Extreme Sea-Surface Cooling Induced by Eddy Heat Advection During Tropical Cyclone in the North Western Pacific Ocean

Extreme Sea-Surface Cooling Induced by Eddy Heat Advection During Tropical Cyclone in the North Western Pacific Ocean

A tropical cyclone (TC) usually induces strong sea-surface cooling due to vertical mixing. In turn, surface cooling influences the intensities and tracks of TCs. Therefore, the relationship between sea-surface temperature (SST) and TC is one of the important components of air-sea interaction. Sea-su...

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Bibliographic Details
Main Authors: Chunhua Qiu, Hong Liang, Xiujun Sun, Huabin Mao, Dongxiao Wang, Zhenhui Yi, Anindya Wirasatriya
Format: Article
Language:English
Published: Frontiers Media S.A. 2021-10-01
Series:Frontiers in Marine Science
Subjects:
wave-glider
eddy heat advection
sea surface cooling
tropical cyclone
Western north pacific (WNP)
Online Access:https://www.frontiersin.org/articles/10.3389/fmars.2021.726306/full

Internet

https://www.frontiersin.org/articles/10.3389/fmars.2021.726306/full

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