摘要
利用1958—2008年的北太平洋海表面高度和风应力资料,并与ENSO和PDO指数进行相关分析。结果发现,风应力及其经向分量主要通过季节振动影响海表面高度(SSH)的年周期变化,纬向风应力主要通过多年振动影响SSH的ENSO和PDO周期。纬向风应力和SSH均以黑潮延伸体主轴为界,两侧呈现出相反的升降趋势,SSH为北降南升,纬向风应力南降北升。风应力和SSH升降趋势相同,均表现为"上升—下降—上升"的变化特征。在地形变化剧烈、等深线南北分布的海区,西风增强会导致SSH升高,且西侧升高较为明显。北风增强将导致北太平洋西岸SSH升高,东岸SSH降低。
Correlation analysis between sea surface height, wind stress and index of ENSO and PDO for the period of 1958--2008 shows in the North Pacific Ocean, wind stress and its meridional component affect the annual cycle of SSH mainly through the seasonal vibration, and the zonal component affect the ENSO and PDO cycles of the SSH through years of vibration. Separated by the Kuroshio extension spindle, the zonal wind stress and SSH show different trends at the same side: SSH decreases at the north while increasing at the south, and the zonal wind stress decreases at the south while in- creasing at the north. Wind stress and SSH has the same trend: "increase--decrease--increase". The westerly enhanced the SSH rise in sea area where the topography is steep and isobaths distribute along the north-south direction, and the west side increased more significantly. The north wind enhancement led to SSH rise at the west coast of the North Pacific and drop at the east coast.
出处
《海洋与湖沼》
CAS
CSCD
北大核心
2013年第1期111-119,共9页
Oceanologia Et Limnologia Sinica
基金
国家自然科学基金项目“太平洋海平面变化的动力和热力学机制研究”,40976006号
科技部科技支撑项目“全球环境变化应对技术研究与示范”,2007BAC03A06号
海洋公益性行业科研专项“中国海平面变化预测及海岸带脆弱性风险评估技术与应用”专题,201005019,201105010,201105009号
关键词
北太平洋
海表面高度
风应力
厄尔尼诺
North Pacific Ocean, Sea Surface Height, Wind Stress, E1 Nifio