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    Please use this identifier to cite or link to this item: https://ir.lib.ncu.edu.tw/handle/987654321/102428


    Title: Rossby waves and eddies observed at a temperature mooring in northern South China sea
    Authors: 黃如瑤;Lin, Y.-C.;Oey, L.-Y.;Wang, J.;Liu, K.-K.
    Contributors: 地球科學學院水文與海洋科學研究所
    Keywords: Altimetry;Eddies;Fluctuations;Marine;Ocean circulation;Ocean currents;Studies;Temperature;Time series;Wind;Winter
    Date: 2016-01-01
    Issue Date: 2026-04-23 11:08:32 (UTC+8)
    Publisher: American Meteorological Society;Boston: American Meteorological Society
    Abstract: 摘要: Annual Rossby waves in northern South China Sea had previously been studied using altimetry and model data; however, how they connect to subsurface temperature fluctuations has not been examined. This study analyzed a 22-month, surface to −500-m temperature time series at 18.3°N, 115.5°E, together with satellite and other data, to show the arrivals near z ≈ −300 m and deeper cool (warm) Rossby waves after their generation near the Luzon Strait in winter (summer). Temperature fluctuations with time scales of a few weeks, and with maximum anomalies near z ≈ −100 m, were also found embedded in the smooth Rossby waves and caused by propagating eddies. Eddy fluctuations and propagation past the mooring were of two types: southwestward from southwestern Taiwan, triggered by Kuroshio intrusion that produced anticyclone–cyclone pairs in late fall and winter, and eddies propagating westward from Luzon forced by annual anomalies of wind stress curl and Kuroshio path in the Luzon Strait
    出版者: Boston: American Meteorological Society
    出版日期: 2016-02-01
    出處: Journal of physical oceanography, 2016-02, Vol.46 (2), p.517-535
    資源來源: Agricultural & Environmental Science Collection
    版權: Copyright American Meteorological Society Feb 2016
    識別號: ISSN: 0022-3670
    識別號: EISSN: 1520-0485
    識別號: DOI: 10.1175/JPO-D-15-0094.1
    Appears in Collections:[Graduate Institute of Hydrological and Oceanic Sciences] journal & Dissertation

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