孙德征
****/博士生导师
dezhengsun@fudan.edu.cn
+86-21-3124-8808

助理：谢梦；mengxie@fudan.edu.cn；+86-21-3124-8804


个人简介
1992年麻省理工学院博士，先后任职于普林斯顿大学、美国国家大气研究中心、美国国家大气海洋局和科罗拉多大学，2019年加入复旦大学。
主要研究方向是气候动力学，包括水汽和云在大气变迁中的反馈，大尺度海气耦合和全球气候变迁的模拟和预测。
原创性科学贡献包括：
高层云在决定热带水汽在气候变迁中反馈的决定角色，大尺度海气耦合在调节热带最高海温的决定角色、厄尔尼诺（El Nino）的非绝热非线性的起源、厄尔尼诺－南方涛动整流 (ENSO rectification) 在产生年代际和更长时间尺度上气候变化的重要角色等。研究成果发表在包括Science（科学）和Journal of Climate（气候）等多种国际顶尖杂志上。主持了多项由NOAA、NSF 等资助的科研项目，累计金额300多万美元。编辑了由美国地球物理学会（AGU）发表的气候动力学专著《气候动力学：气候为什么一直在变化》（Climate Dynamics: Why Does Climate Vary?）

研究兴趣
气候动力学，包括水汽和云在气候变迁中的反馈，大尺度海气相互作用，和全球气候模拟及预测



教育背景
学士学位（1985年），气候学，南京大学
硕士学位（1987年），天气动力学，中国科学院大气物理研究所
博士学位（1992年），气象学，麻省理工学院
研究经历
1992年 —1995年，博士后， 普林斯顿大学
1995年 -—1997年，研究员，美国国家大气研究中心
1997年 -—2016年，研究员，美国国家海洋大气局－卡罗拉多大学联合环境科学研究所
2016年 -—2018年，研究员，卡罗拉多大学大气与海洋科学系
2019年 -— 至今，****，复旦大学大气与海洋科学系
承担课题
1998年5月 —2001年4月,NOAA, The Role of Water Vapor in the Large-scale Ocean-Atmosphere Interaction in the Tropical Pacific Region, USA，$143,722，主持
2000年6月 —2004年6月，NSF，El Ni?o and the Tropical Maximum SST，USA，$199,894，主持
2003年2月 —2006年1月，NSF，The Influence of the Warm-pool SST over the Magnitude of El Ni?o Warming, USA，$197,943，主持
2003年12月 —2007年5月，NSF，Understanding the Causes of the Excessive Cold-tongue in the NCAR CCSM, USA，$131,056，主持
2006年4月 —2009年3月,NSF, The Role of Extratropical Cooling in Determining the Level of ENSO Activity, USA，$365,029，主持
2009年6月 —2013年5月，NSF，The Effects of ENSO on the Mean Climate State of the Tropical Pacific，USA，$410,736，主持
2010年9月 —2013年8月，NOAA，Decadal Variability in the Tropical Pacific SST: A Consequence of Scale Interaction, USA，$361,054，主持
2011年9月 —2014年8月，NOAA，Nonlinearity of Tropical Convection and the Asymmetry of the El Nino Southern Oscillation, USA，$362,993，主持
2014年9月 —2017年8月，NOAA，Excessive Cold-tongue and Weak ENSO Asymmetry: Are These Two Tropical Biases Linked?, USA，$376,061，主持
2015年6月 —2018年5月，NSF，Rectification of El Nino-Southern Oscillation as a Mechanism for the Tropical Pacific Decadal Variability: A Diabatic and Time-Dependent View, USA，$486,044，主持
教学经历

2002年8月 — 2002年12月，Our Changing Environment, 本科生，University of Colorado
2006年8月 —2006年12月，Climate Dynamics Seminar，研究生，University of Colorado
2008年8月 —2008年12月，Climate Dynamics: Why Does Climate Vary? 研究生，University of Colorado
2018年6月 —2018年7月，厄尔尼诺， 研究生，复旦大学

发表论文
1，Wallace J.M., X. Cheng, andD.-Z. Sun,1991: Does low-frequency atmospheric variability exhibit regime-like behavior?Tellus,43 AB, 16-26.
2，Sun, D.-Z.and R.S. Lindzen, 1993: Water vapor feedback and the ice age snowline record.Ann. Geophys.,11, 204-215.
3，Sun, D.-Z. and R.S. Lindzen, 1993: Distribution of tropical tropospheric water vapor.J. Atmos. Sci.,50, 1643-1660.
4，Sun, D.Z. and R.S. Lindzen, 1994: A PV view of the zonal mean distribution of temperature and wind in the extratropical troposphere.J. Atmos. Sci.,51, 757-772.
5，Sun, D.-Z. and A.H. Oort, 1995: Humidity-temperature relationships in the tropical troposphere.J. Climate,8, 1974-1987.
6，Sun, D.-Z.and I.M. Held, 1996: A comparison of modeled and observed relationships between interannual variations of water vapor and temperature.J. Climate,9, 665-675.
7，Sun, D.-Z. and Z. Liu, 1996: Dynamic ocean-atmosphere coupling: a thermostat for the tropics.Science,272, 1148-1150.
8，Sun, D.-Z., 1997: El Ni?o: a coupled response to radiative heating?Geophys. Res. Lett.,24, 2031-2034.
9，Sun, D.-Z.and K.E. Trenberth, 1998: Coordinated heat removal from the equatorial Pacific during the 1986-87 El Ni?o.Geophys. Res. Lett.,,25, 2659-2662
10，Sun, D.-Z., 2000: Global climate change and ENSO: a theoretical framework.El Ni?o: Historical and Paleoclimatic Aspects of the Southern Oscillation, Multiscale variability and Global and Regional Impacts.443-463. Cambridge: Cambridge University Press, edited by Diaz H. F. and V. Markgraf, 476 pp.
11，Sun, D.-Z., 2000b: The heat sources and sinks of the 1986-87 El Ni?o,J. Climate,13, 3533-3550.
12，Fasullo, J., andD.-Z. Sun, 2001: Radiative sensitivies to tropical water vapor under all-sky conditions.J. Climate,14, 2798-2807
13，Sun, D.-Z., C. Covey, and R.S. Lindzen, 2001: Vertical correlations of water vapor in GCMs.Geophys. Res. Lett.,28, 259-262.
14，Sun, D.-Z., 2003:A Possible Effect of An Increase in the Warm-pool SST on the Magnitude of El Ni?o Warming.J. Climate,16, 185-205
15，Sun, D.-Z., J. Fasullo, T. Zhang, and A. Roubicek, 2003:On the Radiative and Dynamical Feedbacks over the Equatorial Cold-tongue.J. Climate,16. 2425-2432
16，Sun, D.-Z., T. Zhang, and S.-I. Shin, 2004: The effect of subtropical cooling on the amplitude of ENSO: a numerical study.J. Climate,17, 3786-3798.
17，Sun, D.-Z., 2004: The Control of Meridional Differential Heating Over the Level of ENSO activity: A Heat-Pump Hypothesis. page 71--83. InEarth's Climate: The Ocean-Atmosphere Interaction, AGU Geophysical Monograph, Vol. 147, 414 pages. Edited by C. Wang, S.-P. Xie, and J. Carton.
18，Zhang, T. and D.-Z. Sun 2006: Response of water vapor and clouds to El Nin? o warming in three National Center for Atmospheric Research atmospheric models. J. Geophys. Res.,111, D17103, doi:10.1029/2005JD006700
19，Sun, D.-Z., T. Zhang, C. Covey,S. Klein, W.D. Collins, J.J. Hack, J.T. Kiehl, G.A. Meehl, I.M. Held, and M. Suarez, 2006: Radiative and Dynamical Feedbacks Over the Equatorial Cold-tongue: Results from Nine Atmospheric GCMs.J. Climate,19, 4059-4074.
20，Sun, D.-Z. and T. Zhang 2006: A Regulatory Effect of ENSO on the Time-Mean Thermal Stratification of the Equatorial Upper Ocean.Geophys. Res. Lett., 33, L07710, doi:10.1029/2005GL025296.
21，Sun, D.-Z., 2007: The Role of ENSO in Regulating its Background State. InNonlinear Dynamics in Geosciences, pages 537-555, Springer New York, 604 pages, Edited by J. Elsner and A. Tsonis.
22，Zhang, T., and D.-Z. Sun, 2008: What Causes the Excessive Response of the Clear-Sky Greenhouse Effect to El Nino Warming in the NCAR Community Atmosphere Models?J. Geophys. Research, 113, D02108, doi:10.1029/2007JD009247.
23，Sun, D.-Z., Y. Yu, and T. Zhang, 2009: Tropical Water Vapor and Cloud Feedbacks in Climate Models: A Further Assessment Using Coupled Simulations.J. Climate,22, 1287-1304.
24，Yu, Y., and D.-Z. Sun, 2009: Response of ENSO and the Mean State of the Tropical Pacific to Extratropical Cooling/Warming: A Study Using the IAP Coupled Model. J. Climate,22, 5902-5917
25，Zhang,T., ,D.-Z. Sun, R. Neal, and P. Rasch, 2009: An Evaluation of ENSO Asymmetry in the Community Climate System Models: A View from the Subsurface. J. Climate,22, 5933-5961.
26，Sura, P. and D.-Z. Sun, 2009: Ocean-Atmosphere Coupling-Preface. Special Issue on Ocean-Atmosphere Coupling, Atmospheric Research,94, 1-2(doi:10.1016/j.atmosres.2009.07.003)
27，Penland C., D.-Z.Sun, and A. Capontondi, 2010: An Introduction to El Nino and La Nina. page 53--64. Climate Dynamics: Why Does Climate Vary?. AGU Geophysical Monograph, Edited by D.-Z. Sun and F. Bryan, AGU.
28，Wu, C., T. Zhou, R. Yu, and D.-Z.Sun, 2010: Regime behavior in the SST-cloud forcing relationships over the Pacific cold-tongue region.Atmos. Oceanic Sci. Lett.,3, 271-276.
29，Sun, D.-Z., 2010: The Diabatic and Nonlinear Aspects of El Nino Southern Oscillation: Implications for its Past and Future Behavior. page 79-104. Climate Dynamics: Why Does Climate Vary?. AGU Geophysical Monograph, Edited by D.-Z. Sun and F. Bryan, AGU.
30，Sun, D.-Z. and F.O. Bryan, 2010: Introduction. page 1-2, Climate Dynamics: Why Does Climate Vary?. AGU Geophysical Monograph, Edited by D.-Z. Sun and F. Bryan, AGU.
31，Sun, D.-Z., and F.O. Bryan, 2010: Preface. Climate Dynamics: Why Does Climate Vary?. AGU Geophysical Monograph, Edited by D.-Z. Sun and F. Bryan
32，Zhang, T., M.P. Hoerling, J. Perlwitz, D.-Z. Sun, and D. Murray, 2010Physics of U.S. surface temperature response to ENSO. J. Climate, 24, 4874-4887.
33，Wu, C., T.Zhou, D.-Z.Sun, Q.Bao, 2011,Water vapor and cloud radiative forcings over the Pacific Ocean simulated by the LASG/IAP AGCM: Sensitivity to convection schemesAdvances in Atmospheric Sciences,28, 809-98.
34，Eric Guilyardi, Wenju Cai, Mat Collins, Alexey Fedorov, Fei-Fei Jin, Arun Kumar, De-Zheng Sun, Andrew Wittenberg, 2011: New strategies for evaluating ENSO processes in climate models. BAMS,236, 235-238.
35，Liang, J., X.-Q. Yang, and D.-Z. Sun, 2012: The effect of ENSO events on the Tropical Pacific Mean Climate: Insights from an Analytical Model.J. Climate,25, 7590-7606.
36，Sheffield, J., S.J. Camargo, R. Fu, Q. Hu, X. Jiang, N. Johnson, K.B. Karnauskas, J. Kinter, S. Kumar, B. Langenbrunner, E. Maloney, A.a Mariotti, J. E. Meyerson, D. Neelin, Z. Pan, A. Ruiz-Barradas, R Seager; Y. L Serra, D.-Z. Sun, C. Wang, S.-P. Xie, J.Y. Yu, T. Zhang, M. Zhao, 2013: North American Climate in CMIP5 Experiments. Part II: Evaluation of 20th Century Intra-Seasonal to Decadal Variability.J. Climate, 26 (23), 9247-9290.
37，Sun, Y., D.-Z. Sun, F. Wang, and L. Wu, 2013: The Western Pacific Warmpool and ENSO Asymmetry in CMIP3 Models. Adv. Atmos. Sci., 30, 940-953doi: 10.1007/s00376-012-2161-1.
38，Ogata, T., S.-P. Xie, A. Wittenberg, and D.-Z. Sun, 2013: Interdecadal amplitude modulation of El Nino/Southern Oscillation and its impacts on tropical Pacific decadal variability. J. Climate, 26, 7280-7297.
39，Chen, L., Y. Yu, and D.-Z. Sun, 2013: Cloud and Water Vapor Feedbacks To El Nino Warming: Are They Still Biased in CMIP5 Models?J. Climate,26, 4947-4961.
40，Shuai, J., Z. Zhang, D.-Z. Sun, F. Tao, and P. Shi, 2013: ENSO, climate variability and crop yields in China. Clim. Res.,58, 133-148.
41，Sun, D.-Z., T. Zhang, Y. Sun, and Y. Yu, 2014: Rectification of El Nino-Southern Oscillation into Climate Anomalies of Decadal and Longer Time-scales: Results from Forced Ocean GCM Experiments. J. Climate,27, 2545-2561.
42，Zhang, T. and D.-Z. Sun, 2014: ENSO Asymmetry in CMIP5 models. J. Climate,27, 4070-4093.
43，Hua, L., Y. Yu, and D.-Z. Sun, 2015: A Further Study of ENSO Rectification: Results From an OGCM With a Seasonal Cycle.J. Climate,28, 1362-1382.
44，Sun, Y., F. Wang, and D.-Z. Sun, 2016: Weak ENSO asymmetry due to weak nonlinear air-sea interaction in CMIP5 climate models. Adv. Atmos. Sci., 33(3), 352-364.
45，Liang, J., X.-Q. Yang, and D.-Z. Sun, 2017: Factors Determining the Asymmetry of ENSO.J. Climate,30, 6097-6106. DOI: 10.1175/JCLI-D-16-0923.1
46，ang, M., G. J. Zhang, and D.-Z. Sun, 2018: Precipitation and Moisture in Four Leading CMIP5 Models: Biases across Large-scale Circulation Regimes and Their Attribution to Dynamic and Thermodynamic Factors.J. Climate,31, 5089--5016.
47，Chen, L., L. Wang, T. Li, D.-Z. Sun, 2018: Contrasting cloud radiative feedbacks during warm pool and cold tongue El Nino, Scientific Online Letters on the Atmosphere, 14, 126-131.
48，Chen, L., D.-Z. Sun, L. Wang, T. Li (2018): A further study on the simulation of cloud radiative feedbacks in the ENSO cycle in the tropical Pacific with a focus on the asymmetry, Asia-Pacific Journal of Atmospheric Sciences, doi:10.1007/s13143-018-0064-5
49，Hua, L., D.-Z. Sun, and Y. Yu, 2018: Why Do We Have El Ni?o: Quantifying A Diabatic and Nonlinear Perspective Using Observations. Climate Dynamics, DOI : 10.1007/s00382-018-4541-4.
50，Zhang, L., D.-Z. Sun,, and K.B. Karnuskas, 2019: The role of the Indian Ocean in determining the tropical pacific SSTresponse to radiative forcing in an idealized model.Dynamics of the Atmosphere and Oceans, 86, 1-9.
51，Lin, X., Y. Qiu, and D.-Z. Sun, 2019: Thermohaline Structures and Heat/Freshwater Transports of Mesoscale Eddies in the Bay of Bengal Observed by Argo and Satellite Data. Remote Sensing, 11, 2989; doi:10.3390/rs**

出版书籍
Sun, D.-Z. and F. Bryan (eds), 2010: Climate Dynamics: Why Does Climate Vary?. AGU Monograph, 216 pages, AGU.

#以上信息由本人提供，更新时间：2020/12/10