Large-scale ocean circulation; Ocean-atmosphere interaction

1999-2002  Ph. D, Department of Physical Oceanography, Ocean University of Qingdao

1995-1998 Master, Department of Physical Oceanography, Ocean University of Qingdao

1991-1995 Bachelor, Department of Physical Oceanography, Ocean University of Qingdao.

2012-Now, Senior scientist in South China Sea Institute of Oceanology, CAS, Guangzhou, China

2007-2012, Research assoicate, Institut für Meerskunde, Universität Hamburg, Germany

2006-2007, post-doctorate, IFM-GEOMAR, Kiel, Germany

2005-2006, visiting scientist, Atlantic Oceanographic and Meteorological Laboratory (AOML), National Oceanic and Atmospheric Administration (NOAA), US

1998-2005, Research Associate, South China Sea Institute of Oceanology, Chinese Academy of Sciences (CAS), China

2000.9, Visiting scientist in Lund University, Sweden

[1]. Liu D, Zhu J, Shu Y*, Wang D, W Wang, Cai S. Model-based assessment of a Northwestern Tropical Pacific moored array to monitor intraseasonal variability [J]. Ocean Modelling, 2018, 126:1-12.

[2]. Liu D, Zhu J, Shu Y*, Wang D, W Wang, Yan C, Zhou W. Targeted Observation Analysis of a Northwestern Tropical Pacific Ocean Mooring Array Using an Ensemble-Based Method. Ocean Dynamic, 2018 (in press).

[3]. Xu, K., Q.L. Huang, C.Y. Tam*, W. Wang, S. Chen, and C. Zhu (2018). Roles of tropical SST patterns during two types of ENSO in modulating wintertime rainfall over southern China, Climate Dynamics., doi:10.1007/s00382-018-4170-y.

[4]. Huang, K., D. Wang, W. Wang, J. Chen, L. Chen, and G. Chen* (2018). Multi-scale variability of the tropical Indian Ocean circulation system revealed by recent observations, SCIENCE CHINA Earth Sciences，doi: 10.1007/s11430-017-9179-x.

[5]. Zhang, T., W. Wang, Q. Xie* and F. Chen (2018). Heat contribution of the Indonesian throughflow to the Indian Ocean. Acta Oceanologica Sinica (in press).

[6]. Huang, K., W. Han, D. Wang, W. Wang, Q. Xie, J. Chen, and G. Chen* (2018). Features of the Equatorial Intermediate Current associated with basin resonance in the Indian Ocean. Journal of Physical Oceanography, doi:10.1175/JPO-D-17-0238.1

[7]. Huang Ke, McPhaden Michael J, D. Wang*, W. Wang*, Q Xie, J Chen, Y Shu, Q Wang, J Li, J Yao, Vertical Propagation of Middepth Zonal Currents Associated With Surface Wind Forcing in the Equatorial Indian Ocean , J. Geophys. Res.-OCEANS, 2018.10,123(10): 7290~7307.

[8]. He Z., R. Wu, W. Wang*, Z. Wen, D. Wang, 2017: Contributions of surface heat fluxes and oceanic processes to tropical SST changes: Seasonal and regional dependence. J. Clim, doi: 10.1175/JCLI-D-16-0500.1.

[9]. Xu, K., R. X. Huang, W. Wang*, C. Zhu, and R. Lu, 2017: Thermocline Fluctuations in the Equatorial Pacific Related to the Two Types of El Niño Events, J. Clim., 30(17), 6611-6627, doi:10.1175/jcli-d-16-0291.1.

[10]. Xu K., C.-Y. Tam, C. Zhu, B. Liu, and W. Wang, 2017: CMIP5 projections of two types of El Niño and their related tropical precipitation in the 21st century, J. Clim, 30, 849-864, doi:10.1175/JCLI-D-16-0413.1.

[11]. Xu K., Congwen Zhu, W. Wang*, 2016: The cooperative impacts of the El Niño–Southern Oscillation and the Indian Ocean Dipole on the interannual variability of autumn rainfall in China, International Journal of Climatology, 36(4): 1987-1999.

[12]. Tan W., X. Wang, W. Wang, C. Wang, and J. Zuo, 2016: Different responses of sea surface temperature in the South China Sea to various El Niño events during boreal autumn. J. Climate, 29: 1127–1142, doi: 10.1175/JCLI-D-15-0338.1.

[13]. Chen G., W. Han, Y. Li, M. J. Mcphaden, J. Chen, W. Wang, D. Wang, 2017: Strong intraseasonal variability of meridional currents near 5°N in the Eastern Indian Ocean: characteristics and causes. J. Phys. Oceanogr. 47(5), doi: 10.1175/JPO-D-16-0250.1

[14]. Qin, H., R. X. Huang, W. Wang*, and H. Xue, 2016: Regulation of South China Sea throughflow by pressure difference, Journal of Geophysical Research: Oceans, n/a-n/a, doi:10.1002/2015JC011177.

[15]. He Z., R. Wu, and W. Wang, 2016: Signals of the South China Sea summer rainfall variability in the Indian Ocean. Climate Dyn., 46, 3181-3195, doi: 10.1007/s00382-015-2760-5.

[16]. Zeng L., Wang D., J. Chen, W. Wang, and R. Chen, 2016: SCSPOD14, a South China Sea physical oceanographic dataset derived from in situ measurements during 1919-2014. Sci. Data, 3, 160029, doi: 10.1038/sdata.2016.29.

[17]. Tan W., R. X. Huang, W. Wang, X. Wang, 2015: Zonal overturning circulation and heat flux induced by heaving modes in the world oceans. Acta Oceanol. Sin., 34(11), 80-91, doi:10.1007/s13131-015-0751-3.

[18]. Wang W.*, X. Zhu, Chunzai Wang, A. Köhl, 2014: Deep Meridional Overturning Circulation in the Indian Ocean and Its Relation to Indian Ocean Dipole. J. Clim, doi: http://dx.doi.org/10.1175/JCLI-D-13-00472.1.

[19]. Qin, H., G. Chen and W. Wang, et al., 2014: Validation and application of MODIS-derivedSST in the South China Sea. International Journal of Remote Sensing, 35, 11-12,DOI:10.1080/01431161.2014.916439.

[20]. Zhu, X., W. Wang*, and K. Fraedrich, 2013: Future Climate in the Tibetan Plateau from a Statistical Regional Climate Model. J. Clim., 26, 10125-10138.

[21]. Wang, W.*, A. Köhl, and D. Stammer, 2012: The deep meridional overturning circulation in the Indian Ocean inferred from the GECCO synthesis. Dynam. Atmos. Ocean, 58, 44-61.

[22]. Wang, W.*, A. Kohl, and D. Stammer, 2010: Estimates of global ocean volume transports during 1960 through 2001, Geophys. Res. Lett., 37.

[23]. T. Frisius, K. Fraedrich, X. Zhu, W. Wang, 2009: A spectral barotropic model of the wind-driven world ocean. Ocean Modelling, 30, 310-322.

[24]. Schott, F. A., L. Stramma, W. Wang, B. S. Giese, R. Zantopp, 2008: Pacific Subtropical Cell variability in the SODA 2.0.2/3 assimilation. Geophys. Res. Lett., 35, L10607, doi: 10.1029/2008GL033757.

[25]. Schott F. A., W. Wang, D. Stammer, 2007: Variability of Pacific subtropical cells in the 50-year ECCO assimilation, Geophys. Res. Lett., 34, L05604, doi:10.1029 /2006GL028478.

[26]. Wang, W., and C. Wang, 2006: Formation and decay of the spring warm pool in the South China Sea, Geophys. Res. Lett., 33, L02615, doi:10.1029/2005GL025097.

[27]. Wang C., W. Wang, D. Wang, Q. Wang, 2006: Interannual variability of the South China Sea associated with El Niño, J. Geophys. Res., 111, C03023, doi:10.1029/2005JC003333.

shallow and deep meridional overturning circulation in the Indian Ocean circulation system and its relation to air-sea interaction

2017, Chief Scientist, open cruise of Indian Ocean expedition

已指导学生

赵德平  硕士研究生  070701-物理海洋学  

黄旭媚  硕士研究生  070701-物理海洋学  

刘大年  博士研究生  070701-物理海洋学  

现指导学生

张文静  博士研究生  070701-物理海洋学  

邢会斌  博士研究生  070701-物理海洋学  

刘素敏  博士研究生  070701-物理海洋学  

房翔  硕士研究生  085229-环境工程