Interannual variability of the subtropical countercurrent eddies in the North Pacific associated with the Western-Pacific teleconnection pattern

被引：11

作者：

Chow, Chun Hoe ^{[1
,4
]}

Tseng, Yu-heng ^{[2
]}

Hsu, Huang-Hsiung ^{[1
]}

Young, Chih-Chieh ^{[3
]}

机构：

[1] Acad Sinica, Res Ctr Environm Changes, Taipei, Taiwan

[2] Natl Ctr Atmospher Res, Climate & Global Dynam Div, Boulder, CO USA

[3] Natl Taiwan Univ, Hydrotech Res Inst, Taipei, Taiwan

[4] Natl Sun Yat Sen Univ, Dept Oceanog, Kaohsiung, Taiwan

来源：

CONTINENTAL SHELF RESEARCH | 2017年 / 143卷

基金：

美国国家科学基金会;

关键词：

Oceanic eddies; Pycnocline shoaling; Western Pacific teleconnection; Air-sea interaction; Interannual variability; SATELLITE-OBSERVATIONS; EAST; TRANSPORT; TAIWAN; HEAT; TOPEX/POSEIDON; TEMPERATURE; CLIMATE; FIELD; ENSO;

D O I：

10.1016/j.csr.2016.08.006

中图分类号：

P7 [海洋学];

学科分类号：

0707 ;

摘要：

The connection and the relevant dynamical processes between oceanic eddies in the North Pacific Subtropical Countercurrent (STCC) region and the atmospheric Western-Pacific (WP) teleconnection is investigated on interannual timescales. North of the STCC region, the local northerly surface wind anomalies cool the ocean surface during negative phases of the WP teleconnection. The local surface cooling modifies the meridional gradient of sea surface temperature (SST), strengthening the SST front at its south. In the STCC region, we show the meridional gradient of surface-heat-flux forcing caused by the local surface cooling is the same order as the Ekman-convergence forcing. The strengthened SST front then leads to the pycnocline shoaling in the STCC region, which can also enhance the growth of baroclinic instability to produce more oceanic eddies, in addition to the enhanced STCC proposed previously. These dynamics are reversed during the positive phases of WP teleconnection.

引用

页码：175 / 184

页数：10