摘要
通过对欧空局提供的ERS卫星微波散射计风场资料的再分析,研究了南沙群岛海域的风场特征,主要包括南沙群岛海域的东北季风和西南季风随纬度的变化以及一年中根据风应力特征划分的4个时期的风应力与风应力旋度的分布特征。
The ERS microwave scatterometer wind data was reanalyzed to study the fea-
tures of the wind field in the Nansha Islands waters, southern South China Sea, inclu-
ding the latitudinal variations of northeast and southwest monsoons and the distribution
characters of wind stress fields as well as the wind stress vorticity fields in four phases
which are divided according to the different features of wind stress in the Nansha Islands
waters. The following results were obtained. (1) The presence frequency of northeast
(southwest) monsoon decreases (increases) with latitude decreasing. (2) In the north-
east monsoon phase (from Nov. to Mar. ), strong northeast monsoon prevails over the
Nansha Islands waters, stronger in the northwest part than in the southeast part. The
wind stress vorticity is the strongest in the first three months and starts to weaken in
February and becomes the weakest in March. (3) During the transition between mon-
soons in Apr. and May, the northeast monsoon still controls the Nansha Islands wa-
ters, but the vorticity almost reaches 0. Usually the southwest monsoon bursts in May,
when the Nansha Islands waters is still controlled by the very weak southwest monsoon,
but the vorticity has become negative in most parts. (4) The southwest monsoon phase
is from June to the end of September. The distribution of wind speed is similar to that in
the northeast monsoon phase. The wind stress vorticity is negative in the south and pos-
itive in the northwest part. (5) During the transition between monsoons in Oct., the
northeast monsoon firstly controls the north part, while the southwest monsoon still
controls the south part (south to 8°N), which indicates that the transition begins in the
north part of the Nansha Islands waters.
出处
《热带海洋学报》
CAS
CSCD
北大核心
2003年第4期18-25,共8页
Journal of Tropical Oceanography
基金
国家重点基础研究发展规划项目(G1999043805
G1999043807)
关键词
南沙群岛海域
东北季风
西南季风
风应力旋度
Nansha Islands waters
northeast monsoon
southwest monsoon
wind stress vorticity