摘要
海洋锋是重要的海洋现象,具有重要的研究意义。尽管台湾以东与黑潮之间表层无明显的锋区,但在水下却常年存在较强的海洋锋,这一现象的研究至今尚少见,本研究采用再分析手段,系统分析了温度锋时空变化规律及其形成变化机制。
Oceanic front is an important phenomenon and is of great significance for research.Although the surface thermal front to the east of Taiwan is not obvious,there is an all-year strong Kuroshio thermal front under the surface,the research on which is rare at this time.Reanalysis method was used in this study to demonstrate the existence of thermal front in this area,study the temporal and spatial variation of the Kuroshio front and discuss the mechanism of frontogenesis.
出处
《海洋通报》
CAS
CSCD
北大核心
2011年第4期401-408,共8页
Marine Science Bulletin
基金
国家重点基础研究发展计划课题(2007CB816001)
国家自然科学基金项目(41030854
40906016
40906015)
关键词
黑潮锋
台湾以东
再分析
时空分布
形成机制
Kuroshio front
the east of Taiwan
reanalysis
temporal and spatial feature
frontogenesis
