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中国科学院青藏高原研究所导师教师师资介绍简介-杨晓新

本站小编 Free考研考试/2020-06-02

姓名:
杨晓新 性别:

学历:
博士 专家类别:
副研究员 
电话:
010-8409 7123 传真:

电子邮件:
xxy@itpcas.ac.cn 个人主页:

通讯地址:
北京市朝阳区林萃路16号院3号楼100101


简历:
2004.6 进入中科院青藏高原研究所,担任研究实习员二级
2005.9-2010.7 直博研究生 中科院青藏高原研究所
2007.3-2007.7, 美国俄亥俄州立大学伯德极地气候研究中心,访问****,合作者:Lonnie G. Thompson
2010.7-2012.6 助研中科院青藏高原研究所
2011.11-2011.12,美国圣地亚哥州立大学,数学系,访问****,合作者: Samuel S.P.Shen
2012.7-今 副研究员 中科院青藏高原研究所
2015/11-2016/10,美国俄亥俄州立大学伯德极地气候研究中心,访问****,合作者:Lonnie G. Thompson和Ellen Mosley-Thompson


研究方向:
水体中的稳定同位素与大气环流


职务:


社会任职:


承担项目:
国家自然科学基金委常规面上项目,**, 通过降水和冰芯稳定同位素揭示ENSO对"第三极"南北部水汽来源的影响,2016/01-2019/12,80万元,主持
科技部国际科技合作与交流专项, 2015DFG22720, 通过水体稳定同位素与冰川物质平衡研究第三极地区环境,2015/04-2018/03,60万元,参加
中国科学院战略性先导科技专项(B类),XDB**,现代高原的地表各圈层相互作用子课题的专题项目“第三极地区现代水体稳定同位素的特征”,2012/09-2017/09,80万元,主持
教育部留学基金委访问****,2015/11-2016/10,美国
中国科学院青年创新促进会会员,2013/01-2016/12,40万元,已结题,主持
国家自然科学基金委青年基金,**,利用降水中稳定同位素研究孟加拉湾和南中国海季风的爆发过程与季节转换特征,2012/01-2014/12,28万元,已结题,主持
国家自然科学基金重点项目,**,中国河水与降水稳定同位素观测研究(CNIRP),2009/01-2012/12,185万元,已结题,参加


获奖及荣誉:


代表论著:
Yang, X.X., Yao, T.D, Deji, Zhao, H.B., and Xu, B.Q. Possible ENSO influences on the northwestern Tibetan Plateau revealed from annually resolved ice core records. Journal of Geophysical Research: Atmospheres, 2018, doi: 10.1002/2017JD027755.

Yang, X.X., Davis, M. E., Acharya, S., Yao, T.D. Asian Monsoon variations revealed from stable isotopes in precipitation. Climate Dynamics, 2017, doi:10.1007/s00382-017-4011-4.

Deji, Yao, TD, Yang, X.X., Xu, BQ, Zhao, HB, Li, JL, Li, Z, Wu, GJ, Yao, P, You, C, Zhu, ML, Wang, M, Qu, DM, Li, QL.Warming and wetting climate during last century revealed by an ice core in northwest Tibetan Plateau. Palaeogeography, Palaeoclimatology, Palaeoecology, 2017,487,270-277.

Yang, X.X., Yao, T., Different sub-monsoon signals in stable oxygen isotope in daily precipitation to the northeast of the Tibetan Plateau. Tellus B, 2016,68, 27922.

Yang, X.X., Yao, T., Joswiak, D., and Yao, P. Integration of Tibetan Plateau ice core temperature records and the influence of atmospheric circulation on isotopic signals in the past century, Quaternary Research, 2014,81(3): 520-530.

Yao, TD,V. Masson-Delmotte, Gao, J, Yu, WS, Yang, XX, C. Risi, C. Sturm, M. Werner,Zhao, HB, He, Y. A review of climatic controls on delta O-18 in precipitation over the Tibetan Plateau: observations and simulations. Reviews of Geophysics, 2013, 51(4), doi: 10.1002/rog.20023.

Ren, W,Yao, TD,Yang, XX,Daniel Joswiak.Implications of variations in delta O-18 and delta D in precipitation at Madoi in the eastern Tibetan Plateau. Quaternary International,2013. 313, 56-61.

Yao, T.D., Thompson, L., Yang, W., Yu, WS, Gao, Y, Guo, XJ, Yang, XX, Duan, KQ Zhao, HB, Xu, BQ. Different glacier status with atmospheric circulations in Tibetan Plateau and surroundings. Nature Climate Change, 2012, 2(9), 663-667.

Wang, WC, Yang, XX, Yao, TD. Evaluation of ASTER GDEM and SRTM and their suitability in hydraulic modelling of a glacial lake outburst flood in southeast Tibet. Hydrological Processes,2012, 26(2), 213-225.

Yang, X.X, T. Yao, W. Yang, B. Xu, Y. He, and D. Qu, 2012: Isotopic signal of earlier summer monsoon onset in the Bay of Bengal, J Climate, 25:2509-2516.
Yang, X.X., B. Xu, W. Yang, and D. Qu, 2012: The Indian monsoonal influence on altitude effect of d18O in surface water on southeast Tibetan Plateau. Science China-Earth Sciences, 55(3):438-445.
Yang, X.X., T. Yao, W. Yang, W. Yu, and D. Qu, 2011: Co-existence of temperature and amount effects on precipitation d18O in the Asian monsoon region. Geophys. Res. Lett., 38, L21809. doi:10.1029/2011GL049353.
Yang, X.X., Xu, B.Q., Yang, W., Qu, D.M., and Lin, P.-N., 2009. Study of altitudinal lapse rates of d18O in precipitation/river water with seasons on the southeast Tibetan Plateau. Chinese Sci. Bull., 54: 2742-2750.
Yao, T.D., Zhou, H., and Yang, X.X., 2009. Indian monsoon influences altitude effect of d 18O in precipitation/river water on the Tibetan Plateau. Chinese Sci. Bull., 54: 2724-2731.
Yao, Tandong, K.Duan, B.Xu, N.Wang, X.Guo, X. Yang, 2008. Precipitation record since AD 1600 from ice cores on the central Tibetan Plateau, Climate of the Past, 4:175-180.

Yao Tandong, Guo Xuejun, L.G. Thompson, Duan Keqin, Wang Ninglian, Pu Jianchen, Xu Baiqing, Yang Xiaoxin, and Sun Weizhen, 2006. δ18O record and temperature change over the past 100 years in ice cores on the Tibetan Plateau. Science in China (Ser. D), 49(1):1-9.


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