Lei Zhou
Shanghai Jiao Tong University
56 Papers
251 Citations
Lei Zhou is an academic researcher from Shanghai Jiao Tong University. The author has contributed to research in topics: Madden–Julian oscillation & Monsoon. The author has an hindex of 17, co-authored 53 publications. Previous affiliations of Lei Zhou include University of Maryland, College Park & Ontario Ministry of Natural Resources.
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Papers
Strong influence of westerly wind bursts on El Niño diversity
Dake Chen,Tao Lian,Congbin Fu,Mark A. Cane,Youmin Tang,Raghu Murtugudde,Xunshu Song,Qiaoyan Wu,Lei Zhou +8 more
TL;DR: In this paper, an overview of existing work along with a fuzzy clustering analysis and simulations suggest that the asymmetry, irregularity and extremes of El Nino result from westerly wind bursts.
329
Upper ocean response to typhoon Kalmaegi (2014)
TL;DR: In this paper, a model-based heat budget analysis suggests that vertical mixing was mainly responsible for the surface cooling and subsurface warming, while upwelling was the cause of cooling from below.
171
Regional Simulation of the October and November MJO Events Observed during the CINDY/DYNAMO Field Campaign at Gray Zone Resolution
TL;DR: In this paper, the authors investigated the October and November MJO events observed during the Cooperative Indian Ocean Experiment on Intraseasonal Variability in the Year 2011 (CINDY)/Dynamics of the MJO field campaign through cloud-permitting numerical simulations.
Improved Madden–Julian Oscillations with Improved Physics: The Impact of Modified Convection Parameterizations
TL;DR: In this paper, two modifications are made to the deep convection parameterization in the NCAR Community Climate System Model, version 3 (CCSM3): a dilute plume approximation and an implementation of the convective momentum transport (CMT).
55
Dynamics of the Intraseasonal Oscillations in the Indian Ocean South Equatorial Current
TL;DR: In this article, the spatial and temporal features of intraseasonal oscillations in the southwestern Indian Ocean are studied by analyzing model simulations for the Indo-Pacific region, and the authors show that the first baroclinic mode dominates during most of the year, but during boreal winter and spring the second mode contributes significantly and often equally.