Characteristics and mechanisms of the upwelling in the southern Taiwan Strait: a three-dimensional numerical model study
Characteristics and mechanisms of the upwelling in the southern Taiwan Strait: a three-dimensional numerical model study
复制标题
台湾海峡南部上升流特征及机制：三维数值模型研究
DOI：
10.1007/s10872-011-0080-x
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发表时间：
2011-10
影响因子：
2.3
通讯作者：
Hong, Huasheng
中科院分区：
文献类型：
--
作者：
Jiang, Yuwu;Chai, Fei;Wan, Zhenwen;Zhang, Xin;Hong, Huasheng
本文利用基于普林斯顿海洋模式的嵌套环流模式，研究了台湾海峡南部两个主要的上升流：西南上升流和台湾岸上升流的特征和机制。西南上升流存在于西南季风占主导地位的夏季，台湾浅滩上升流出现的时间较长，从5月到9月。在明显加宽的陆架上的上坡流将下层冷水向岸上输送，西南季风风将冷水向表层输送，形成西南上升流，而潮余流则减弱了上坡平流。对于台湾浅滩上升流，由于浅滩地形，南海水的向上输送将冷水从次表层带到台湾浅滩附近约25 m的深度，然后强烈的潮汐混合迫使该上升流进一步向上到达表层。
Using a nested circulation model based on the Princeton Ocean Model, we investigate the characteristics and mechanisms of two main upwellings in the southern Taiwan Strait: the Southwest upwelling and the Taiwan Bank upwelling. The Southwest upwelling exists in summer when the southwesterly monsoon dominates, and the Taiwan Bank upwelling occurs over a longer period from May to September. The upslope current over a distinctly widened shelf transports the cold water on-shoreward at the lower layer and the southwesterly monsoon wind drives the cold water to the surface layer, forming the Southwest upwelling, while tidal residual current weakens the upslope advection. For the Taiwan Bank upwelling, the upward transport of the South China Sea water due to the Bank topography carries the cold water from the subsurface layer to the depth of approximately 25 m near the Taiwan Bank, then the strong tidal mixing forces this upwelled water further upward to the surface layer.
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DOI：
10.1016/0278-4343(82)90001-2
发表时间：
1982-11
期刊：
--
影响因子：
--
作者：
G. Janowitz;L. Pietrafesa
通讯作者：
G. Janowitz;L. Pietrafesa
影响因子：
13.5
作者：
Caiyun Zhang;Chuanmin Hu;S. Shang;F. Muller‐Karger;Yan Li;M. Dai;Bangqin Huang;X. Ning;H. Hong
通讯作者：
Caiyun Zhang;Chuanmin Hu;S. Shang;F. Muller‐Karger;Yan Li;M. Dai;Bangqin Huang;X. Ning;H. Hong
影响因子：
3.6
作者：
Jan, Sen;Sheu, David D.;Kuo, Huei-Ming
通讯作者：
Kuo, Huei-Ming
DOI：
10.1016/0198-0149(81)90006-6
发表时间：
1981-01-01
期刊：
DEEP-SEA RESEARCH PART A-OCEANOGRAPHIC RESEARCH PAPERS
影响因子：
--
作者：
BLANTON, JO;ATKINSON, LP;LEE, TN
通讯作者：
LEE, TN
影响因子：
13.5
作者：
D. Tang;D. R. Kester;I. Ni;H. Kawamura;H. Hong
通讯作者：
D. Tang;D. R. Kester;I. Ni;H. Kawamura;H. Hong