杨海军 - 复旦大学 - 大气与海洋科学系、大气科学研究院

个人简介

教育背景学士学位（1993年），气象学，云南大学硕士学位（1996年），气象学，中国科学院兰州高原大气物理研究所博士学位（2000年），物理海洋学，中国（青岛）海洋大学研究经历 2020年3月 — 至今，教授，复旦大学大气与海洋科学系 2009年 8月— 2020年2月，教授，北京大学物理学院大气与海洋科学系 2007年 9月— 2008年6月，访问学者，瑞典斯德哥尔摩大学气象系 2003年 8月— 2009年7月，副教授，北京大学物理学院大气科学与海洋科学系 2000年 8月— 2003年7月，博士后，美国 Wisconsin-Madison 大学大气与海洋科学系 1999年1月 — 2000年6月，研究助理，美国 Wisconsin-Madison 大学大气与海洋科学系获奖情况 2005年，第十一届（2004－2005年度）“涂长望青年气象科技奖”二等奖。获奖项目：用海盆模的观点理解太平洋年代际振荡。中国 2005年，中国教育部科学技术进步二等奖，证书号：2004－071。获奖项目：南海上层海洋环流、热结构的季节和季节内变化特征及形成机制。第二完成人。中国

研究领域

全球气候变化及全球变暖，大尺度海洋－大气相互作用，大洋风生环流与热盐环流动力学和数值模拟，区域海洋学与南海环流

近期论文

查看导师新发文章（温馨提示：请注意重名现象，建议点开原文通过作者单位确认）

Wen, Q., K. Doos, Z. Lu, Z. Han, and *H. Yang, 2020: Investigating the role of the Tibetan Plateau in ENSO variability. J. Climate, 33, doi: 10.1175/JCLI-D-19-0422.1. Wen, Q., and *H. Yang, 2020: Investigating the role of the Tibetan Plateau in the formation of Pacific meridional overturning circulation. J. Climate, 33, doi: 10.1175/JCLI-D-19-0206.1. *Yang, H., and Q. Wen, 2020: Investigating the role of the Tibetan Plateau in the formation of Atlantic meridional overturning circulation. J. Climate, 33, doi: 10.1175/JCLI-D-19-0205.1. *Yang, H., X. Shen, J. Yao and Q. Wen, 2020: Portraying the impact of the Tibetan Plateau on global climate. J. Climate, 33, doi: 10.1175/JCLI-D-18-0734.1. Wen, Q., J. Yao, K. Doos, and *H, Yang, 2018: Decoding the hosing and heat effects on global temperature and meridional circulations in a warming climate. J. Climate, 31(23), 9605-9623, doi: 10.1075/JCLI-D- 18-0297.1. Yang, Q., Y. Zhao, Q. Wen, J. Yao, and *H. Yang, 2018: Understanding Bjerknes compensation in meridional heat transports and the role of freshwater in a warming climate. J. Climate, 31(12), 4791- 4806, doi: 10.1175/JCLI-D-17-0587.1. *Yang, H., Q. Wen, J. Yao, and Y. Wang, 2017: Bjerknes compensation in meridional heat transport under freshwater forcing and the role of climate feedback. J. Climate, 30(14), 5167-5185, doi: 10.1175/JCLI-D-16-0824.1. Dai, H., *H. Yang, and J. Yin, 2017: Roles of energy conservation and regional climate feedback in Bjerknes compensation: a coupled modeling study. Climate Dynamics, 49, 1513-1529, doi: 10.1007/s00382-016-3386-y. Zhao, Y., *H. Yang, and Z. Liu, 2016: Assessing Bjerknes compensation for climate variability and its timescale dependence. J. Climate, 29(15), 5501-5512. *Yang, H., Y. Zhao, and Z. Liu, 2016a: Understanding Bjerknes compensation in atmosphere and ocean heat transports using a coupled box model. J. Climate, 29(6), 2145-2160, doi: 10.1175/JCLI-D-15- 0281.1. *Yang, H., K. Wang, H. Dai, Y, Wang, and Q. Li, 2016b: Wind effect on the Atlantic meridional overturning circulation via sea ice and vertical diffusion. Climate Dynamics, 46(11), 3387-3403, doi: 10.1007/s00382-015-2774-z. *Liu, Z., H. Yang, C. He, and Y. Zhao, 2016: A theory for Bjerknes compensation: the role of climate feedback. J. Climate, 29(1), 191-208. doi: 10.1175/JCLI-D-15-0227.1. *Yang, H., Y. Zhao, Q. Li, and Z. Liu, 2015: Heat transport in atmosphere and ocean over the past 22,000 years. Nature Scientific Reports, 5: 16661. doi: 10.1038/srep16661. *Yang, H., and H. Dai, 2015: Effect of wind forcing on the meridional heat transport in a coupled model: equilibrium response. Climate Dynamics, 45(5): 1451-1470, doi: 10.1007/s00382-014-2393-0. *Yang, H., Q. Li, K. Wang, Y. Sun and D. Sun, 2015: Decomposing the meridional heat transport in the climate system. Climate Dynamics, doi: 10.1007/s00382-014-2380-5, 44: 2751-2768. *Wang, L., and H. Yang, 2014: The role of atmospheric teleconnection in the subtropical thermal forcing on the equatorial Pacific. Adv. Atmos. Sci., 31(4), 985–994, doi: 10.1007/s00376-013-3173-1. *Huang, B., J. Zhu, and H. Yang, 2014: Mechanisms of Atlantic meridional overturning circulation (AMOC) variability in a coupled ocean--atmosphere GCM. Adv. Atmos. Sci., 31(2), 241-251, doi: 10.1007/s00376-013-3021-3. *Wang, Y. X., H. Yang, and T. Furevik, 2013: What determines the amplitude of ENSO events? Atmospheric and Oceanic Science Letters. 6(2), 90-96. *Yang, H., 2013: Assessing the meridional atmosphere and ocean energy transport in a varying climate. Chinese Science Bulletin, 58(15), 1737-1740, doi: 10.1007/s11434-01305665-x. *Yang, H., Y. Wang, and Z. Liu, 2013: A modeling studies of the Bjerknes compensation in the meridional heat transport in a freshening ocean. Tellus A, 65, 18480, http://dx.doi.org/10.3402/tellusa.v65i0.18480. *Yang, H., and L. Wang, 2011: Tropical Oceanic Response to Extratropical Thermal Forcing in a Coupled Climate Model: A Comparison between the Atlantic and Pacific Oceans. J. Climate, 24, 3850-3866. *Yang, H., and J. Zhu, 2011: Equilibrium Thermal Response Timescale of Global Oceans. Geophys. Res. Lett., 38, L14711, doi:10.1029/2011GL048076. *Yang, H., and F. Wang, 2009: A Revisit on the Thermocline Depth in the Equatorial Pacific. J. Climate, 22, 3856-3863. *Yang, H., F. Wang, and A. Sun, 2009: Understanding the Ocean Temperature Change in Global warming: the Tropical Pacific. Tellus, 61A(3), 371-380. Zhang, Q., Y. Guan, and *H. Yang, 2008: ENSO Amplitude Change in Observation and Coupled Models. Adv. Atmos. Sci., 25(3), 361-366. *Yang, H., and L. Wang, 2008: Estimating the nonlinear response of tropical ocean to extratropical forcing in a coupled climate model. Geophys. Res. Lett., 35, L15705, doi:10.1029/2008GL034256. *Yang, H., and Q. Zhang, 2008: Anatomizing the Ocean Role in ENSO Changes under Global Warming. J. Climate, doi: 10.1175/2008JCLI2324.1., 21(24), 6539-6555. *Su, J., H. Wang, H. Yang, H. Drange, Y. Gao, and M. Bentsen, 2008: Role of the meridional overturning circulation in the tropical SST changes. J. Climate, 21, 2019-2034. Zhang, Q., *H. Yang, Y. Zhong, and D. Wang, 2005: An Idealized Study of the Impact of Extratropical Climate Change on ENSO. Climate Dynamics, 25, 869-880, doi: 10.1007/s00382-005-0062-z. *Yang, H. and Z. Liu, 2005: Tropical-Extratropical Climate Interaction as Revealed in Idealized Coupled Climate Model Experiments. Climate Dynamics, 24, 863-879, doi: 10.1007/s00382-005-0021-8. *Yang, H., H. Jiang, and B. Tan, 2005: Asymmetric impact of the North and South Pacific on the Equator in a coupled climate model. Geophys. Res. Lett., 32(5), L05604, doi: 10.1029/2004GL021925. *Yang, H., Q. Zhang, Y. Zhong, S. Vavrus, and Z. Liu, 2005: How does Extratropical Warming Affect ENSO? Geophys. Res. Lett., 32(1), L01702, doi: 10.1029/2004GL021624. *Yang, H., Z. Liu and Q. Zhang, 2004: Tropical Ocean Decadal Variability and Resonance of Planetary Wave basin Modes: II. Numerical Study. J. Climate, 17, 1711-1721. *Yang, H., Z. Liu and H. Wang, 2004: Influence of Extratropical Thermal and Wind Forcing on Equatorial Thermocline in an Ocean GCM. J. Phys. Oceanogr., 34(1), 174-187. *Yang, H. and Z. Liu, 2003: Basin Modes in a Tropical-Extratropical Basin. J. Phys. Oceanogr., 33(12), 2751-2763. *Yang, H. and Q.Y. Liu, 2003: Forced Rossby Wave in the Northern South China Sea. Deep Sea Res.(I), 50, 917-926. *杨海军，刘秦玉，2003：缓变风场驱动下正压环流中的多涡结构。热带海洋学报，22(4)，51-59。 *Yang, H. and Q. Zhang, 2003: On the Decadal and Interdecadal variability in the Pacific Ocean. Adv. Atmos. Sci., 20(2), 173-184. *Liu, Z. and H. Yang, 2003: Extratropical Control on Tropical Climate, the Atmospheric Bridge and Oceanic Tunnel. Geophys. Res. Lett., 30(5), 1230, doi: 10.1029/2002GL016492. *Yang, H., Q.Y. Liu, Z. Liu, D.X. Wang and X.B. Liu, 2002: A GCM Study of the Dynamics of the Upper Ocean Circulation of the South China Sea. J. Geophys. Res., 107, 10.1029/2001JC001084. *Liu, Z., H. Yang and Q. Y. Liu, 2001: Regional dynamics of seasonal variability in the South China Sea. J. Phys. Oceanogr., 31(1), 272-284. *Stephens, M., Z. Liu and H. Yang, 2001: Evolution of Subduction Planetary Waves with Application to North Pacific Decadal Thermocline Variability. J. Phys. Oceanogr., 31(7), 1733-1746. *Liu, Q.Y., H. Yang and Z. Liu, 2001: Seasonal Features of the Sverdrup Circulation in the South China Sea. Progress in Natural Sciences, 11(3), 203-206. *刘秦玉，杨海军，贾英来，甘子钧，2001：南海海面高度季节变化的数值模拟。海洋学报，23(2)，9- 17. *刘秦玉，杨海军，鲍洪彤，李薇，2000：北太平洋副热带逆流的气候特征。大气科学，24(3)，363-372. *Liu, Q.Y., H. Yang and Q. Wang, 2000: Dynamic Characteristics of Seasonal Thermocline in the Deep Sea Region of South China Sea. Chinese. J. Oceanol. Limnol., 18(2), 104-109. *刘秦玉，杨海军，李薇，刘倬腾，2000：吕宋海峡上层纬向海流及质量输送。海洋学报，22(2)，1-8. *Liu, Q.Y., H. Yang, W. Li and K. Nishiyama, 2000: Subtropical Countercurrent and Intraseasonal Oscillation in the North Pacific. Proceedings of China-Japan Joint Symposium on Cooperative Study of Subtropical Circulation System. China Ocean Press, 125-134. *Yang, H., Q.Y. Liu and X.J. Jia, 1999: On the Upper Oceanic Heat Budget in the South China Sea: Annual Cycle. Adv. Atmos. Sci., 16(4), 619-629. *Yang, H., Q.Y. Liu and W. Li, 1998: An Influence of Bottom Topography on the Western Boundary Current. Acta Oceanographica Taiwanica, 37(1), 77-88. *杨海军，刘秦玉，1998：南海上层水温分布季节特征。海洋与湖沼，29(5)，501-507. *杨海军，刘秦玉，1998：南海海洋环流研究综述。地球科学进展，13(4)，364-368.

学术兼职

2015年 — 至今，大气与海洋快报（AOSL）英文版，编委 2016年 — 至今，科学通报中文版编委 2018年 — 至今，大气科学进展（AAS）英文版，编委