Coupled response of the trade wind, SST gradient, and SST in the caribbean sea, and the potential impact on loop current's interannual variability

Y. L. Chang, L. Y. Oey*

*此作品的通信作者

    研究成果: 雜誌貢獻期刊論文同行評審

    27 引文 斯高帕斯(Scopus)

    摘要

    Air-sea coupling in the IntraAmerican seas (IAS; Caribbean Sea and Gulf of Mexico) is studied through analyses of observational data from satellite, reanalysis products, and in situ measurements.Astrong coupling is found between the easterly trade wind 2U and meridional SST gradient ≥T/≥y across a localized region of the southern-central Caribbean Sea from seasonal and interannual to decadal time scales. The ≥T/≥y anomaly is caused by a variation in the strength of coastal upwelling off the Venezuelan coast by the wind, which in turn strengthens (weakens) for stronger (weaker) ≥T/≥y. Wind speeds and seasonal fluctuations in IAS have increased in the past two decades with a transition near 1994 coinciding approximately with when the Atlantic multidecadal oscillation (AMO) turned from cold to warm phases. In particular, the seasonal swing from summer's strong to fall's weak trade wind has become larger. The ocean's upper-layer depth has also deepened, by as much as 50% on average in the eastern Gulf of Mexico. These conditions favor the shedding of eddies from the Loop Current, making it more likely to shed at a biannual frequency, as has been observed from altimetry data.

    原文英語
    頁(從 - 到)1325-1344
    頁數20
    期刊Journal of Physical Oceanography
    43
    發行號7
    DOIs
    出版狀態已發佈 - 2013

    ASJC Scopus subject areas

    • 海洋學

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