SEASONAL REVERSE OF SEA SURFACE SLOPE IN THE NORTHERN YELLOW SEA AND ITS DYNAMIC RELATION WITH MONSOON EFFECTS

Based on the monthly average sea level data from the tide gauge measurement(1999-2001),the seasonal variability of the sea level in the Northern and Middle Yellow Sea is studied to reveal that the sea surface height at all the tide gauges becomes higher in summer than that in winter.In addition,the sea surface height of the Northern Yellow Sea is higher than the one of the Middle Yellow Sea with a slope downward from the north to the south in summer,while it is lower with a reversed slope in winter.The seasonal reverse of the sea surface slope can be attributed to the monsoon effects i.e.the annual reverse of the monsoon direction and the annual variation of the monsoon rainfall.A set of equations are established in light of the dynamic principles to expound how the monsoon forcing and the sea surface slope generate a summer outflow and a winter inflow in the Yellow Sea.

作 者： PU Shu-zhen CHENG Jun ZHANG Yi-jun SHI Qiang   作者單位： PU Shu-zhen,CHENG Jun(Key Laboratory of Marine Science and Numerical Modeling,The First Institute of Oceanography,State Oceanic Administration,Qingdao 266061,China)

ZHANG Yi-jun(Marine Information Center,State Oceanic Administration,Tianjin 300171,China)

SHI Qiang(North Sea Branch of State Oceanic Administration,Qingdao 266033,China) 

刊 名： 水動(dòng)力學(xué)研究與進(jìn)展B輯  ISTIC EI 英文刊名： JOURNAL OF HYDRODYNAMICS  年，卷(期)： 2004 16(5)  分類號： P7  關(guān)鍵詞： Yellow Sea   sea surface slope   monsoon driven current   dynamics  

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