摘要
To study the variations in surface hydrography and circulation in northern South China Sea (NSCS), rotated empirical orthogonal function (REOF) and extended associate pattern analysis (EAPA) are used with daily sea surface salinity (SSS), sea surface temperature (SST) and sea surface height (SSH) datasets cover- ing 1 126 days from American Navy Experimental Real-Time East Asian Seas Ocean Nowcast System in this paper. Results show that in summer, the SCS Diluted Water Expansion (SDWE) is the most dominant factor con- trolling SSS variations in the NSCS. The remarkable SDWE usually begins in early July, reaches its maximum in middle August and weakens in late September. In summer flourishing period, its low saline core is just limited between 21°N and 22°N because of strong surface anomalous anticyclonic circulation in the NSCS. In early or late stage, the anomalous anticyclonic circulation becomes weak or turns into cyclonic one, thus the weak SCS diluted water can disperse. And its influence on the SSS variations has obviously decreased. The Kuroshio intrusion is the second controlling factor, and it has the almost opposite seasonal or intraseasonal oscillations and spatial charac- teristics to the SDWE. Winter Kuroshio Intrusion (WKI) begins in early November and lasts about three months. Intraseasonal Kuroshio Intrusion (IKI) takes place at any seasons. The westward Ekman transport produced by the north anomaly of East Asia Monsoon (EAM) pushes warmer and more saline seawater into the NSCS through the Bashi Strait and seems to decide the intensity of seasonal and intraseasonal Kuroshio intrusions.
To study the variations in surface hydrography and circulation in northern South China Sea （＇NSCS）, rotated empirical orthogonal function （REOF） and extended associate pattern analysis （EAPA） are used with daily sea surface salinity （SSS）, sea surface temperature （SST） and sea surface height （SSH） datasets covering 1 126 days from American Navy Experimental Real-Time East Asian Seas Ocean Nowcast System in this paper. Results show that in summer, the SCS Diluted Water Expansion （SDWE） is the most dominant factor controlling SSS variations in the NSCS. The remarkable SDWE usually begins in early July, reaches its maximum in middle August and weakens in late September. In summer flourishing period, its low saline core is just limited between 21°N and 22°N because of strong surface anomalous anticyclonic circulation in the NSCS. In early or late stage, the anomalous anticyclonic circulation becomes weak or turns into cyclonic one, thus the weak SCS diluted water can disperse. And its influence on the SSS variations has obviously decreased. The Kuroshio intrusion is the second controlling factor, and it has the almost opposite seasonal or intraseasonal oscillations and spatial characteristics to the SDWE. Winter Kuroshio Intrusion （WKI） begins in early November and lasts about three months. Intraseasonal Kuroshio Intrusion （IKI） takes place at any seasons. The westward Ekman transport produced by the north anomaly of East Asia Monsoon （EAM） pushes warmer and more saline seawater into the NSCS through the Bashi Strait and seems to decide the intensity of seasonal and intraseasonal Kuroshio intrusions.
基金
This work is supported by the Innovation Project of Chinese Academyof Sciences (KZCX3-SW-222)
关键词
海洋
水文地理学
循环变化
南海
SCS
variations, SCS diluted water expansion （SDWE）, intraseasonal Kuroshio intrusion （IKI）, winter Kuroshio intrusion （WKI）, empirical orthogonal function （REOF）, extended associate pattern analysis （EAPA）
