Influence of mechanical mixing on a low summertime SST in the western North Pacific ITCZ region

N. Sato, H. Tokinaga, R. Shirooka, N. Suginohara

研究成果: ジャーナルへの寄稿記事

4 引用 (Scopus)

抜粋

A region with a low sea-surface temperature (SST) was identified in the western North Pacific (WNP) Intertropical Convergence Zone (ITCZ) or warm water pool region in boreal summer. The SST decreases by up to 0.5°C from May to the June-July-August (JJA) season just east of Mindanao Island. Analyses of the observed data indicated that a northeastward surface current constantly exists throughout the year, supplying cold subsurface water through the Molucca Strait. As a result, the subsurface water is colder by several degrees compared with that in the surrounding regions. The sea-surface wind is strong over this region in the JJA season. Examination of Argo float data demonstrated that the mixed layer becomes deeper from May to the JJA season. It is suggested that the strong wind causes vertical mixing between the surface and subsurface layers, resulting in the low summertime SST.

元の言語英語
記事番号L14608
ジャーナルGeophysical Research Letters
33
発行部数14
DOI
出版物ステータス出版済み - 7 1 2006
外部発表Yes

All Science Journal Classification (ASJC) codes

  • Geophysics
  • Earth and Planetary Sciences(all)

フィンガープリント Influence of mechanical mixing on a low summertime SST in the western North Pacific ITCZ region' の研究トピックを掘り下げます。これらはともに一意のフィンガープリントを構成します。

  • これを引用