In this paper, we synthetically analyses the data of marine survey during January to February 1964, December 1983 ad January 1984 in and northern Parts of Taiwan strait. It preliminarily shows, that main factors of Mi...In this paper, we synthetically analyses the data of marine survey during January to February 1964, December 1983 ad January 1984 in and northern Parts of Taiwan strait. It preliminarily shows, that main factors of Minzhong coastal upwelling formation in summer- the northward current (strait warm current) and its on-shore component caused by the influence of topography also exist in winter. The main indication of Minzhong coastal upwelling existing in winter are the temperature and salinity fronts caused by the mixing of different water mass sloping from surface layer of Offlying sea to near-bottom layer of sea near-shore, cross flow existing in vertical coast direction and ome zooplankton of high temperature offlying sea emerging.展开更多
文摘In this paper, we synthetically analyses the data of marine survey during January to February 1964, December 1983 ad January 1984 in and northern Parts of Taiwan strait. It preliminarily shows, that main factors of Minzhong coastal upwelling formation in summer- the northward current (strait warm current) and its on-shore component caused by the influence of topography also exist in winter. The main indication of Minzhong coastal upwelling existing in winter are the temperature and salinity fronts caused by the mixing of different water mass sloping from surface layer of Offlying sea to near-bottom layer of sea near-shore, cross flow existing in vertical coast direction and ome zooplankton of high temperature offlying sea emerging.
