A Positive Feedback Onto ENSO Due to Tropical Instability Wave (TIW)-Induced Chlorophyoll Effects in the Pacific

doi:10.1029/2018GL081275

IOCAS-IR > 海洋环流与波动重点实验室

	A Positive Feedback Onto ENSO Due to Tropical Instability Wave (TIW)-Induced Chlorophyoll Effects in the Pacific
	Tian, Feng 1,2; Zhang, Rong-Hua1,2,3,4 ; Wang, Xiujun 5
	2019-01-28
发表期刊	GEOPHYSICAL RESEARCH LETTERS
ISSN	0094-8276
卷号	46 期号:2 页码:889-897
通讯作者	Zhang, Rong-Hua([email protected])
摘要	Tropical instability waves (TIWs) induce large physical and biological perturbations, which have a feedback onto the tropical Pacific climate and ecosystem. However, the extent to which TIW-induced chlorophyll perturbations (Chl(TIW)) can influence El Nirio-Southern Oscillation (ENSO) remains unknown. Here we used a hybrid-coupled model to investigate the Chl(TIW) effect on ENSO. Two experiments are conducted, one with the Chl(TIW) effect being represented in the control run (CTRL) and other with the Chl(TIW) effect being purposely excluded by filtering out Chl(TIW) signals (FILT). Results show that the amplitude of ENSO is increased by 27% in CTRL compared to FILT. Chl(TIW) tends to modulate the penetrative solar radiation in the upper ocean, acting to weaken the intensity of TIWs. Then, the weakened TIWs lead to a reduction in the equatorward meridional heat transport and consequently less warming effect on the cold tongue. Therefore, La Nina conditions tend to be intensified, and ENSO amplitude is increased. Plain Language Summary Tropical instability waves (TIWs) are prominent cusp-like waves in the tropical Pacific and Atlantic, with the period of 20-40 days and wavelength of 600-1,000 km. TIWs can induce large perturbations in chlorophyll (Chl(TIW)) and sea surface temperature. Given that chlorophyll absorbs solar radiation in the upper ocean and alters the upper-ocean temperature structure, it is natural to ask the following question: Can TIW-related mesoscale biology processes likeChl(TIW) influence the tropical climate? Here we examine the Chl(TIW) effect on El Nino-Southern Oscillation (ENSO) using a coupled physics-biogeochemistry model, with the Chl(TIW) effect taken into account or not. Results suggest that the Chl(TIW) effects tend to increase ENSO amplitude by 27%. This is because the Chl(TIW) effect weakens the intensity of TIW itself, which inevitably decreases the meridional heat transport onto the equator and consequently less warming effect on the cold tongue in the eastern equatorial Pacific. As a result, La Nina conditions tend to be intensified and ENSO amplitude is increased. Our study contributes to resolving the ongoing debate on the role of biological processes in modulating ENSO amplitude (i.e., increase or decrease), and improves current understanding of ENSO modulation.
DOI	10.1029/2018GL081275
收录类别	SCI
语种	英语
资助项目	NASA Earth Sciences Program###524; Taishan Scholarship###104; NSFC-Shandong Joint Fund for Marine Science Research Centers[U1406402]###370; Strategic Priority Research Program of the Chinese Academy of Sciences[XDA19060102]###367; National Natural Science Foundation of China (NFSC)[41421005]###523; National Natural Science Foundation of China (NFSC)[41490644(41490640)]###522; National Natural Science Foundation of China (NFSC)[41690122(41690120)]###521; National Natural Science Foundation of China (NFSC)[41475101]###520; National Natural Science Foundation of China (NFSC)[41475101]; National Natural Science Foundation of China (NFSC)[41690122(41690120)]; National Natural Science Foundation of China (NFSC)[41490644(41490640)]; National Natural Science Foundation of China (NFSC)[41421005]; Strategic Priority Research Program of the Chinese Academy of Sciences[XDA19060102]; NSFC-Shandong Joint Fund for Marine Science Research Centers[U1406402]; Taishan Scholarship; NASA Earth Sciences Program
WOS研究方向	Geology
WOS类目	Geosciences, Multidisciplinary
WOS记录号	WOS:000458607400040
出版者	AMER GEOPHYSICAL UNION
引用统计	被引频次：14[WOS] [WOS记录] [WOS相关记录]
文献类型	期刊论文
条目标识符	http://ir.qdio.ac.cn/handle/337002/155598
专题	海洋环流与波动重点实验室
通讯作者	Zhang, Rong-Hua
作者单位	1.Chinese Acad Sci, Inst Oceanol, CAS Key Lab Ocean Circulat & Waves, Qingdao, Peoples R China 2.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing, Peoples R China 3.Pilot Natl Lab Marine Sci & Technol, Qingdao, Peoples R China 4.Chinese Acad Sci, Ctr Ocean Mega Sci, Qingdao, Peoples R China 5.Beijing Normal Univ, Joint Ctr Global Change Studies, Coll Global Change & Earth Syst Sci, Beijing, Peoples R China
第一作者单位	中国科学院海洋研究所
通讯作者单位	中国科学院海洋研究所
推荐引用方式 GB/T 7714	Tian, Feng,Zhang, Rong-Hua,Wang, Xiujun. A Positive Feedback Onto ENSO Due to Tropical Instability Wave (TIW)-Induced Chlorophyoll Effects in the Pacific[J]. GEOPHYSICAL RESEARCH LETTERS,2019,46(2):889-897.
APA	Tian, Feng,Zhang, Rong-Hua,&Wang, Xiujun.(2019).A Positive Feedback Onto ENSO Due to Tropical Instability Wave (TIW)-Induced Chlorophyoll Effects in the Pacific.GEOPHYSICAL RESEARCH LETTERS,46(2),889-897.
MLA	Tian, Feng,et al."A Positive Feedback Onto ENSO Due to Tropical Instability Wave (TIW)-Induced Chlorophyoll Effects in the Pacific".GEOPHYSICAL RESEARCH LETTERS 46.2(2019):889-897.

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