Asymmetric chlorophyll responses enhanced by internal waves near the Dongsha Atoll in the South China Sea -- Journal of Oceanology and Limnology,2023,41(2):418-426

	Cite this paper:
	Meilin Wu, Huijie Xue, Fei Chai. Asymmetric chlorophyll responses enhanced by internal waves near the Dongsha Atoll in the South China Sea[J]. Journal of Oceanology and Limnology, 2023, 41(2): 418-426

Asymmetric chlorophyll responses enhanced by internal waves near the Dongsha Atoll in the South China Sea

Meilin Wu^1,2,3,4, Huijie Xue¹, Fei Chai¹

1. State Key Laboratory of Marine Environmental Science, College of Ocean and Earth Sciences, Xiamen University, Xiamen, 361102, China;
2. State Key Laboratory of Tropical Oceanography, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou, 510301, China;
3. Southern Marine Science and Engineering Guangdong Laboratory(Guangzhou), Guangzhou, 511458, China;
4. Innovation Academy of South China Sea Ecology and Environmental Engineering, Chinese Academy of Sciences, Guangzhou, 510301, China

Abstract:

Internal waves (IWs) are small-scale physical processes that occur frequently in stratified marginal seas. IWs are ubiquitous and well documented in the northern South China Sea (nSCS), but few studies have explored the ecosystem responses to the IWs. MODISA chlorophyll-a (Chl-a) data from 2002 to 2014 were used to examine the distribution of Chl a near the Dongsha Atoll (DSA). Composite Chl a from about 40 IWs during spring and summer showed stronger response on the northern side than on the southern side of the DSA. One day after the passage of IWs, composite surface Chl a on the northern side increased from 0.11 mg/m³ to a maximum mean value of 0.18 mg/m³. It decreased to 0.13 mg/m³ after two days and maintained that level for several days after the passage of IWs. The enhanced surface Chl a likely caused subsurface Chl-a maximum and nutrients in the surface layer. Approximately 64% of the increase in surface Chl a was due to the uplift of the subsurface Chl-a maximum one day after the passage of IWs, while nutrient-induced new phytoplankton growth contributed about 18% of the increase a few days later. When the IWs occurred frequently in spring and summer, Chl-a level on the northern side was about 30% higher than that on the southern side. IW dissipation and its impact on nutrients and chlorophyll were stronger on the northern side of the DSA than on the south, which caused a north-south asymmetric distribution of Chl a in the region.

Key words: internal waves (IWs)|phytoplankton|nutrients|Dongsha Atoll|northern South China Sea

Received: 2021-12-29 Revised:

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