcroix, Groupe SURTROPAC, Institut Francais de Recherche Scientifique pour le Developpement en Cooperation (ORSTOM), BP A5, 98848, Noumea, New Caledonia. C. Menkes, Centre de Recherche Oceanographique, ORSTOM, Abidjan, Ivory Coast. M. J. McPhaden, Pacific Marine Environmental Laboratory, National Oceanic and Atmospheric Administration, Seattle, WA 98115, USA.

Science (New York, N.Y.)
|November 29, 1996
PubMed
まとめ

西赤道太平洋の温水池は,海流によって誘発される南方振動指数とともに東西に移動する. これらのアドベクティブプロセスは暖かいプールを形成し,エルニーニョ-南方振動 (ENSO) 相互作用に影響を与えます.

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