

FOLLOWUS
1.Key Laboratory of Ocean Observation and Forecasting, Qingdao 266071, China
2.Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China
3.Key Laboratory of Ocean Circulation and Waves, Institute of Oceanology, Qingdao 266071, China
4.University of Chinese Academy of Sciences, Beijing 100049, China
yangbing@qdio.ac.cn
收稿:2025-01-17,
录用:2025-03-09,
网络首发:2025-06-06,
纸质出版:2026-03-01
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Haoyu WANG, Bing YANG, Yuqi YIN, 等. Mechanisms of upper ocean chlorophyll
WANG Haoyu,YANG Bing,YIN Yuqi,et al.Mechanisms of upper ocean chlorophyll ,a response to fast-moving Typhoon Hagupit in South China Sea[J].Journal of Oceanology and Limnology,2026,44(02):528-544.
Haoyu WANG, Bing YANG, Yuqi YIN, 等. Mechanisms of upper ocean chlorophyll
WANG Haoyu,YANG Bing,YIN Yuqi,et al.Mechanisms of upper ocean chlorophyll ,a response to fast-moving Typhoon Hagupit in South China Sea[J].Journal of Oceanology and Limnology,2026,44(02):528-544. DOI: 10.1007/s00343-025-5018-z.
Typhoons can induce significant changes in the upper ocean
increasing sea surface nutrients via mixing
entrainment
and upwelling
which often leads to a substantial phytoplankton bloom in an oligotrophic region of the South China Sea (SCS)
subsequently triggers carbon cycling and ecosystem responses
and enhances local marine primary productivity. Using a coupled physical-biogeochemical model
we analyzed the dynamic and ecological responses of the shelf region near the Dongsha Islands in the SCS caused by the fast-moving Typhoon Hagupit
and investigated the underlying mechanisms of sea surface chlorophyll-
a
increase. Results indicate that after Hagupit
sea surface temperature along the typhoon path rapidly decreased by maximum of 5.2 °C
and the chlorophyll
a
along the typhoon path increased. In the shelf region near the Dongsha Islands
the sea surface chlorophyll
a
increased from 0.07 mg/m
3
(weekly average) to 0.14 mg/m
3
after Hagupit. The maximum increase reached 0.16 mg/m
3
occurred 6 days after Hagupit
which is more than twice the average concentration before the typhoon. In contrast
the subsurface chlorophyll
a
decreased from 0.18 to
0.10 mg/m
3
. Power spectral analysis of horizontal velocity indicated that Hagupit triggered strong near-inertial waves (NIWs)
which had a period of approximately 31.45 h
slightly greater than the local inertial period
and lasted for about one week. Therefore
we believed that while fast-moving typhoons cannot induce strong Ekman pumping velocity (EPV) as slow-moving ones do
they can trigger NIWs. The NIWs enhanced turbulent mixing in the upper 60 m
causing directly a rapid increase in sea surface chlorophyll
a
and nutrients after the typhoon. Two to three days later
the nitrates uptake by sea surface phytoplankton increased
promoting phytoplankton growth. Therefore
the variability in upper-ocean chlorophyll
a
induced by fast-moving typhoons involves not only strong dynamic processes but also significant participation of marine biological processes.
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