Coupled ocean-atmospheric waves on the equatorial front

Shang Ping Xie, Masaki Ishiwatari, Hiroshi Hashizume, Kensuke Takeuchi

研究成果: Article査読

93 被引用数 (Scopus)

抄録

Striking 20-30-day sea surface temperature waves observed along the equatorial front in the later half of the year are generally believed to be of an oceanic origin. Here we report the detection of atmospheric waves that are unambiguously tied to these oceanic waves, using flew satellite measurements of surface winds. A general circulation model simulation reveals that these atmospheric waves have a shallow vertical structure trapped in the planetary boundary layer (PBL), unlike El Nino/Southern Oscillation where changes in deep convection are the cause of anomalous winds. Vertical wave motion penetrates well above the PBL and is likely to impact the distribution and transport of climatically important gas species such as ozone and dimethyl sulfide.

本文言語English
ページ(範囲)3863-3866
ページ数4
ジャーナルGeophysical Research Letters
25
20
DOI
出版ステータスPublished - 1998 10 15

ASJC Scopus subject areas

  • Geophysics
  • Earth and Planetary Sciences(all)

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