陈兆云教师个人简介

姓名：       陈兆云    

性别：          男

出生日期： 1985/4/2

职务：

学术兼职：

社会兼职：

电话：

手机：

传真：

Email:     chenzy@stu.edu.cn

学历简介：

博士：2009–2014，美国特拉华大学和厦门大学联培双博士学位，物理海洋专业；

硕士：2007–2009，厦门大学，物理海洋专业；

本科：2003–2007，武汉理工大学，环境科学专业。

工作经历：

教授：2018–至今，汕头大学

特聘研究员：2016–2018，中山大学；

博士后：2014–2016，香港中文大学。

主讲课程：

《物理海洋学》、《海洋数据处理与可视化》、《海洋科学导论》

主要研究兴趣：

研究方向：近岸上升流与冲淡水动力

研究方法：水动力数值模拟；生态动力数值模拟；深度学习遥感图像识别

承担项目：

国家自然科学基金－面上项目，42276013，层化对近岸峡谷处风生上升流动力的调控作用：以台湾海峡为例，2023–2026，54万，主持。

国家自然科学基金－青年科学基金项目，41706001，夏季南海东北部上升流变化对珠江冲淡水动力作用及机制研究，2018–2020，25万，主持。

研究成果：

从业十余载，虽未见大成，然亦有所得，勉力为之，自得其乐，概言：

1、 新现象：(1)宁德外海上升流核心 (Chen et al., 2014); (2)珠江冲淡水丝状结构 (filaments; Chen et al., 2017) ; (3)冲淡水两侧次级上升流环流结构 (Chen et al., 2019) ; (4)冲淡水两侧湍动能生成率不对称结构 (Deng et al., 2023)。

2、现象机理解释：(1)为什么在峡谷和岬角下游出现上升流强化现象 (Chen et al., 2014) ？ (2)珠江冲淡水为何会脱离孤立低盐水团 (Chen et al., 2016) ？ (3)当粤东上升流由弱变强时，珠江冲淡水路径为何从浅滩上升流以西转向以东海域(Chen et al., 2017)？ (4)为什么珠江冲淡水呈现射流状结构(Chen et al., 2017)？ (5) 为什么在冲淡水两侧形成次级上升流环流结构(Chen et al., 2019)？ (6) 为什么冲淡水两侧湍动能生成率呈现不对称结构(Deng et al., 2023)？

3、新观点：(1)台湾海峡沿岸流（含台湾暖流）的流态存在争议。我们指出，黑潮造成的北向压强梯度力与风是沿岸流的共同源动力，两者通过竞争或者协同作用调控跨岸地转调整，其与风生流共同决定沿岸流的结构，揭示了沿岸流三种流态的形成机制，为中国近海另外两大海流的研究提供了新的思路和参考(Zong et al., 2024)。

 (2)受Zhang & Lentz (2017)工作启发，我们提出，峡谷处激发的近岸陷波造成的水位变化是改变峡谷处压强梯度力和上升流强度的源动力，避免了传统从动量平衡出发进行机理解释时所陷入的“鸡生蛋、蛋生鸡”的困境。同时，阐明了在层化条件下峡谷处上升流进一步强化的动力机制(Chen et al., 2024)。

代表性论文：

[ 9 ] Qiang Lian, Haiyuan Lin, Yawen Huang, Shuwen Zhang, Zhaoyun Chen* (2024); Monthly and Interannual Variations in Upwelling and Chlorophyll off the Vietnam Coast in Summer Based on Deep Learning; Journal of Geophysical Research-Oceans, 129, e2024JC021362.

[ 8 ] Zhaoyun Chen*, Chaohan Li, Shuwen Zhang, Yuwu Jiang, Aijun Wang (2024); Effects of Stratification on Wind-Driven Upwelling Over a Coastal Valley; Journal of Geophysical Research-Oceans, 129, e2024JC021063.

[ 7 ] Xiaolong Zong, Zhong Sheng, Shuwen Zhang, Aijun Wang, Fangjing Deng, Qiang Wang, Zhaoyun Chen* (2024); Dynamics of Alongshore Current in the Taiwan Strait: A Perspective on the Southward Kuroshio Branch in Winter; Limnology and Oceanography, 69, 1734–1745.

[ 6 ] Fangjing Deng, Shuwen Zhang, Wenping Gong, Xiaolong Zong, Zhaoyun Chen*, (2023); Turbulent Kinetic Energy Production in a Far-Field River Plume Under Upwelling-Favorable Winds; Journal of Geophysical Research-Oceans, 128,  e2021JC018176.

[ 5 ] Wenping Gong, Lianghong Chen, Heng Zhang, Lirong Yuan, Zhaoyun Chen*, (2020); Plume Dynamics of a Lateral River Tributary Influenced by River Discharge From the Estuary Head; Journal of Geophysical Research-Oceans, 125, e2019JC015580.

[ 4 ] Zhaoyun Chen, Yuwu Jiang, Jia Wang, Wenping Gong*, (2019); Influence of a River Plume on Coastal Upwelling Dynamics: Importance of Stratification; Journal  of Physical Oceanography, 49, 2345–2363.

[ 3 ] Zhaoyun Chen, Yuwu Jiang, James T. Liu, Wenping Gong*, (2017); Development of Upwelling on Pathway and Freshwater Transport of Pearl River plume in Northeastern South China Sea; Journal of Geophysical Research-Oceans, 122, 6090–6109.

[ 2 ] Zhaoyun Chen, Jiayi Pan*, Yuwu Jiang (2016); Role of Pulsed Winds on Detachment of Low Salinity Water from the Pearl River Plume: Upwelling and Mixing Processes; Journal of Geophysical Research-Oceans, 121, 2769–2788.

[ 1 ] Zhaoyun Chen, Xiao-Hai Yan, Yuwu Jiang* (2014); Coastal Cape and Canyon Effects on Wind-driven Upwelling in Northern Taiwan Strait; Journal of Geophysical Research-Oceans, 119, 4605–4625.

主流期刊论文：

[ 8 ] Xiaolong Zong, Xuan Cheng, Shuwen Zhang, Qiang Lian, Fangjing Deng, Zhaoyun Chen* (2024); Tidal Effects on Dynamics and Freshwater Transport of a Medium-Scale River Plume with Multiple Outlets; Ocean Modelling, 188, 102338.

[ 7 ] Fangjing Deng, Feiyu Jia, Rui Shi, Shuwen Zhang, Qiang Lian, Xiaolong Zong, Zhaoyun Chen* (2024); Influence of Stratification and Wind Forcing on the Dynamics of Lagrangian Residual Velocity in a Periodically Stratified Estuary; Ocean Science, 20, 499–519.

[ 6 ] Wenping Gong, Zhongyuan Lin, Yunzhen Chen, Zhaoyun Chen*, Jian Shen, Heng Zhang* (2018); Effect of Waves on the Dispersal of the Pearl River Plume in Winter; Journal of Marine Systems, 186, 47–67.

[ 5 ] Wenping Gong, Yunzhen Chen, Heng Zhang, Zhaoyun Chen* (2018); Effects of Wave–Current Interaction on Salt Intrusion During a Typhoon Event in a Highly Stratified Estuary; Estuaries and Coasts, 41, 1904–1923.

[ 4 ] Zhaoyun Chen, Wenping Gong, Huayang Cai, Yunzhen Chen, Heng Zhang* (2017); Dispersal of the Pearl River Plume over Continental Shelf in Summer; Estuarine, Coastal and Shelf Science, 194, 252–262.

[ 3 ] Zhaoyun Chen, Jiayi Pan*, Yuwu Jiang, Hui Lin (2017); Far-reaching Transport of Pearl River Plume Water by Upwelling Jet in the Northeastern South China Sea; Journal of Marine Systems, 173, 60–69.

[ 2 ] Zhaoyun Chen, Xiao-Hai Yan, Yuwu Jiang*, Lide Jiang (2013); Roles of Shelf Slope and Wind on Upwelling: A Case Study off East And West Coasts of the US; Ocean Modelling, 69, 136–145.

[ 1 ] Zhaoyun Chen, Xiao-Hai Yan, Young-Heon Jo, Lide Jiang, Yuwu Jiang* (2012); A Study of Benguela Upwelling System using Different Upwelling Indices Derived from Remotely Sensed Data; Continental Shelf Research, 45, 27–33.