Response of Sea Surface Temperature and Chlorophyll-a to Typhoon Lekima (2019)

Author:

Shi Yaowei1,Guo Biyun12ORCID,Niu Yuqian34,Mantravadi Venkata Subrahmanyam5ORCID,Wang Jushang1,Ji Zhaokang1,Che Yingliang1,Ye Menglu1

Affiliation:

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

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

3. Ocean College, Zhejiang University, Zhoushan 316022, China

4. State Key Laboratory of Satellite Ocean Environment Dynamics, Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou 310012, China

5. School of Marine Science and Technology, Hainan Tropical Ocean University, Sanya 572022, China

Abstract

Typhoon (hurricane) is the most influential process of ocean–air interaction on the synoptic scale; it has a great influence on the heat exchange, mixing and ecological processes in the upper ocean, which in turn affect sea surface temperature (SST), leading to chlorophyll-a (Chl-a) concentration variation. SST is also an important factor affecting marine fishery resources. Chl-a is closely related to the marine ecosystem and primary productivity. In this study, we analyzed the response of SST and Chl-a to Typhoon Lekima (2019) process. The result indicates that the response of temperature to typhoon decreases from the center to the outer edge, which has a good correlation with the location, path and influence area of the typhoon center. The mean SST in the study area (14°~40° N, 116°~136° E) decreased during the typhoon’s passage, from 28.97 °C at the beginning (5 August) to 28.22 °C (15 August). The concentration of Chl-a was high in the northwest and coastal areas; its mean value in the study area decreased from 2 to 8 August (on 2 and 8 August, the concentration was 0.484 mg/m3 and 0.405 mg/m3, respectively). From 8 to 14 August, Chl-a decreased with the increase in SST, and 10 and 14 August were the two peak values of Chl-a (while SST was low). Chl-a concentration increased after the typhoon’s landfall (from 15 to 31 August); the Chl-a trend was the same as that of SST. The stronger the typhoon and the longer the residence time, the greater the contribution to the increase in Chl-a concentration at sea surface. Typhoon-induced rainfall over the ocean surface, increased evaporation of seawater, enhanced mixing within the mixed layer and upwelling of the pycnocline resulted in an increase in Chl-a quantity. This study describes the spatial response of the upper ocean to typhoons. It provides a general method for the comprehensive assessment of typhoons in marginal seas and upper open oceans, which has wide applicability and good scientific application prospects.

Funder

Consultation and Evaluation Program of the Department of Chinese Academy of Science

open research fund program of State Key Laboratory of Hydroscience and Engineering, Tsinghua University

China Scholarship Council

National College Students Innovation and Entrepreneurship Training Program

Zhejiang University Students Science and Technology Innovation Activity Plan

Open Research Fund Program of Key Laboratory for Water Ecology Management and Protection in River Source Areas, Ministry of Water Resources

National Natural Science Foundation of China

Publisher

MDPI AG

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