王闪闪，女，博士，兰州大学青年研究员，硕士导师。2015年获得兰州大学气象学博士学位。2015-2019年工作于中国气象局兰州干旱气象研究所，期间赴中科院大气物理研究所学术访问1年，现工作于兰州大学大气科学学院。主要从事干旱半干旱地区的气候变化、极端天气气候事件检测归因、干旱成因分析及预测等方面的研究工作，在BAMS、Scientific Report、Hydrol. Earth Syst. Sci.、International Journal of Climatology、Climate Dynamics等期刊上发表SCI论文10余篇。
联系方式：
E-mail: wangss@lzu.edu.cn
研究方向：
干旱半干旱区气候变化、海气相互作用、极端天气气候事件归因
代表性论文：
[1]Wang S, Yuan X, Wu RG. Attribution of the persistent spring-summer hot and dry extremes over Northeast China in 2017. Bulletin of the American Meteorological Society, 2018, DOI:10.1175/BAMS-D-18-0120.1, S86-S89.
[2]Wang S, Yuan X. Extending seasonal predictability of Yangtze River summer floods. Hydrol. Earth Syst. Sci., 2018, 22, 4201-4211, https://doi.org/10.5194/hess-22-4201-2018.
[3]Wang S, Yuan X, Li YH. Does a strong El Ni?o imply a higher predictability of extreme drought? Scientific Report, 2017, 7, 40741, doi: 10.1038/srep40741.
[4]Wang S, Huang J., He Y. and Guan Y: Combined effects of the Pacific Decadal Oscillation and El Ni?o-Southern Oscillation on Global Land Dry–Wet Changes. Scientific Report, 4, doi:10.1038/srep06651, 2014.
[5]Yuan X, Wang S, Hu Z-Z. Do Climate Change And El Ni?o Increase Likelihood Of Yangtze River Extreme Rainfall? Bulletin of the American Meteorological Society, 2017, 98, doi:10.1175/BAMS-D-17-0089.
[6]Chen X, Wang S, Hu ZY, et al. Spatiotemporal characteristics of seasonal precipitation and their relationships with ENSO in Central Asia during 1901–2013. J. Geogr. Sci., 2018, 28(9), 1341-1368. DOI: https://doi.org/10.1007/s11442-018-1529-2.
[7]Wang, S., Guan Y., Li Z., Chao Y. and Huang J: Variable characteristics of the wintertime net heat flux along the Kuroshio system and its association with climate in China. Int. J. Climatol., 2015, 35:1180-1191.
[8]Veettil B. K., S. Wang, J. C. Simoes, et al. Regional climate forcing and topographic influence on glacier shrinkage: eastern cordilleras of Peru. Int. J. Climatol.,2017, DOI: 10.1002/joc.5226.
[9]Huang J, Ji M, Xie Y, Wang S, He Y., Ran J. Global semi-arid climate change over last 60 years, Climate Dynamics, doi:10.1007/s00382-015-2636-8, 2015.