Summertime Subtropical Countercurrent on isopycnals in the western North Pacific |
| |
Authors: | Rongfeng Li Xiaobao You P Chu |
| |
Institution: | (1) LASG Institute of Atmospheric Physics, Chinese Academy of Sciences, 100029 Beijing, China;(2) Department of Oceanography, Naval Postgraduate School, 93943 Monterey, CA, USA |
| |
Abstract: | Circulations on isopycnals (σθ) in the western North Pacific were investigated by using P-vector method; the data were taken from the U.S. Navy’s climatological
temperature and salinity dataset (public domain) with 1/2° ×1/2° resolution. Results not only show the main circulation systems
on isopycnals in the western North Pacific such as the North Equatorial Current (NEC), Kuroshio and Kuroshio Countercurrent,
but also reveal the Subtropical Countercurrent (STCC) clearly. In this note we pay attention to discussing the distribution
of STCC in summer (in June). The STCC flows eastward along a winding road; on shallow isopycnals, the STCC originates from
the area east of Bashi Strait at about 122.5°E; with the isopycnals increasing, the origin and flow core of STCC move to north
and east, but the main part of STCC is still between 18° and 23.5°N, i.e. near the Tropic of Cancer. There exists STCC on
all isopycnals between the sea surface and 25.8 σθ.
The current vectors of STCC on isopycnals are shown for the first time, and the distribution of the potential vorticity indicates
that STCC is just overlying the southern boundary of the Subtropical Mode Water (STMW). |
| |
Keywords: | P-vector method isopycnals Subtropical Countercurrent |
本文献已被 万方数据 SpringerLink 等数据库收录! |
| 点击此处可从《中国科学通报(英文版)》浏览原始摘要信息 |
| 点击此处可从《中国科学通报(英文版)》下载免费的PDF全文 |
|