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DOI10.1007/s00382-019-04844-8
Observed structural relationships between ocean chlorophyll variability and its heating effects on the ENSO
Zhang R.-H.; Tian F.; Zhi H.; Kang X.
发表日期2019
ISSN0930-7575
起始页码5165
结束页码5186
卷号53期号:2020-09-10
英文摘要Ocean chlorophyll (Chl)-induced heating can affect the climate system through the penetration of solar radiation in the upper ocean. Currently, the ocean biology-induced heating (OBH) feedback effects on the climate in the tropical Pacific are still not well understood, and the mechanisms regarding how SST is modulated remain elusive. In this paper, chlorophyll (Chl) data from satellites are combined with physical fields from Argo profiles to estimate OBH-related fields, including the penetration depth (Hp) and the ocean mixed-layer (ML) depth (Hm). In addition, some directly related heating terms with Hm and Hp are diagnosed, including the absorbed solar radiation component within the ML (denoted as Qabs), the rate of ML temperature changes that are directly induced by Qabs (denoted as Rsr = Qabs/(ρ0CpHm)), and the portion of solar radiation that penetrates through the bottom of the ML (denoted as Qpen). The structural relationships between these related fields are examined to illustrate how these heating terms are affected by Hp and Hm. The extent to which Rsr and Qpen are modulated by Hp is strikingly different during ENSO cycles. In the western-central equatorial Pacific, inter-annual variations in Hp tend to be out of phase with those in Hm. A decrease (increase) in Qabs from a positive (negative) Hp anomaly during El Niño (La Niña) tends to be offset by a negative (positive) Hm anomaly. Thus, Rsr is not closely related with Hp, even though Qabs is highly correlated with Hp, indicating that the direct thermal effect through Qabs is not a dominant factor that affects the SST. In contrast, the inter-annual variability of Qpen in the region is significantly enhanced by that of Hp, with their high positive correlation. The Hp-induced differential heating in the ML and subsurface layers from the Qpen and Qabs terms modifies the thermal contrast, stratification and vertical mixing, which represent a dominant indirect ocean dynamical effect on the SST. The revealed relationships between these related fields provide an observational basis for gaining structural insights into the OBH feedback effects and validating model simulations in the tropical Pacific. © 2019, Springer-Verlag GmbH Germany, part of Springer Nature.
英文关键词Chlorophyll variability; ENSO modulations; Ocean biology-induced heating; Satellite and Argo data; The penetration depth and mixed layer depth
语种英语
scopus关键词air-sea interaction; annual variation; Argo; chlorophyll; El Nino-Southern Oscillation; mixed layer; satellite data; sea surface temperature; solar radiation
来源期刊Climate Dynamics
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/145924
作者单位CAS Key Laboratory of Ocean Circulation and Waves, Institute of Oceanology, Chinese Academy of Sciences, Qingdao, 266071, China; Center for Ocean Mega-Science, Chinese Academy of Sciences, Qingdao, 266071, China; Center for Excellence in Quaternary Science and Global Change, Chinese Academy of Sciences, Xi’an, 710061, China; Qingdao National Laboratory for Marine Science and Technology, Qingdao, 266237, China; University of Chinese Academy of Sciences, Beijing, 10029, China; College of Atmospheric Sciences, Nanjing University of Information Science and Technology, Nanjing, 210044, China; College of Air Traffic Management, Civil Aviation Flight University of China, Guanghan, 618307, China
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Zhang R.-H.,Tian F.,Zhi H.,et al. Observed structural relationships between ocean chlorophyll variability and its heating effects on the ENSO[J],2019,53(2020-09-10).
APA Zhang R.-H.,Tian F.,Zhi H.,&Kang X..(2019).Observed structural relationships between ocean chlorophyll variability and its heating effects on the ENSO.Climate Dynamics,53(2020-09-10).
MLA Zhang R.-H.,et al."Observed structural relationships between ocean chlorophyll variability and its heating effects on the ENSO".Climate Dynamics 53.2020-09-10(2019).
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