莊文思2006-07-252018-06-282006-07-252018-06-282006http://ntur.lib.ntu.edu.tw//handle/246246/14869本計畫研究之海洋數值模式，將利用美國邁阿密大學發展的海洋數值模式MICOM（Miami Isopycnic Coordinate Ocean Model），模式範圍為95°E-160°E 及20°S-45°N，水平解析度約0.25°。預期模擬解釋1960-2003 年間南海海洋溫度場與流場之年變化、年際變化、各聖嬰事件對南海的影響程度，及南海與其鄰近海域間海洋互動機制之探討。The Miami Isopycnic Coordinate Ocean Model (MICOM) developed by University of Miami is organized and applied in this study. The model domain includes the western Pacific and the South China Sea with boundaries at 20.8°S, 45.1°N and 95°E, 160°E. The horizontal grid is defined on a Mercator projection with resolution given by 1/4° × 1/4°cosφ (meridional × zonal), where φ is the latitude. The model results of year 1960-2003 will be used to explore the annual and inter-annual variations of thermal and current in the South China Sea (SCS), the influences of various El Niño events on the SCS, the interaction mechanism of the South China Sea with its adjacent seas. The model output forced by the 6hourly winds is also available in the discussion of the Typhoon effect on the SCS. The MICOM model is mainly forced by the ECMWF model wind of resolution 2.5°x2.5° and assisted by the high resolution 0.5°x0.5° of satellite wind data, e.g. NSCAT（NASA Scatterometer）and QSCAT(NASA Quick Scatterometer).application/pdf678250 bytesapplication/pdfzh-TW國立臺灣大學海洋研究所數值模式年變化年際變化聖嬰事件南海reporthttp://ntur.lib.ntu.edu.tw/bitstream/246246/14869/1/932611M002014.pdf