Dynamic Response of Atmospheric and Ocean Parameters and Their Relation to Typhoon Haikui (2012) Using Satellite Data-Reference-Cited by-同舟云学术

Dynamic Response of Atmospheric and Ocean Parameters and Their Relation to Typhoon Haikui (2012) Using Satellite Data

Published:2023-03-08 Issue:3 Volume:14 Page:518
ISSN:2073-4433
Container-title:Atmosphere
language:en
Short-container-title:Atmosphere

Author:

Zhu Wangyuan¹²,Subrahmanyam Mantravadi Venkata¹^ORCID,Wang Liuzhu¹,Guo Biyun¹³

Affiliation:

1. School of Marine Science and Technology, Zhejiang Ocean University, Zhoushan 316022, China

2. Zhejiang Haida Marine Survey, Planning and Design Co., Ltd., Zhoushan 316022, China

3. State Key Laboratory of Hydroscience and Engineering, Tsinghua University, Beijing 100084, China

Abstract

Typhoon Haikui (2012) occurred in the northwestern Pacific Ocean, and landfall on the east coast of China brought heavy rainfall with strong winds. Because of Typhoon Haikui, sea surface temperature (SST) cooling of 3 °C occurred on the right side of the track, mainly due to Ekman transport and upwelling. SST cooling on the left side was lower than on the right side, mainly due to the rainfall. Heavy precipitation occurred on both sides of the typhoon track; however, rainfall was higher on the left side of the typhoon track. This paper explains the dynamic process between atmospheric and oceanographic parameters and verifies the variations in chlorophyll and sea surface height data before, during, and after the typhoon. Typhoon Haikui demonstrates dynamic variations and intuitively illustrates the relationship between the ocean and atmospheric parameters.

Funder

Tsinghua university

Chinese Academy of Sciences

Publisher

MDPI AG

Subject

Atmospheric Science,Environmental Science (miscellaneous)

Link

https://www.mdpi.com/2073-4433/14/3/518/pdf

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