段安民，研究员，教授，博士生导师，国家杰出青年基金获得者。
Prof. DUAN Anmin, Ph.D tutor, the National Science Fund for Distinguished Young Scholars

个人简历    CV
2013夏威夷国际海洋科学年会.jpg

研究方向：青藏高原气候动力学、亚洲季风，海-陆-气相互作用。

我的主要研究兴趣是从地球气候系统海-陆-气相互作用的视角出发，认识青藏高原对亚洲季风形成和变异的影响。冬季青藏高原大地形对西风气流的阻挡和抬升作用以及夏季其强大的热力作用是北半球大气环流系统的重要影响因子，亦是全球最强的副热带冬季风和夏季风之所以出现在东亚地区的根本原因。我的研究工作致力于回答如下科学问题：（1）为什么青藏高原对亚洲季风的形成和不同时间尺度变率产生如此重要的影响？（2）什么原因造成了青藏高原地表和大气热源（汇）的时空演变？（3）哪些类型的亚洲季风空间格局和时间变率直接受制于青藏高原的影响？（4）如何考虑青藏高原与大尺度海-气自然变率的协同效应，从而为亚洲季风预测提供有用的信息。我的研究方法主要是多源资料分析和数值模拟结合，模式工具包括全球和区域尺度的大气、海洋和海-气耦合模式。研究成果详见发表论文和承担项目。


Research Interest: Tibetan Plateau climate dynamics, Asian monsoon, land-air-sea interaction

My research focuses mainly on the impact of the Tibetan Plateau (TP) on the Asian monsoon formation, variability, and change in the framework of the global land-air-sea coupled system. The TP importance for climate is evident from the facts that both its mechanical forcing in winter and thermal forcing in summer exert significant influence on the atmospheric general circulation. This is the reason why the strongest subtropical winter and summer monsoon on earth appear in East Asia.My research contributes to answering such fundamental questions as why TP is so important for the formation and multi-scale variation of Asian monsoon, what determines the spatial and temporalevolution of the land and atmospheric heat source/sink over TP, how preferred patterns and variability of Asia monsoon are connected with the TP forcing, and how predictable climate in the Asian monsoon region can be determined by the signal originated from TP, together with the remote large-scale atmospheric and oceanic natural variability.I carry out both diagnostic and modeling studies, using observations and numerical models of the global and regional atmosphere, ocean,and their coupled system. For more information, please see the linkage of publications and projects.


Potential regulation on the climatic effect of Tibetan Plateau heating by tropical air-sea coupling in regional models[PDF]
Tibetan Plateau heating as a driver of monsoon rainfall variability in Pakistan[PDF]
Spatiotemporal distributions of cloud parameters and their response to meteorological factors over the Tibetan Plateau during 2003–2015 based on MODIS data[PDF]
Surface energy budget diagnosis reveals possible mechanism for the different warming rate among Earth’s three poles in recent decades[PDF]
Atmospheric heat sinks over the western Tibetan Plateau associated with snow depth in late spring[PDF]
Response of the Indian Ocean to the Tibetan Plateau Thermal Forcing in Late Spring[PDF]
Revisiting the Cross-Equatorial Flows and Asian Summer Monsoon Precipitation Associated with the Maritime Continent[PDF]
Zhou T J, Wang B, Yu Y Q, et al. The FGOALS climate system model as a modeling tool for supporting climate sciences: An overview[J]. Earth and Planetary Physics, 2018, 2(4): 276-291.[PDF]
段安民, 肖志祥, 王子谦. 青藏高原冬春积雪和地表热源影响亚洲夏季风的研究进展[J]. 大气科学, 2018, 42(4): 755-766.[PDF]
Zhao Y, Duan A, Wu G. Interannual Variability of Late-spring Circulation and Diabatic Heating over the Tibetan Plateau Associated with Indian Ocean Forcing[J]. Advances in Atmospheric Sciences, 2018, 35(8): 927-941.[PDF]
Wang M, Wang J, Duan A, et al. Coupling of the quasi‐biweekly oscillation of the Tibetan Plateau summer monsoon with the Arctic Oscillation[J]. Geophysical Research Letters, 2018.[PDF]
Bao S, Letu H, Zhao J, et al. Spatiotemporal distributions of cloud parameters and their response to meteorological factors over the Tibetan Plateau during 2003–2015 based on MODIS data[J]. International Journal of Climatology.[PDF]
Duan A, Liu S, Zhao Y, et al. Atmospheric heat source/sink dataset over the Tibetan Plateau based on satellite and routine meteorological observations[J]. Big Earth Data, 2018: 1-11.[PDF]
段丽君，段安民*，胡文婷，等. 2017. 2014 年夏季青藏高原狮泉河与林芝降水低频振荡及陆—气过程日变化特征 [J]. 大气科学, 41 (4): 767–783.(第一单位 成都信息工程大学)[PDF]
谢志昂, 段安民. 2017：盛夏青藏高原热源与菲律宾海对流活动的联系. 大气科学, 41(4):811-830.[PDF]
刘森峰，段安民，2017：基于青藏高原春季感热异常信号的中国东部夏季降水统计预测模型. 气象学报, 75(6):903-916[PDF]
Wu, G. X., B. He, A. M. Duan, Y. M. Liu, and W. Yu, 2017: Formation and variation of the atmospheric heat source over the Tibetan Plateau and its climate effects. Adv. Atmos. Sci., 34(10), 1169–1184, doi: 10.1007/s00376-017-7014-5.[PDF]
Duan A*, Sun R,He J, 2017: Impact of surface sensible heating over the Tibetan Plateau on the western Pacific subtropical high: A land-air-sea interaction perspective[J]. Advances in Atmospheric Sciences, 34(2): 157-168. SCI[PDF]
Wang, Z. Q.*, A. M. Duan, S. Yang, and K. Ullah, 2017: Atmospheric moisture budget and its regulation on the variability of summer precipitation over the Tibetan Plateau. J. Geophys. Res. Atmos., 122, 614–630, doi: 10.1002/2016JD025515. （第一单位 中山大学）[PDF]
Hu, W. T., A. Duan and B. He 2017: Evaluation of intra-seasonal oscillation simulations in IPCC AR5 coupled GCMs associated with the Asian summer monsoon. Int. J. Climatol. 37: 476–496. doi:10.1002/joc.5016[PDF]
Liu, S. F., and A. M. Duan, 2017: Impacts of the leading modes of the tropical Indian Ocean sea surface temperature anomaly on the sub-seasonal evolution of the circulation and rainfall over East Asia during boreal spring and summer. Journal of Meteorological Research, 31: 171-186, doi: 10.1007/s13351-016-6093-z.[PDF]
Su Jiayi, Duan Anmin and Xu Haiming, 2017, Quantitative analysis of surface warming amplification over the Tibetan Plateau after the late 1990s using surface energy balance equation, Atmos. Sci. Lett. 3(18): 112–117, doi: 10.1002/asl.732. （第一单位 南京信息工程大学）[PDF]
Xie, Z., Duan, A. and Tian, Q. ，2017：Weighted composite analysis and its application: an example using ENSO and geopotential height. Atmos. Sci. Lett, 18: 435–440. doi:10.1002/asl.786[PDF]
Liu, S., A. Duan, 2017: Impacts of the global sea surface temperature anomaly on the evolution of circulation and precipitation in East Asia on a quasi-quadrennial cycle. Climate Dynamics. doi: 10.1007/s00382-017-3663-4[PDF]
赵俊杰,薛峰,林万涛,段安民. 2016. El Niño 对东亚夏季风和夏季降水季节内变化的影响 [J]. 气候与环境研究, 21(6): 678−686 Zhao Junjie, Xue Feng, Lin Wantao, et al. 2016. The El Niño influence on intra-seasonal variations of East Asian summer monsoon and summer rainfall [J]. Climatic and Environmental Research(in Chinese), 21 (6): 678−686, doi:10.3878/j.issn.1006-9585.2016.15244.[PDF]
段安民, 肖志祥, 吴国雄，2016: 1979—2014年全球变暖背景下青藏高原气候变化特征[J]. 气候变化研究进展, 12(5): 374-381. CSCD[PDF]
Hu, W. T*., A. Duan, Y. Li, and B. He, 2016: The Intraseasonal Oscillation of Eastern Tibetan Plateau Precipitation in Response to the Summer Eurasian Wave Train. J. Climate, 29, 7215–7230, doi: 10.1175/JCLI-D-15-0620.1. SCI[PDF]
王子谦，段安民，李茂善等, 2016: 基于WRF模式的青藏高原斜坡和平台加热影响亚洲夏季风的模拟研究. 地球物理学报, 59(9), 3175–3187, doi: 10.6038/cjg20160904. SCI[PDF]
Xiao, Z. X., and Duan, A. M.*, 2016: Impacts of Tibetan Plateau Snow Cover on the Interannual Variability of the East Asian Summer Monsoon. Journal of Climate, 29(23),8495-8514,doi: 10.1175/JCLI-D-16-0029.1. SCI[PDF]
田珊儒, 段安民, 王子谦, 巩远发. 2015: 地面加热与高原低涡和对流系统相互作用的一次个例研究．大气科学, 39 (1): 125-136，doi: 10.3878/j.issn.1006-9895.1404.13311. CSCD[PDF]
王子谦，段安民，李聪，2015：东风急流对孟加拉湾热带气旋初始涡旋形成的影响. 大气科学学报，38, (1), 1-8. doi: 10.13878/j.cnki.dqkxxb.20130523005. CSCD[PDF]
Hu Wenting, Anmin Duan, and Guoxiong Wu. 2015: Impact of sub-daily air-sea interaction on simulating intraseasonal oscillations over the tropical Asian monsoon region. Journal of Climate. 28, 1057-1073, doi: 10.1175/JCLI-D-14-00407.1. SCI[PDF]
An, Z. S., G. X. Wu, J. P. Li, Y. B. Sun, Y. M. Liu, W. J. Zhou, Y. J. Cai, A. M. Duan, L. Li, J. Y. Mao, H. Cheng, Z. G. Shi, L. S. Tan, H. Yan, H. Ao, H. Chang, and J. Feng, 2015: Global Monsoon Dynamics and Climate Change. Annu. Rev. Earth Planet. Sci., 43: 29-77, doi: 10.1146/annurev-earth-060313-054623. SCI[PDF]
Cui Yangfan, Duan Anmin, Liu Yimin, and Wu Guoxiong. 2015: Interannual variability of the spring atmospheric heat source over the Tibetan Plateau forced by the North Atlantic SSTA, Climate Dynamics, 45(5), 1617-1634, doi: 10.1007/s00382-014-2417-9. SCI[PDF]
Wu Guoxiong, Duan Anmin, Yimin Liu, et al. 2015: Tibetan Plateau climate dynamics: recent research progress and outlook. National Science Reivew, 2, 100-116. doi:10.1093/nsr/nwu045[PDF]
Duan, A. M.*, Z. X. Xiao, 2015: Does the climate warming hiatus exist over the Tibetan Plateau.Scientific Reports, 5, 13711. doi: 10.1038/srep13711. SCI[PDF]
Wang, Z. Q., A. M. Duan*, G. X. Wu, and Y Song, 2015: Mechanism for occurrence of precipitation over the southern slope of the Tibetan Plateau without local surface heating. International Journal of Climatology, 36, doi: 10.1002/joc.4609. SCI[PDF]
Hu, J., and A. M. Duan*, 2015: Relative contributions of the Tibetan Plateau thermal forcing and the Indian Ocean Sea surface temperature basin mode to the interannual variability of the East Asian summer monsoon. Climate Dynamics, 45(9), 2697-2711, doi: 10.1007/s00382-015-2503-7. SCI[PDF]
Xiao, Z. X., and A. M. Duan, 2015: Can the tropical storms originated from the Bay of Bengal impact the precipitation and soil moisture over the Tibetan Plateau? Science China: Earth Sciences, 58(6), 915-928, doi: 10.1007/s11430-014-5028-8. SCI 肖志祥, 段安民. 2015. 孟加拉湾热带风暴对青藏高原降水和土壤湿度的影响. 中国科学: 地球科学, 45: 625–638, doi: 10.1007/s11430-014-5028-8.[PDF]
Wang, M. R., A. M. Duan*, 2015: Quasi-biweekly oscillation over the Tibetan Plateau and its link with the Asian Summer monsoon. Jou 29 rnal of Climate, 28, 4921-4940. doi: 10.1175/JCLI-D-14-00658.1. SCI[PDF]
段安民，青藏高原地气系统作用特征、机制及其对气候系统影响的研究，青藏高原研究学科发展报告，郑度，中国科学技术出版社， pp 131-161，中国，2014/4. 【注：书籍章节】[PDF]
段安民, 肖志祥, 吴国雄, 王美蓉. 2014: 青藏高原冬春积雪影响亚洲夏季风的研究进展. 气象与环境科学, 37(3): 94-101. CSCD[PDF]
马耀明，胡泽勇，田立德，张凡，段安民等. 2014: 青藏高原气候系统变化及其对东亚区域的影响与机制研究进展. 地球科学进展, 29(2): 207-215. CSCD[PDF]
Wang Ziqian, Duan Anmin, Wu Guoxiong, 2014: Time-lagged impact of spring sensible heat over the Tibetan Plateau on the summer rainfall anomaly in East China: case studies using the WRF model. Climate Dynamics, 42, 2885-2898, doi: 10.1007/s00382-013-1800-2. SCI[PDF]
Duan Anmin, Xiao Zhixiang, and Hu Jun, 2014: Can current AGCMs reproduce hsitoriscal changes in the atmospheric diabatic heating over the Tibetan Plateau? Atmospheric and Oceanic Science Letters, 7(2), 143-148.[PDF]
Duan Anmin, Wang Meirong, and Xiao Zhixiang. 2014. Uncertainties in quantitatively estimating the atmospheric heat source over the Tibetan Plateau, Atmospheric and Oceanic Science Letters, 7(1), 28-33.[PDF]
Wang Ziqian, Duan Anmin, Wu Guoxiong, 2014: Impacts of Boundary Layer Parameterization Schemes and Air-sea Coupling on WRF Simulation of the East Asian Summer Monsoon.Science China Earth Sciences,57(7),1480-1493. 王子谦, 段安民, 吴国雄. 2014. 边界层参数化方案及海气耦合对 WRF 模拟东亚夏季风的影响. 中国科学: 地球科学, 44: 548–562. SCI EI CSCD[PDF]
吴国雄, 段安民, 刘屹岷, 颜京辉, 刘伯奇, 任素玲, 张亚妮, 王同美, 梁潇云, 关月. 2013. 关于亚洲夏季风爆发的动力学研究的若干近期进展[J]. 大气科学, 37(2): 211–228, doi:10.3878/j.issn.1006-9895.2012. Wu Guoxiong, Anmin Duan, Yimin Liu, JingHui Yan, Boqi Liu, Suling Ren, Yani Zhang, Tongmei Wang, Xiaoyun Liang, and Yue Guan, 2013: Recent advances in the study on the dynamics of the Asian summer monsoon onset. Chinese Journal of Atmospheric Sciences (in Chinese), 37, 211–228.[PDF]
吴国雄，段安民，张雪芹，刘屹岷，马耀明，阳坤，2013. 青藏高原极端天气气候变化及其环境效应，自然杂志，35（3），167－171. doi: 10.3969/j.issn.2095-1973.2013.03.007.[PDF]
何洁琳, 段安民, 黄永森. 2013. 西北太平洋热带气旋群发与MJO的联系，气象科技进展，3 (3): 46-51，doi:10.3878/j.issn.1006-9585.2012.11075.[PDF]
何洁琳, 段安民, 覃卫坚. 2013: 热带大气季节内振荡与西北太平洋热带气旋活动的季节预测:统计事实研究.气候与环境研究，18(1):101-110,doi:10.3878/j.issn.1006-9585.2012.11075. CSCD[PDF]
Liu Yimin, Hu Jun, He Bian, Bao Qing, Duan Anmin, and Wu Guoxiong, 2013: Seasonal evolution of subtropical anticyclones in the climate system model FGOALS-s2. Advances in Atmospheric Sciences, 30(3), 593–606, doi:10.1007/s00376-012-2154-0. SCI[PDF]
Hu Wenting, Duan Anmin, and Wu Guoxiong, 2013: Performance of FGOALS-s2 in simulating intraseasonal oscillation over the South Asian monsoon region. Advances in Atmospheric Sciences, 30(3), 607–620, doi:10.1007/s00376-013-2156-6. SCI[PDF]
Duan Anmin, Wang Meirong, Lei Yonghui, and Cui Yangfan, 2013: Trends in Summer Rainfall over China Associated with the Tibetan Plateau Sensible Heat Source during 1980–2008. Journal of Climate, 26, 261–275.SCI EI[PDF]
Duan Anmin, Hu jun, Xiao Zhixiang, 2013: The Tibetan Plateau Summer Monsoon in the CMIP5 Simulations. Journal of Climate, 26, 7747–7766. SCI EI[PDF]
王子谦, 段安民, 郑永骏, 刘琨, 梁旭东, 马光. 2012: 中尺度海-气耦合模式GRAPES_OMLM对台风珍珠的模拟研究. 气象学报, 70(2): 261-274. CSCD[PDF]
Yuanjian Yang, Liang Sun, Anmin Duan, Yubin Li, Yunfei Fu, Youfang Yan, Ziqian Wang, Tao Xian. 2012: Impacts of the binary typhoons on upper ocean environments in November 2007. Journal of Applied Remote Sensing, 6, 063583, doi:10.1117/1.JRS.6.063583. SCI EI[PDF]
Wu Guoxiong, Liu Yimin, He Bian, Bao Qing, Duan Anmin, Jin Feifei. 2012: Thermal Controls on the Asian Summer Monsoon. Scientific Report. 2. 404, doi:10.1038/srep00404. SCI[PDF]
Wang Ziqian, Duan Anmin. 2012: A New Ocean Mixed-Layer Model Coupled into WRF.Atmospheric and Oceanic Science Letters, 5(3), 170−175.[PDF]
Wang Meirong, Zhou Shunwu, Duan Anmin. 2012: Trend in the atmospheric heat source over the central and eastern Tibetan Plateau during recent decades: Comparison of observations and reanalysis data. Chinese Science Bulletin, 57(5), 548–557. 王美蓉, 周顺武, 段安民. 2012: 近30年青藏高原中东部大气热源变化趋势：观测与在分析资料对比. 科学通报, 57（2-3）：178–188. SCI CSCD[PDF]
Liu Yimin, Wu Guoxiong, Hong Jieli, Wang Bin, Dong Buwen, Duan Anmin, Bao Qing, Zhou Linjiong. 2012: Revisiting Asian monsoon formation and change associated with Tibetan Plateau forcing: II. Change. Climate Dynamics, 39(5), 1183–1195. SCI[PDF]
Wu Guoxiong, Liu Yimin, Dong Buwen, Liang Xiaoyun, Duan Anmin, Bao Qing, Yu Jingjing. 2012: Revisiting Asian monsoon formation and change associated with Tibetan Plateau forcing: I. Formation. Climate Dynamics, 39(5), 1169-1181. SCI[PDF]
Duan Anmin, Wu Guoxiong, Liu Yimin, Ma Yaoming, Zhao Ping. 2012: Weather and Climate Effects of the Tibetan Plateau. Advances in Atmospheric Sciences, 29(5), 978–992. SCI[PDF]
Lei, Yonghui & Duan, Anmin. (2011). Prolonged dry episodes and drought over China. International Journal of Climatology. 31. 1831 - 1840. Doi: 10.1002/joc.2197.[PDF]
Hu Wenting, Duan Anmin, Wu Guoxiong. 2011: Sensitivity of simulated tropical intraseasonal oscillations to cumulus schemes. Science China Earth Sciences, 54(11), 1761–1771. 胡文婷, 段安民, 吴国雄. 2011：积云对流参数化方案对热带大气季节内振荡模拟的影响. 中国科学：地球科学.41（9），1341-1351. SCI EI CSCD[PDF]
Duan Anmin, Li Fei, Wang Meirong, Wu Guoxiong. 2011: Persistent Weakening Trend in the Spring Sensible Heat Source over the Tibetan Plateau and Its Impact on the Asian Summer Monsoon. Journal of Climate, 24(21), 5671-5682. SCI EI[PDF]
李菲, 段安民. 2011: 青藏高原夏季风强弱变化及其对亚洲地区降水和环流的影响-2008年个例分析.大气科学, 35(4), 694-706. CSCD[PDF]
段安民, 吴国雄, 青藏高原对东亚气候变化的影响， 《10000个科学难题：地球科学卷》， 罗吉等， 科学出版社， pp 812-815， 中国， 2010/12. 【注：书籍章节】[PDF]
王子谦, 朱伟军, 段安民＊. 2010: 孟湾风暴影响高原暴雪的个例分析：基于倾斜涡度发展的研究. 高原气象, 29(3), 703-711. CSCD[PDF]
段安民 天气、气候系统和空间天气的变化与趋势预测 21世纪中国地球科学发展战略报告， 候俊林， 科学出版社， pp 212-214， 中国， 2009/1. 【注：书籍章节】[PDF]
Wu Guoxiong, Y. Liu, X. Zhu, W. Li R. Ren, A. Duan, and X. Liang. 2009： Multi-scale forcing and the formation of subtropical desert and monsoon. Annals of Geophysics, 27(9), 3631–3644[PDF]
Duan Anmin, Wu Guoxiong. 2009: Weakening Trend in the Atmospheric Heat Source over the Tibetan Plateau during Recent Decades. Part II: Connection with climate warming, Journal of Climate, 22(15), 4197-4212. SCI.EI[PDF]
Duan Anmin, Sui Chung-Hsiung, Wu Guoxiong. 2009: Local air-sea interaction in ITZC simulations, Journal of Geophysical Research, 114, D22101, doi:10.1029/2009JD012405, 2009. [PDF]
Duan Anmin, Wu Guoxiong, and Liang Xiaoyun. 2008: Influence of the Tibetan Plateau on the summer climate patterns over East Asia in the IAP/LASG SAMIL model, Advances in Atmospheric Sciences, 25(4), 518-528.[PDF]
Duan Anmin, Sui Chunghsiung, Wu Guoxiong, 2008: Simulation of local air-sea interaction in the great warm pool and its influence on Asian monsoon, Journal of Geophysical Research, 113, D22105, doi:10.1029/2008JD010520.[PDF]
Duan Anmin, Wu Guoxiong. 2008: Weakening Trend in the Atmospheric Heat Source over the Tibetan Plateau during Recent Decades. Part I: Observations, Journal of Climate, 21(13), 3149-3164. EI[PDF]
Wu Guoxiong, Liu Yimin, Wang Tongmei, Wan Rijin, Liu Xin, Li Weiping, Wang Zaizhi, Zhang Qiong, Duan Anmin, Liang Xiaoyun, 2007: The Influence of Mechanical and Thermal Forcing by the Tibetan Plateau on Asian Climate. Journal of Hyfrometeorology, 8(4), 770-789.[PDF]
Liu Yimin, Bao Qing, Duan Anmin, Qian Zhengan, Wu Guoxiong. 2007. Recent Progress in the Impact of the Tibetan Plateau on Climate in China. Advances in Atmospheric Sciences, 24(6), 1060-1076.[PDF]
Duan Anmin. 2007: Cooling trend in the upper troposphere and lower stratosphere over China, Geophysical Research Letters, 34(15), doi:10.1029/2007GL029667.[PDF]
Wu Guoxiong, Jiangyu Mao, Anmin Duan, and Qiong Zhang, 2006: Current progresses in study of impacts of the Tibetan Plateau on Asian summer climate. Acta Meteor. Sinica, 20(2), 144-158.[PDF]
吴国雄, 李建平, 周天军, 陆日宇, 俞永强, 朱 江, 穆 穆, 段安民, 任荣彩, 丁一汇, 李维京, 何金海, 王 凡, 于卫东, 乔方利, 袁东亮, 齐义泉, 2006：影响我国短期气候异常的关键区：亚印太交汇区, 地球科学进展, 21(11), 1109-1118.[PDF]
段安民*, 吴国雄. 2006: 定常条件下感热和地形影响的Rossby波. 气象学报, 64(2), 129-136.[PDF]
Duan Anmin, Wu Guoxiong, Zhang Qiong, Liu Yimin. 2006: New proofs of the recent climate warming over the Tibetan Plateau as a resultof the increasing greenhouse gases emissions. Chinese Science Bulletin, 51(11), 1396－1400. [PDF]
Duan Anmin, Wu Guoxiong. 2006: Change of cloud amount and the climate warming on the Tibetan Plateau. Geophysical Research Letters, 33(22), L22704, doi: 10.1029/2006GL027946.[PDF]
吴国雄, 刘屹岷, 刘新, 段安民, 梁潇云. 2005: 青藏高原加热如何影响亚洲夏季的气候格局. 大气科学, 2005, 29(1), 47-56.[PDF]
段安民, 吴国雄. 2005: 青藏高原气温的年际变率与大气环状波动模. 气象学报, 63(5), 790-798.[PDF]
Duan Anmin, Wu Guoxiong. 2005: Wave-mean flow interaction and its relationship with the atmospheric energy cycle with diabatic heating, Science in China Series D Earth Sciences, 48(8), 1293-1302.[PDF]
Duan Anmin, Liu Yimin, Wu Guoxiong. 2005: Heating status of the Tibetan Plateau from April to June and rainfall and atmospheric circulation anomaly over East Asia in midsummer, Science in China Series D Earth Sciences, 48(2), 250-257.[PDF]
Duan Anmin, Wu Guoxiong. 2005: Role of the Tibetan Plateau Thermal Forcing in the Summer Climate Patterns over Subtropical Asia. Climate Dynamics.24(7-8), 793－807. [PDF]
吴国雄, 毛江玉, 段安民, 张琼. 2004: 青藏高原影响亚洲夏季气候研究的最新进展. 气象学报, 62(5), 528-540.[PDF]
段安民, 毛江玉, 吴国雄. 2004: 孟加拉湾季风爆发可预测性的分析和初步应用, 高原气象, 2004, 23(1), 18-25.[PDF]
Duan Anmin, Wu Guoxiong. 2004: Main heating modes over the Tibetan Plateau in July and the correlation patterns of circulation and precipitation over East Asia, Aata Meteorological Sinica Press, 18(2), 167-178.[PDF]
段安民, 吴国雄. 2003: 7月青藏高原大气热源主要空间型及其与东亚大气环流和降水的相关研究. 气象学报, 61(4), 447-456.[PDF]
毛江玉, 段安民, 刘屹岷, 吴国雄. 2003: 副高脊面反转与亚洲夏季风爆发可预测性分析. 科学通报, 48 (S2), 55-59.[PDF]
Mao Jiangyu, Duan Anmin, Liu Yimin, Wu Guoxiong. 2003: Change in the tilting of the ridgeline surface of the subtropical anticyclone and the predictability of the onset of the Asian summer monsoon. Chinese Science Bulletion, 48 (S2), 18-23. [PDF]
段安民. 1999: 拉萨气温和降水变化特征的小波分析，西藏科技，1999，4(5), 40-44.[PDF]
吴洪宝, 段安民. 1998: 兰州气温变化长期倾向和振荡的检测及预报试验. 南京气象学院学报, 22(4), 629-636[PDF]
吴洪宝, 段安民. 1998: 全球热带SSTA与中国7月降水和气温的伴随相关型分析. 南京气象学院学报, 21(3), 418-423.[PDF]
段安民, 吴洪宝. 1998: 全球热带海表温度异常的POP预报模型. 南京气象学院学报, 21(3), 346-353.[PDF]
段安民, 吴洪宝. 1998: 全球热带海表温度异常的主振荡型分析. 南京气象学院学报, 21(1), 61-69.[PDF]

Atmospheric heat source sink dataset over the Tibetan Plateau based on satellite and routine meteorological observations.pdf

 

高原大气热源数据介绍（Please refer to the article for the English introduction）


青藏高原作为地球的第三极，春夏季作为热源对区域和全球的天气和气候有着重要的影响。为了探究高原多时间尺度热力强迫作用的时空变化特征，建立一套持续、可靠的长时间观测的观测数据为基础的高原热源或汇数据是十分有必要的。本套数据利用中国气象局在青藏高原上80（32）个观测台站1979—2016（1960—2016）年的气象要素（地表温度、地表气温、10m 风速、 日累计降水量等）为基础计算得到感热（SH）和潜热（LH），同时利用卫星资料处理得到高原上1984—2015年的净辐射通量（RC）。


数据处理方法说明：
大气热源或汇（E）的表达式 ：E = SH + LH +RC  （1）


1，利用总体动力学公式估计地表感热通量SH：


1.png （2）

    

其中，u.png是近地面观测层的风速大小，Tg.png是地表温度，Ta.png是近地面观测层的气温，肉.png是空气密度，Cp.png是定压比热，Ch.png是总体热输送系数。考虑到Ch.png存在日变化特征，这里使用Yang et al. (2009)提出的方案来估计地表感热通量。为了适应Ch.png的日变化，使用青藏高原试验的高分辨率资料和低分辨率的中国气象局站点资料，基于统计降尺度的方法得到逐小时的风速大小、地表温度和气温。详细计算方法参考Yang et al.（2009）。



2，凝结潜热释放


2.png （3）

    

其中P.png是降水量，3.png是凝结加热系数，4.png是水的密度。公式（2）的降水量使用中国气象局提供的24小时累积（北京时间20时到次日20时）的降水资料（Duan &Wu, 2008）。

 

3. 净辐射通量 


逐月的卫星资料（GEWEX/SRB和CERES/EBAF）的时间范围分别是1984–2007和2000–2015。从两套卫星资料获取净辐射通量的步骤如下：第一步，将格点资料使用双线性插值方法插值到80个站点，使用两者重复的时间段2000-2007建立线性回归模型来订正后者的系统性偏差。在线性回归模型中，假设误差项是正态分布，EBAF资料在每个站点被当作是预报因子x，而SRB资料是预报量，模型方程为


y=wx+b+ε （4）


 其中，ε 是误差项，w 和 b是待估计的权重和偏差。2000–2007年经过插值的EBAF和SRB资料被用于估计每个站点的参数，2007年以后的资料将根据线性回归模型将EBAF订正到SRB来消除系统性偏差。大气柱的净辐射通量计算公式为


 RC=R_∞-R_0=(S_∞^↓-S_∞^↑ )-(S_0^↓-S_0^↑ )-(F_0^↓-F_0^↑ )-F_∞,  （5）


其中，R_∞  和 R_0 分别代表大气层顶和地表的净辐射通量。变量S 和F 分别表示短波和长波辐射通量，其中上标 ↓ 和 ↑ 分别代表向下和向上的辐射通量。特别的，F_0 和 F_∞ 分别表示地表和大气层顶的长波辐射通量。从1984到2007年，资料只依赖于SRB，而在2008–2015年是基于SRB 和 EBAF。随着系统性误差被剔除，资料可以被看作是没有间断的长期序列。
1. 国家自然科学基金委员会与泰国研究基金会“气候变化”合作研究项目“中南半岛和华南极端降水事件年代际变化的机理，影响和未来预估”（4181101153），2019－2021，中方项目负责人。

The Major International (Regional) Joint Research Project between the National Natural Science Foundation of China and Thailand research Foundation: Mechanisms, impacts and future projections of the interdecadal variations of rainfall extremes in Indochina Peninsula and southern China [grand no. 4181101153]. 2019－2021, PI in China group.


2. 国家自然科学基金杰出青年基金项目“海气自然变率影响青藏高原热源的过程和机理”（41725018），2018－2022，项目负责人。

The National Science Fund for Distinguished Young Scholars：The processes and mechanism of the air-sea natural variability in modulating the atmospheric heat source over the Tibetan Plateau [grand no. 41725018]. 2018－2022, PI.


3. 中国科学院先导A类项目“地球大数据科学工程”项目七：“时空三极环境”第四课题：“三极气候系统多圈层相互作用”（XDA19070404），2018-2022。课题负责人。

The Strategic Priority Research Program of the Chinese Academy of Sciences. Task 4: “The interaction of climate system in the three poles on earth” under Project 7: “The spatial-temporal environment of the three poles on earth” in the framework of “The earth big data scientific project”. [grant no. XDA19070404]. 2018－2022, PI.


4. 国家自然科学基金重大研究计划重点支持项目＂青藏高原与热带海洋对东亚季风年际变率的协同影响＂（91337216），2014－2017，项目负责人。

The Key Project of the Major Research Program of National Natural Science Foundation of China: “The combined effect of the Tibetan Plateau and tropical oceans on the interannual variability of East Asian summer monsoon” [Grant No. 91337216]. 2014－2017. PI.


5. 国家自然科学基金面上项目＂青藏高原夏季风的多尺度变率＂(41175070)，2012－2015，项目负责人。

The General Project of the National Natural Science Foundation of China: “The multi-scale of the Tibetan Plateau summer monsoon” [Grant No. 41175070]. 2012－2015. PI.


6. 国家自然科学基金面上项目＂青藏高原春季热状况与东亚季风的长期变化趋势＂(40975047)，2010－2012，项目负责人。

The General Project of the National Natural Science Foundation of China: “The linkage between the spring heat status over the Tibetan Plateau and East Asian summer monsoon” [Grant No. 40975047]. 2010－2012. PI.


7. 全球变化研究国家重大科学研究计划项目＂青藏高原气候系统变化及其对东亚区域的影响与机制研究＂(2010CB951700)，2011－2015，课题负责人。

The National Major Science Research Program for Global Change [Grant No. 2010CB951703]. 2011－2015. PI of Task 4.


8. 国家重点基础研究发展计划（973计划）项目＂全球变暖背景下东亚能量和水循环变异及其对我国极端气候的影响＂（2009CB421403），2009－2013，专题负责人。

The National Key Basic Research Development Plan: “Variation of energy and water cycle in East Asia and its impact on extreme climate”. [Grant No. 2009CB421403]. 2009－2013. The core scientist.


9. 国家重点基础研究发展计划（973计划）项目＂亚印太交汇区海气相互作用及其对我国短期气候的影响＂（S200604029），2006-2010，专题负责人。

The National Key Basic Research Development Plan: “The air-sea interaction in the Asia-Indian Ocean-Pacific region and its impact on short-range climate in China” [Grant No. S200604029]. 2006－2010. The core scientist.


10. 国家自然科学基金青年科学基金项目＂青藏高原激发的大气定常波对亚洲气候的影响＂（40405016），2005－2007，项目负责人。

The Youth Science Foundation Program of the National Natural Science Foundation of China: “The influence of the steady atmospheric wave stimulated by the Tibetan Plateau upon the Asian climate” [Grant No. 40405016]. 2005－2007. PI.


11. 公益性行业（气象）专项项目课题＂东亚区域云与陆表物理过程的模式参数化技术研究＂（GYHY2010060140），2012-2013，课题负责人。

Task 3 of The Public Welfare Industry (Meteorology) special project: “Parameterization skill of cloud and land surface physical processes in East Asia” [Grant No. GYHY2010060140]. 2008－2013. PI.


12. 中国科学院知识创新工程重要方向项目＂亚洲季风区海－陆－气相互作用对我国气候变化的影响＂课题：青藏高原和印度洋，太平洋热力差异对我国气候变化的影响，2010－2012，专题负责人。

Task 4 of the Key Direction Project of the Chinese Academy of Sciences Knowledge Innovation Program named “Land-air-sea interaction impact on climate change in China”: “The thermal contrast among the Tibetan Plateau, Indian Ocean, and the Pacific and its impact on climate change in China”. 2010-2012. The core scientist

1. 世界气候研究计划（WCRP）全球能量与水分循环（GEWEX）中国委员会委员，2012 年7 月至今
2. 中国气象学会高原气象委员会委员，2013 年5 月至今
3. 《大气科学》常务编委，2014 年7 月至今
4. 《气象学报》编委，2011 年9 月至今
5. 中国科学院大气物理研究所青年科学家实验室第一期联合主任，2012 年7 月－2014 年6 月

2016 IRS- Auckland
“Does the climate warming hiatus exist over the Tibetan Plateau?”


2016 CCGG-Nanjing
“Impact of Surface Sensible Heating over the Tibetan Plateau on the Western Pacific Subtropical High: a Land–Air–Sea Interaction Perspective”


2016 EAC-Beijing (Invited speech)
“Relative contribution of the Tibetan Plateau thermal forcing and the Indian Ocean SST Basin Mode to the interannual variability of the East Asian Summer Monsoon”


2016 Future Earth-Haikou
“Recent climate over the Tibetan Plateau and its disaster and environment impacts”


2016 AGU-San Francisco
“Warming amplification over the Tibetan Plateau since the end of 1990s”


2017 干旱气候变化与减灾-Lanzhou
“Circulation and precipitation in East Asia associated with the global SSTA on the quasi-quadrennial cycle”


2017 IAPSO-IAMAS-IAGA
“Impact of Surface Sensible Heating over the Tibetan Plateau on the Western Pacific Subtropical High: a Land–Air–Sea Interaction Perspective”


2017 ICTP-Italy
“Impact of the Tibetan Plateau on East Asian Summer Monsoon: a Land–Air–Sea Interaction Perspective”


2017 EGU-Vienna (Invited speech)
“Impact of Tibetan Plateau snow cover on the interannual variability of the East Asian summer monsoon”


2017 AGU-New Orleans
“Alteration of the Oceanic Forcing of the East Asian Summer Monsoon by the Effect of Tibetan Plateau heating”


2018 NASA-Chengdu
“Simulation of the Tibetan Plateau thermal forcing on East Asian summer monsoon”


2018 AOGS-Hawaii
“Quantitative Analysis of Surface Warming Amplification over the Tibetan Plateau after the Late 1990s Using Surface Energy Balance Equation”


2018 CSSP-Shanghai
“Atmospheric heat source/sink dataset over the Tibetan Plateau based on satellite and routine meteorological observations”


2018 HiMAC-Finland
“Atmospheric heat source/sink dataset over Tibetan Plateau during 1960-2016 based on satellite and routine meteorological observations”


2018 CGU-Beijing (Invited speech)

“Response of the Indian Ocean mixed layer and upper layer current to the Tibetan Plateau thermal forcing in late spring”


2018 AGU-Washington DC
“Atmospheric heat source/sink dataset over Tibetan Plateau during 1960-2016 based on satellite and routine meteorological observations”


2019 中德科学前沿研讨会-吕贝克，德国

“Tibetan Plateau and Monsoon”


2019 AOGS-新加坡 (Invited speech)

 “The Synergetic Effects Between the Tibetan Plateau and Tropical Ocean on the Interannual Variability of East Asian Summer Monsoon”


2019 CSSP-英国

“The Tibetan Plateau thermal forcing on East Asian Summer Monsoon in the view of land-air-sea interaction”


2019AGU-美国

“Interannual variability of the North Pacific mixed layer associated with the spring Tibetan Plateau thermal forcing”毕业博士：

胡文婷（2012）  王子谦（2014）  王美蓉（2015）  崔扬帆（2015）  肖志祥（2016）  刘森峰（2018）

毕业硕士：

李菲（2011）  胡俊（2014）  田珊儒（2014）  段丽君（2017）  苏珈仪（2017）  赵俊杰（2016）  谢志昂（2018）

在读博士生：

赵宇  孙睿藻  庄默然  高凯伦  陈宇航（客座）  沈子力（客座）

在读硕士生：

彭玉琢  张萍  汤彬  魏吉林


Graduated Ph.D students:

HU Wenting(2012)   WANG Ziqian(2014)   WANG Meirong(2015)   CUI Yangfan(2015)   XIAO Zhixiang(2016)   LIU Senfeng(2018)

Graduated Master students:

LI Fei(2011)   HU Jun(2014)   TIAN Shanru(2014)   DUAN Lijun(2017)   SU Jiayi(2017)   ZHAO Junjie(2016)   XIE Zhiang(2018)

Current Ph.D students:

ZHAO Yu,  SUN Ruizao,   ZHUANG Moran,   GAO Kailun,   CHEN Yuhang(Visiting),   SHEN Zili(Visiting)

Current Master students:

PENG Yuzhuo,   ZHANG Ping,   TANG Bin,   WEI Jilin