Response of upper ocean currents to typhoons at two ADCP moorings west of the Luzon Strait

Fei Chen; Yan Du; Li Yan; Dongxiao Wang; Ping Shi

doi:10.1007/s00343-010-0025-z

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Response of upper ocean currents to typhoons at two ADCP moorings west of the Luzon Strait

Updated：2023-05-16

- Response of upper ocean currents to typhoons at two ADCP moorings west of the Luzon Strait
- Journal of Oceanology and Limnology Vol. 28, Issue 5, Pages: 1002-1011(2010)
- Affiliations：
  
  1. LED South China Sea Institute of Oceanology Chinese Academy of Sciences
  2. GKSS Coastal Research Center
  3. Yantai Institute of Coastal Zone Research Chinese Academy of Sciences
- Author bio：
- Funds：
- DOI：10.1007/s00343-010-0025-z
  CLC：
- Online First：11 September 2010，
  
  Published：2010
- Accepted：
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Chen, F., Du, Y., Yan, L. et al. Response of upper ocean currents to typhoons at two ADCP moorings west of the Luzon Strait., Chin. J. Ocean. Limnol. 28, 1002–1011 (2010). https://doi.org/10.1007/s00343-010-0025-z
DOI：

Chen, F., Du, Y., Yan, L. et al. Response of upper ocean currents to typhoons at two ADCP moorings west of the Luzon Strait., Chin. J. Ocean. Limnol. 28, 1002–1011 (2010). https://doi.org/10.1007/s00343-010-0025-z DOI：

摘要

Abstract

We deployed two ADCP mooring systems west of the Luzon Strait in August 2008

and measured the upper ocean currents at high frequency. Two typhoons passed over the moorings during approximately one-month observation period. Using ADCP observations

satellite wind and heat flux measurements

and high-resolution model assimilation products

we studied the response of the upper ocean to typhoons. The first typhoon

Nuri

passed over one of the moorings

resulting in strong Ekman divergence and significant surface cooling. The cooling of surface water lagged the typhoon wind forcing about one day and lasted about five days. The second typhoon

Sinlaku

moved northward east of the Luzon Strait

and did not directly impact currents near the observation regions. Sinlaku increased anomalous surface water transport exchange across the Luzon Strait

which modulated the surface layer current of the Kuroshio.

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Keywords

references

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