一、个人简介
葛旭阳，男，1972年6月生，教授，博士生导师。
美国夏威夷大学博士，先后在宾夕法尼亚州立大学/马里兰大学博士后和NOAA/NCEP访问学者，主要从事台风动力学与高影响致灾天气机理及预报研究。主持或参与各类科研与社会服务项目30余项，其中国家级项目10余项；发表核心以上学术论文100篇（其中SCI 60余篇），授权国家发明专利1项。
联系电话：15295739439
E-Mail: xuyang@jou.edu.cn
通讯地址：江苏省连云港市苍梧59号 江苏海洋大学 海洋技术与测绘学院
二、研究方向
台风动力学；高影响致灾天气机理及预报技术；中尺度气象学及数值模拟。
三、教育经历
2002年7月—2008年6月：美国夏威夷大学，气象学，博士
1994年9月—1997年6月：南京气象学院，气象学，硕士
1990年9月—1994年6月：南京气象学院, 天气动力学，本科
四、工作经历
2015年11月—至今：江苏海洋大学，教授，博导
2013年9月—2025年10月：南京信息工程大学，教授，博导
2015年10月—2016年6月：NOAA/NCEP/CPC/ESSIC, 访问学者
2012年6月—2013年9月：夏威夷大学国际太平洋研究中心，博士后
2011年6月—2012年5月：NOAA/NCEP/EMC, UCAR访问学者
2010年10月—2011年5月：美国宾夕法尼亚州立大学，博士后
2008年6月—2010年10月：夏威夷大学国际太平洋研究中心，博士后
1997年7月—2002年6月：上海气候中心，工程师
五、社会兼职
2015年江苏省“六大人才高峰”高层次人才
国家自然科学基金、出版基金评审人
《气象与环境科学》编委 2025-2028
六、代表性科研项目
1. 云-辐射作用影响快速增强台风高层对流非对称性及强度演变机制.上海台风基金重点项目(TFJJ202402). 主持，2024.12-2026.11
2. 复杂环境下登陆热带气旋降雨精细结构特征和机理研究.国自然气象联合基金重点项目(U2342202). 骨干，2024.1-2027.12.
3. 垂直风切变下“非典型”台风强度快速变化的物理机制. 国家自然基金面上项目(42175003)，主持，2022.1-2025.12.
4. 基于气象保障的宁波港船舶调度关键技术提升及应用研究.宁波科技局重大攻关项目. 子课题负责人，2019-2021.
5. 24h警戒区登陆台风精细化和概率预报服务产品子系统：国家气象中心雷达工程. 主持，2019.4-2022.3
6. 重大灾害性天气的短时短期精细化无缝隙预报技术研究. 国家重点研发计划项目(2017YFC1502002), 骨干，2018.1-2022.12.
7. 青藏高原热力强迫影响西北太平洋热带气旋活动的机理研究. 国家自然基金重点项目(41730961)，骨干，2018.1-2022.12.
8. 高空外流特征及其对热带气旋强度与强度变化的影响. 国家自然基金面上项目(41775058)，骨干，2018.1-2021.12.
9. 台风双眼墙结构和强度变化研究. 国家自然基金面上项目( 41575056)，主持，2016.1-2019.12.
10. GRAPES区域集合预报多尺度混合扰动关键技术研究.公益性行业科研专项(201506007-02), 骨干, 2015.1-2017.12
11. 科技部973项目“登陆台风精细结构的观测、预报与影响评估”第3课题：“登陆台风精细化结构演变特征及其机理研究”（2015CB452803）,骨干，2015.1-2019.8
12. “袋鼠”理论在西北太平洋热带气旋生成中的应用研究. 国家自然基金面上项目（41075037）, 骨干，2011/01 – 2013/12
13. 低纬度中层涡旋诱发南海热带气旋形成的机制研究. 国家自然基金面上项目（40875026）, 骨干，2009/01 – 2011/12
七、代表性科研论文
(#学生；*通讯作者)
[1] Wang, W. H#., X. Ge*, M. Peng. 2025: Unusual Tropical Cyclone Tracks associated with Monsoon Gyre near an Isolated High Mountain. Atmospheric Research, 334 (2026) 108761.
[2] Li, H. #, Z Wang, C. Davis; M. Peng; R. McTaggart-Cowan, X. Ge. 2025: Tropical Cyclogenesis under the Influence of an Upper Tropospheric Cold Low in Idealized Numerical Simulations. J. Atmos. Sci., 83(1):105-123.
[3] Lyu, L.Y#., X. GE*, M. Peng. 2025: Dynamic Vortex Initialization for Tropical Cyclone Predictions Utilizing PV-ω Equation and Nudging. Atmospheric Research, 327(2026)108400.
[4] Wang, W. H#., M. Peng, X. GE*, M. Chen. 2025: Decadal variations of rapid intensification tropical cyclone ratios in the Northwest Pacific during autumn. Climate Dynamics. 63:253. DOI: 10.1007/s00382-025-07732-6.
[5] Zhang, J., Li, Q., Wu, L., Qian, Q., Ge, X., et al., 2025: Influence of Inner-core Symmetry on Tropical Cyclone Rapid Intensification and its Forecasting by a Machine Learning Ensemble Model. Weather and Climate Extremes.48, https://doi.org/10.1016/j.wace.2025.100770.
[6] Li, H#, X. Ge*, M. Peng, Z. Wang. 2024: Impacts of an Upper-Tropospheric Cold Low on Tropical Cyclone Intensity. Mon. Wea. Rev.,152(12):2661-2677.
[7] Ling, J. W.#, X. Ge*, M. Peng, Q. Huang#, 2024: Thermodynamical impacts on the boundary layer imbalance during secondary eyewall formation. Atmospheric Research, 310 (2024) 107610
[8] He, L. K., Q. L. Li, L. Wu, X. Ge, and et al., 2024: The impact of monsoon on the landfalling tropical cyclone persistent precipitation in South China. Environmental Research Letters. 19 (2024)084003.
[9] Lai, Z. Y., Y. S. Zhou, X. Ge, et al., 2024: Comparison of kinetic energy conversion characteristics of two extreme precipitation episodes during persistent unusually heavy rainfall on 17-23 July 2021 in Henan, China. Atmos. Res., 309(2024)107546. https://doi.org/10.1016/j.atmosres.2024.107546
[10] Li, H#, Z. Yan#, M. Peng, X. Ge*, Z. Wang, 2024: Unusual Tropical cyclone Tracks under the Influence of Upper Tropospheric Cold Low. Mon. Wea. Rev.,152(1):39-58. DOI: 10.1175/MWR-D-23-0074.1
[11] Ling, J. W.#, X. Ge*, M. Peng, Q. Huang#, 2023：Modulation of high-latitude tropical cyclone recurvature by solar radiation. Journal of Meteorological Research, 37(6): 802-811.
[12] Huang, Q. J.#, X. GE*, 2023: Sensitivity of Tropical Cyclone Development to the Vortex Size under Vertical Wind Shear. JGR-atmosphere, 128, e2023JD038802. https://doi.org/10.1029/2023JD038802.
[13] Deng, Z. R. #, S.W. Zhou*, X. Ge*, Y. Qing, Y. Cheng. 2023: An Interdecadal Change in the Relationship between Summer Arctic Oscillation and Surface Air Temperature on the eastern Tibetan Plateau around the late 1990s. Climate Dynamics. DOI: 10.1007/s00382-023-06899-0
[14] Yan, Z. Y. #, Z. Wang, M. Peng, and X. Ge. 2023: Polar Low Motion and Track Characteristics over the North Atlantic. J. Climate, 36(7):4550-4569. https://doi.org/10.1175/JCLI-D-22-0547.1.
[15] Du, X. G., H. S. Chen, Q. Q. Li, and X. Ge, 2023: Urban Impact on Landfalling Tropical Cyclone Precipitation: A Numerical Study of Typhoon Rumbia (2018). Adv. Atm. Sci. 40:1-17.
[16] Bi, M. Y., R. Wang, T. Li, and X. GE, 2023: Effects of vertical shear on tropical cyclones with different initial sizes. Frontiers in Earth Science. 11:1106204. doi: 10.3389/feart.2023.1106204.
[17] Huang Q. J. #, B.Y. Guo#, X. Ge*. 2022: Simulations of multiple Tropical cyclones event associated with the monsoon trough over the western North Pacific. Meteorological Applications, 29(6), e2104. https://doi.org/10.1002/met.2104.
[18] Li, H.#, X. Ge*, M. Peng, and L. Li, 2022: The influences of Monsoon Trough on the relative motion of Binary Tropical Cyclones. J. Meteor. Soc. Japan, 100(5):729–749, doi:10.2151/jmsj.2022-038.
[19] Huang, Q. J.#, X. GE*, M. Peng, and Z. R. Deng, 2022: Sensitivity analysis of the super heavy rainfall event in Henan on 20 July (2021) using ECMWF ensemble forecasts. J. Tropical Meteorology, 28(3): 308-325.
[20] Yu. H., C. Wang, X. Ge#. 2022: Modulation of Pacific Sea surface temperatures on the late-season typhoon tracks and its implication for seasonal forecasting. Frontiers in Earth Science. DOI:10.3389/feart.2022.835001.
[21] Huang, Q. J.#, X. Ge*, and M. Bi. 2022. Simulation of Rapid intensification of super Typhoon Lekima (2019). Part II: The critical role of cloud-radiation interaction of asymmetric convection. Frontiers in Earth Science. DOI: 10.3389/feart.2021.832670.
[22] Lu, C. H., X. GE*, M. Peng, and T. Li. 2022: Influence of El Niño decaying pace on low latitude tropical cyclogenesis over the western North Pacific. Int. J. Climatology, 1-11. https://doi.org/10.1002/joc.7288
[23] Huang, Q. J. #, X. Ge*, M. Peng, 2021: Simulation of Rapid Intensification of Super Typhoon Lekima (2019). Part I: Evolution characteristics of asymmetric convection under Upper-Level Vertical Shear. Frontiers in Earth Science. 9:739507. doi: 10.3389/feart.2021.739507
[24] Lu, C. H., X. GE*, and M. Peng 2021: Comparison of Controlling Parameters for the Formation of Near-Equatorial Tropical Cyclone between Western North Pacific and North Atlantic. Journal of Meteorological Research. 35(4): 623-634. doi: 10.1007/s13351-021-0208-x.
[25] He, J. X., Ma, X. Ge, et al. 2021: Variational Quality Control of Non-Gaussian Innovations in the GRAPES m3DVAR Model: Part II. Mass Field Evaluation of Conventional Observational Assimilation. Adv. Atmos. Sci., 38(6): 1510–1524.
[26] Yan, Z. Y. #, X. Ge*, Z. Wang, C. C. Wu, and M. Peng. 2021: Understanding the impacts of upper-tropospheric cold low on typhoon Jongdari (2018) using Piecewise potential vorticity inversion. Mon. Wea. Rev., 149(5):1499-1515.
[27] Li L.#, and X. Ge*, 2021: Intensity change of tropical cyclone Noru (2017) during binary interaction. Asian-Pacific Journal of Atmospheric Science, 57(1):135–147.
[28] Huang, Q. J.#, X. Ge*, M. Peng, 2020: Impacts of upper easterly wave on the sudden track change of Typhoon Megi (2010). J. Meteor. Soc. Japan., 98(6), 1335-1352.
[29] Shi, D. L. #, X. Ge*, and M. Peng, T. Li, 2019: Characterization of tropical cyclone rapid intensification under two types of El Niño events in the Western North Pacific. Int. J. Climatology, DOI: 10.1002/joc.6338
[30] Shi, D. L. #, X. Ge*, and M. Peng, 2019: Latitudinal Dependence of Dry Air Effect on Tropical Cyclone Intensification. Dynamics of Atmospheres and Oceans, 87, 1-15.
[31] Yan Z. Y. #, X. Ge*, M. S. Peng, and T. Li, 2019. Does Monsoon Gyre always favor Tropical Cyclone Rapid Intensification? Q. J. R. Meteor. Soc., 1-13. DOI: 10.1002/qj.3586.
[32] Cai, M., Y. Q. Wang*, and X. Ge, 2019: Simulated Spiral Rainbands in Typhoon Chanchu (2006): Model verification and Fine Rainband Structures. J. Tropical Meteorology, 25(2): 141-152.
[33] Ge, X.*, and D. L. Shi#, 2019: The Mid-latitudinal influences on the formation of the monsoon gyre in August 1991. Dynamics of Atmospheres and Oceans, 86，52-62.
[34] Guo, B.Y.#, and X. Ge*, 2018: Monsoon Trough Influences on Multiple Tropical Cyclone Events in the western North Pacific. Atmos. Sci. Lett., e851. https://doi.org/10.1002/asl.851.
[35] Ge, X*, Z. Yan#, M. S. Peng, M. Bi, and T. Li, 2018. Sensitivity of Tropical Cyclone Track to the vertical structure of a nearby Monsoon Gyre. J. Atmos. Sci., 75(6), 2017-2028.
[36] Ge, X.*, D. L. Shi#, and L. Guan#, 2018. Monthly variation of tropical cyclone rapid intensification ratio in the western North Pacific. Atmos. Sci. Lett., 19 (4):1-6. https://doi.org/10.1002/asl.814.
[37] Ge, X.*, L. Guan#, and Z. Yan#, 2018: Impacts of Raindrop Evaporation on Tropical Cyclone Secondary Eyewall Formation. Dynamics of Atmospheres and Oceans, 82, 54-63.
[38] Guan, L#., and X. Ge*, 2018: How does tropical cyclone initial size affect the secondary eyewall formation? J. Meteor. Res., 31(1): 124-134.
[39] Bi, M., X. Ge*, and T. Li, 2018: Dependence of tropical cyclone intensification on the latitude under vertical shear. J. Meteor. Res., 32(1): 113-123, 10.1007/s13351-018-7055-4.
[40] Yan, Z. #, X. Ge*, and B.Y. Guo#, 2017: Simulated sensitivity of tropical cyclone track to the moisture in an idealized monsoon gyre. Dynamics of Atmospheres and Oceans, 80(12), 173-182.
[41] Ma, X., J. He, and X. Ge*, 2017: Simulated sensitivity of tropical cyclone eyewall replacement cycle to the ambient temperature profile. Adv. Atmos. Sci., 34(9), 1047 -1056.
[42] Ge, X, W. Wang*, A. Kumar, and Y. Zhang, 2017: Importance of the vertical resolution in simulating SST diurnal and intra-seasonal variability in an oceanic general circulation model. J. Climate, 30(11), 3963-3978.
[43] Ge, X*, and L. Guan#, S. W. Zhou. 2016: Impacts of initial structure of tropical cyclone on secondary eyewall formation. Atmos. Sci. Lett., 17，569-574.
[44] Zhou, S. W., Y. Ma#, and X. Ge*, 2016: Impacts of diurnal cycle of solar radiation on spiral rainbands. Adv. Atmos. Sci., 33(9), 1085–1095.
[45] Xu, M. T#, S. Zhou., and X. Ge*, 2016: An idealized simulation study of the impact of monsoon gyre on tropical cyclogenesis. Acta Meteorologic Sinica, 74(5), 81-91.
[46] Ge, X.*, W. Xu#, S.W. Zhou, 2015: Sensitivity of tropical cyclone intensification on initial inner-core structure. Adv. Atmos. Sci., 32(10), 1407-1418.
[47] Ge, X.*, Y. Ma#, S.W. Zhou, and T. Li, 2015: Sensitivity of tropical cyclone warm-core on the solar radiation. Adv. Atmos. Sci., 32(8), 1038-1048.
[48] Ge, X.*, 2015: The impacts of environmental humidity on concentric eyewall structure. Atmos. Sci. Lett., 16, 273-278.
[49] Ge, X.*, Y. Ma#, S.W. Zhou, and T. Li, 2014: The impacts of diurnal cycle of radiation on tropical cyclone intensification and structure. Adv. Atmos. Sci., 31(6), 1377–1385.
[50] Ge, X., T. Li, and M. S. Peng, 2013: Effects of vertical shears and mid-level dry air on tropical cyclone developments. J. Atmos. Sci., 70(12), 3859-3875.
[51] Ge, X., T. Li, and M. S. Peng, 2013: Tropical cyclone genesis efficiency: mid-level versus bottom vortex. J. Tropical Meteorology, 19 (3), 197-213.
[52] Li, T., X. Ge, M. S. Peng, and W. Wang, 2012: Dependence of tropical cyclone intensification on the Coriolis parameter. Tropical Cyclone Research and Review, 1(2), 242-253.
[53] Zhang, S. J., T. Li, X. Ge, M. S. Peng, and N. Pan, 2012: A 3DVAR-based Dynamical Initialization Scheme for Tropical Cyclone Predictions. Weather forecasting, 27,473-483.
[54] Liang J., L. Wu, X. Ge, and C.-C. Wu, 2011: Monsoonal Influence on Typhoon Morakot (2009). Part II: Numerical Study. J. Atmos. Sci., 68, 2222–2235.
[55] Hendricks, E. A., M. S. Peng, X. Ge, and T. Li, 2011: Performance of a Dynamic Initialization Scheme in the Coupled Ocean/Atmosphere Mesoscale Prediction System for Tropical Cyclones (COAMPS-TC), Wea. Forecasting, 26, 650–663
[56] Zhou, X. Q., B. Wang, X. Ge, and T. Li, 2011: Response of Tropical Cyclone Intensity to Secondary Eyewall Heating. J. Atmos. Sci., 68, 450–456.
[57] Ge, X., T. Li, S. Zhang, and M. S. Peng, 2010: What causes the extremely heavy rainfall in Taiwan during Typhoon Morakot (2009)? Atmos. Res. Lett., 11, 46–50.
[58] Ge, X., T. Li, and M. Peng, 2010: Cyclogenesis simulations of Typhoon Prapiroon (2000) associated with Rossby wave energy dispersion. Mon. Wea. Rev., 138, 42–54.
[59] Peng, J., M. S. Peng, T. Li, and X. Ge, 2009: Barotropic instability in the tropical cyclone outer region. Q. J. R. Meteor. Soc., 135, 851 – 864.
[60] Ge, X., T. Li, Y. Wang, and M. S. Peng, 2008: Tropical cyclone energy dispersion in a three-dimensional primitive equation model: Upper tropospheric influence. J. Atmos. Sci., 65, 2272–2289.
[61] Ge, X., T. Li., and X. Zhou, 2007: Tropical cyclone energy dispersion under vertical shears. Geophys. Res. Lett., 34, L23807, doi:10.1029/2007GL031867.
[62] Li, T., X. Ge, B. Wang, and Y. Zhu, 2006: Tropical cyclogenesis associated with Rossby wave energy dispersion of a pre-existing typhoon. Part II: Numerical simulations. J. Atmos. Sci., 63, 1390–1409.
[63] Li, T., B. Fu, X. Ge, B. Wang, and M. S. Peng, 2003: Satellite data analysis and numerical simulation of tropical cyclone formation. Geophys. Res. Lett., 30, 2122, doi:10.1029/2003GL018556.
八、代表性专利
[1] 一种台风涡旋初始化方法及系统.发明专利号(202510245917.6)
