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郭晓军

时间:2020-09-15  来源: 文本大小:【 |  | 】  【打印

 

郭晓军 

副研究员,硕导

    

  个人简介从事泥石流形成过程和监测预警预报研究,发表学术论文40余篇,其中第一/通讯作者SCI论文11篇,主持自然科学基金青年项目和面上项目各1项,获中国科学院优秀博士论文奖 

  担任亚洲泥石流学会秘书、2020 EGU-Debris Flow专题的召集人。任Journal of HydrologyLandslidesCatenaBOEGEESJMS等多个国际期刊的审稿专家。 

  热爱野外工作,以大山为家,越艰苦越坚韧,长期坚守在青藏高原周边地区,跋山涉水,建设野外监测预警示范流域,通过高质量论文,将中国灾害现象呈现给世界。      

  招生专业:自然地理学/岩土工程    

  学习与工作经历 

  2003.09-2007.06:四川大学 水文与水资源工程工学学士 

  2007.09-2010.06:中国科学院大学 防灾减灾工程与防护工程工学硕士 

  2012.09-2016.06:中国科学院大学 岩土工程工学博士 

  2010.07-至今: 中国科学院、水利部成都山地灾害与环境研究所  

  研究方向及科研工作 

    研究方向:1)泥石流形成机理和过程;2)泥石流监测预警和预报。 

  从事泥石流形成机理过程研究。从流域系统出发,以水文过程为主线,揭示了山区流域的降雨-水文特征; 提出了基于水文参数的泥石流形成模式; 提出了土体随机补给理论,构建了坡元补给模型; 提出了跨尺度流域泥石流汇流理论,建立泥石流形成的随机过程模型,丰富了泥石流形成机理研究体系。 

  从事泥石流监测预警研究,针对泥石流形成演进过程,提出监测预警模式,开发系列监测技术,提出基于诱发因子的泥石流预报模型,揭示了震后泥石流的时空特征和发展趋势。    

  社会任职、荣誉称号 亚洲泥石流学会秘书     

  代表性论文论著 

  [1]Guo Xiaojun*, Li Yong, Cui Peng, Yan Hua, Zhuang Jianqi. 2020. Intermittent viscous debris flow formation in Jiangjia Gully from the perspectives of hydrological processes and material supply. Journal of Hydrology, 589: 125184.  

  [2]Guo Xiaojun, Cui Peng*, Li Yong, Ma Li, Ge Yonggang, William B. Mahoney. 2016. Intensity-duration threshold of rainfall-triggered debris flows in the Wenchuan Earthquake affected area, China. Geomorphology, 253: 208-216. 

  [3]Guo Xiaojun, Cui Peng*, Li Yong, Zou Qiang, Kong Yingde. 2016. The formation and development of debris flows in large watersheds after the 2008 Wenchuan Earthquake. Landslides, 13(1): 116-125. 

  [4]Guo Xiaojun, Cui Peng*, Li Yong, Zhang Jianqiang, Ma Li, William B. Mahoney. 2016. Spatial distribution of debris flows and responsible rainfall threshold in the Wenchuan earthquake area. Landslides, 13(5): 1215-1229. 

  [5]Guo Xiaojun*, Cui Peng, Li Yong, Fan Jianglin, Yan Yan, Ge Yonggang. 2016. Temporal differentiation of rainfall thresholds for debris flows in Wenchuan earthquake-affected areas, Environmental Earth Sciences, 75(2): 109-121. 

  [6]Guo Xiaojun, Cui Peng, Lorenzo Marchi, Ge Yonggang*. 2017. Characteristics of rainfall responsible for debris flows in Wenchuan Earthquake area. Environmental Earth Sciences, 2017, 76: 596-605. 

  [7]Guo Xiaojun, Li Yong*, Cui Peng, Zhao Wanyu, Jiang Xingyuan, Yan Yan. 2016. Discontinuous slope failures and pore-water pressure variation. Journal of Mountain Science, 13(1): 116-125. 

  [8]Guo Xiaojun; Cui Peng*, Li Yong, Liu Jinfeng; Ge Yonggang, Wang Cide. 2019. Evaluation of a traditional method for peak flow discharge estimation for floods in the Wenchuan Earthquake area, Sichuan Province, China. Journal of Mountain Science, 16(3): 641-656. 

  [9] Cui Peng, Guo Xiaojun*, Yan Yan, Li Yong, Ge Yonggang. 2018. Real-time observation of an active debris flow watershed in the Wenchuan Earthquake area. Geomorphology, 321: 153-166. 

  [10] Xuanmei Fan*, Gianvito Scaringi, Guillem Domènech, Fan Yang, Xiaojun Guo*, Lanxin Dai, Chaoyang He, Qiang Xu*, Runqiu Huang. 2019. Two multi-temporal datasets that track the enhanced landsliding after the 2008 Wenchuan earthquake. Earth Syst. Sci. Data, 11: 35-55.  

    

  联系方式 

  通讯方式:610041,成都市人民南路49号,中国科学院水利部成都山地灾害与环境研究所      

  Email:aaronguo@imde.ac.cn 

    

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