Leilei Jiang scite author profile

The El Niño-Southern Oscillation (ENSO) is an inherently unstable climatic oscillation of the tropical Pacific oceanic-atmospheric system between positive (El Niño) and negative (La Niña) phases with a periodicity of 2 to 8 years (Timmermann et al., 2018;Wang & Fiedler, 2006). The impacts of ENSO activity can be transmitted worldwide through atmospheric teleconnections, significantly altering global redistribution of heat and moisture fluxes (

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Microbiome community and complexity indicate environmental gradient acclimatisation and potential microbial interaction of endemic coral holobionts in the South China Sea

Chen

Liao

et al. 2021

Science of The Total Environment

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Dispersal, genetic variation, and symbiont interaction network of heat-tolerant endosymbiont Durusdinium trenchii: Insights into the adaptive potential of coral to climate change

Chen

Qin

et al. 2020

Science of The Total Environment

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Coral perspective on temperature seasonality and interannual variability in the northern South China Sea during the Roman Warm Period

Jiang

Han

et al. 2021

Global and Planetary Change

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Modulation of East Asian monsoon strength by ENSO during the warm periods of the late Holocene: Evidence from Porites corals in the northern South China Sea

Jiang

Tao

et al. 2023

Global and Planetary Change

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Leilei Jiang

ENSO Variability During the Medieval Climate Anomaly as Recorded by Porites Corals From the Northern South China Sea

Microbiome community and complexity indicate environmental gradient acclimatisation and potential microbial interaction of endemic coral holobionts in the South China Sea

Dispersal, genetic variation, and symbiont interaction network of heat-tolerant endosymbiont Durusdinium trenchii: Insights into the adaptive potential of coral to climate change

Coral perspective on temperature seasonality and interannual variability in the northern South China Sea during the Roman Warm Period

Modulation of East Asian monsoon strength by ENSO during the warm periods of the late Holocene: Evidence from Porites corals in the northern South China Sea

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