Decadal change in the tropical Pacific Ocean

Hye Rim Kim, Soon II An

Research output: Contribution to conferencePaper

Abstract

Using the SODA-POP ocean assimilation data, the decadal evolution in the tropical Pacific Ocean spanning from 1961 to 1998 is analyzed. During the pre-1980, the ocean temperature anomalies in the meridional cross section were positive in the subsurface southwestern Pacific and negative in the surface layer of the tropical Pacific. This more or less stationary pre-1980's pattern reversed after early 1980s. Rather than gradual changing, an abrupt phase transition occurred between 1977 and 1981. During the transition period, the trade wind becomes weaker, and the warm subsurface water in the western Pacific moved toward the surface layer of the eastern equatorial Pacific as well as toward the subsurface in the northwestern Pacific. The transition mechanism resembles the recharge-oscillator hypothesis on the ENSO such that the warm water is accumulated in the western Pacific before the ENSO starts and the weakening of the trade wind may be related to the triggering mechanism.

Original languageEnglish
Publication statusPublished - 2007 Dec 1
Event87th AMS Annual Meeting - San Antonio, TX, United States
Duration: 2007 Jan 142007 Jan 18

Other

Other87th AMS Annual Meeting
CountryUnited States
CitySan Antonio, TX
Period07/1/1407/1/18

All Science Journal Classification (ASJC) codes

  • Environmental Engineering
  • Global and Planetary Change
  • Management, Monitoring, Policy and Law

Fingerprint Dive into the research topics of 'Decadal change in the tropical Pacific Ocean'. Together they form a unique fingerprint.

  • Cite this

    Kim, H. R., & An, S. II. (2007). Decadal change in the tropical Pacific Ocean. Paper presented at 87th AMS Annual Meeting, San Antonio, TX, United States.