Min Wu

Guiyang College of Traditional Chinese Medicine

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Zhenliang Yin

Jiangxi Agricultural University

Li Qi

Xi'an Railway Survey and Design Institute

Derek Hao

RMIT University

Pan Wu

Guizhou University

Xiaohu Wen

Northwest Institute of Eco-Environment and Resources

Zhang Shui

China University of Petroleum, Beijing

Linna Wu

Institute of Plant Protection

Ling Li

Institute of Microelectronics

Yang Tang

Hong Kong Polytechnic University

Jan Adamowski

McGill University

Cooperative Institutions

Chinese Academy of Sciences

Northwest Institute of Eco-Environment and Resources

University of Chinese Academy of Sciences

Ministry of Natural Resources

Guizhou University

Gansu Qilian Mountains Water Conservation Forest Research Institute

Gansu Academy of Sciences

Institute of Geographic Sciences and Natural Resources Research

Research Center for Eco-Environmental Sciences

Tsinghua University

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Geochemical behaviors of antimony in mining-affected water environment (Southwest China)

Environmental Geochemistry and Health (2019)

Ling Li Han Tu Zhang Shui Linna Wu Min Wu

10.1007/s10653-019-00285-8

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Citations (29)

Erratum to ‘Spatio-temporal variation of reference evapotranspiration in northwest China based on CORDEX-EA’ [Atmos. Res. 238 (2020) 104868]

Atmospheric Research (2021)

Linshan Yang Qi Feng Jan Adamowski Zhenliang Yin Xiaohu Wen

Variation (astronomy)

10.1016/j.atmosres.2020.105425

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Citations (2)

Distinct Evolution of Sea Surface Temperature over the Cold Tongue Region in South China Sea during Various El Niño Events

Atmosphere (2021)

Min Wu Li Qi

This study investigates the evolution of the sea surface temperature (SST) over the cold tongue (CT) region in the central South China Sea (SCS) during various El Niño events. A significant and distinct double-peak warming evolution can occur during EP El Niño and CP El Niño events, with the former being more remarkable and robust than the latter. Further analyses show that the weak and insignificant CT SST anomaly in CP El Niño events is influenced by some CP El Niño events in which the warm sea surface temperature anomaly (SSTA) is located west of 175° E (WCP El Niño). The response of CT SSTA mainly depends on the warm SSTA location of CP El Niño. The different corresponding mechanisms in winter, spring and summer are discussed respectively in this work. Further analysis reveals that the weak and insignificant SST anomaly over the CT region in CP El Niño events is caused by the faint SSTA response during the WCP El Niño events. The results of this study call attention to the response of the SCS climate in both atmosphere and ocean to the diversity of ENSO, especially the CP El Niño.

Anomaly (physics)

Surface air temperature

10.3390/atmos12121689

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