作者:聚创中国海大考研网-小厦老师 点击量: 293 发布时间: 2012-11-17 09:08 【微信号:扫码加咨询】
罗德海,男, 1963年11月生,博士,教授,博士生导师
现主要从事海洋-大气动力学和气候动力学的教学和研究工作,在国内外刊物上发表论文数十篇,专著两部. 通过一定的数学技巧巧妙地将行星尺度波与天气尺度波联系起来,在国际上创造性地提出和建立了大气阻塞和北大西洋涛动(NAO)形成的行星尺度波与天气尺度波相互作用新的解析理论,并在国际顶尖刊物上发表了一系列论文(Quart. J. Royal Meteoro. Soc.,2005a, J. Atmos. Sci., 2005b-e,2006, 2007a-c,, 2008a-b,2010a-b)为阻塞和NAO问题的解决开辟了一个新的途径。
获得的奖励和荣誉:
1996年第五届中国青年科技奖,
2000年第二届教育部青年教师奖.
2000年国家政府津贴获得者,青岛市拔尖人才
2003年山东省高等学校学科带头人
2003年国家杰出青年科学基金获得者。
2005年 山东省泰山学者特聘教授
国内外进修情况:
2002年10月~2003年10月在加拿大多伦多大学合作研究一年。
2007年10月-2008年1月在香港城市大学合作研究3个月
已主持和现主持的基金项目:
(1) 国家自然科学基金项目“北大西洋涛动的动力学研究”,2006.1~2008.12 (35万)
(2) 国家杰出青年科学基金,物理海洋学,2004.1~2007.12 (100万).
(3) 泰山学者特聘教授奖励基金,2006.1-2011.12 (50万)
主要的研究领域:
(1)大气动力学: 阻塞和北大西洋振荡(NAO)的动力学和观测资料研究,风暴路径动力学和观测资料研究。
(2)海洋动力学:大洋环流,中高纬度地区海洋-大气年代际相互作用,海洋涡旋的动力学及与大尺度海洋环流的相互作用。
主要的科研合作者:
(1) 穆穆院士(杰出基金获得者), 中国科学院大气物理研究所
(2) 李建平研究员(杰出基金获得者), 中国科学院大气物理研究所
(3) 马柱国研究员, 中国科学院大气物理研究所
(4) Anthony R. Lupo教授,美国密苏苏里(Missouri)大学土壤,环境和大气科学系。
(5) Steven, Feldstein教授,美国宾州(Pennsylvannia state)大学气象系.
(6) 李双林研究员(百人计划) ,中国科学院大气物理研究所
部分代表性国际论文(SCI):
(28) D. Luo and S. Ren, 2010: Different impact of the SST-wind stress coupling on the baroclinic instability of ocean currents inside and outside the SST frontal zone (submitted).
(27) D. Luo, Y. Diao and S. B. Feldstein, 2010: The variability of the Atlantic storm track activity and the phase transition of North Atlantic Oscillations: A link between intraseasonal and interannual variability (submitted)
(26) D. Luo, L. Zhong, R. Ren and C. Wang, 2010b: Spatial pattern and zonal shift of the North Atlantic Oscillation. Part II: Numerical experiments. J. Atmos. Sci. (accepted).
(25) D. Luo, Z. Zhu, R. Ren, L. Zhong and C. Wang, 2010a: Spatial pattern and zonal shift of the North Atlantic Oscillation. Part I: A dynamical interpretation. J. Atmos. Sci. (accepted).(24), T. Gong, S. B. Feldstein and D. Luo, 2010: The impact of ENSO on wave breaking and Southern annular mode events. J. Atmos. Sci. (accepted)
(23) D. Luo, W. Zhou, and K. Wei, 2010: Dynamics of eddy-driven North Atlantic Oscillations in a localized shifting jet: zonal structure and downstream blocking, Climate dynamics,34, 73-100. DOI 10.1007/s00382-009-0559-y.
(22) Wang, Y., S. Li, and D. Luo, 2009, Seasonal response of Asian monsoonal climate to the Atlantic Multidecadal Oscillation, J. Geophys. Res., 114, D02112, doi:10.1029/2008JD010929(21) D. Luo, T. Gong and L. Zhong, 2008b: Dynamical relationship between the phase of North Atlantic Oscillations and meridional excursion of a preexisting jet: An analytical study. J. Atmos. Sci., 65, 1838-1858
(20)D. Luo, T. Gong and Y. Diao, 2008a: Dynamics of eddy-driven low-frequency dipole modes. Part IV: Planetary and synoptic wave breaking processes during the NAO life cycle. J. Atmos. Sci., 65, 737-765.
(19) D. Luo, T. Gong , Y. Diao and W. Zhou, 2007: Storm tracks and Annular Modes. Geophys. Res. Lett.., 34, L1780110.1029/2007GL030436.(18) D. Luo, T. Gong and Y. Diao, 2007c: Dynamics of eddy-driven low-frequency dipole modes. Part III: Meridional shifts of westerly jet anomalies during two phases of NAO. J. Atmos. Sci. 64,3232-3243.
(17)D. Luo, T. Gong and A., R. Lupo, 2007b: Dynamics of eddy-driven low- frequency dipole modes. Part II: Free mode characteristics of NAO and diagnostic study. J. Atmos. Sci., 64, 29-51.
(16)D. Luo, A., R. Lupo and H. Wan, 2007a: Dynamics of eddy-driven low- frequency dipole modes. Part I: A simple model of North Atlantic Oscillations. J. Atmos. Sci., 64, 3-28.
(15) D. Luo and T. Gong, 2006c: A possible mechanism for the eastward shift of interannual NAO action centers in last three decades. Geophy. Res. Lett., 33, L24815, doi:10.1029 /2006G L027860.
(14)D. Luo and Z. Chen, 2006b: The role of land-sea topography in blocking formation in a block-eddy interaction model, J. Atmos. Sci.,63,3056-3065.
(13) Y. Diao, J. Li and D. Luo, 2006a: A new blocking index and its application: Blocking action in the Northern Hemisphere, J. Climate, 19, 4819-4839.
(12) D. Luo and H. Wan, 2005g: Decadal variability of wintertime North Atlantic and Pacific blockings: A possible cause, Geophys. Res. Lett., 32, L23810, doi: 10. 1029/2005GL024329.
(11) D. Luo, 2005f: Why is the North Atlantic block more frequent and long-lived during the negative NAO phase, Geophys. Res. Lett., 32, L20804,doi:10, 1029/ 2005GL022927.
(10) D. Luo, 2005e: A barotropic envelope Rossby soliton model for block-eddy interaction. Part IV: Block activity and its linkage with sheared environment, J. Atmos. Sci. 62, 3860-3884(9) D. Luo, 2005d: A barotropic envelope Rossby soliton model for block-eddy interaction. Part III: Wavenumber conservation theorems for isolated blocks and deformed eddies, J. Atmos. Sci., 62, 3839-3859(8) D. Luo, 2005c: A barotropic envelope Rossby soliton model for block-eddy interaction. Part II: Role of westward-traveling planetary waves, J. Atmos. Sci., 62, 22-40.
(7) D. Luo, 2005b: A barotropic envelope Rossby soliton model for block-eddy interaction. Part I: Effect of topography, J. Atmos. Sci., 62,5-21.
(6) D. Luo, 2005a: Interaction between envelope soliton vortex pair block and synoptic-scale eddies in an inhomogeneous baroclinicity environment, Quart. J. Roy. Meteoro. Soc. ,131, 125-154.
(5) D. Luo, Huang F. and Y. Diao, 2001: Interaction between antecedent planetary- scale envelope soliton blocking anticyclone and synoptic-scale eddies: Observations and theory. J. Geophys. Res. Vol. 106, 31795—31816.
(4) D. Luo, 2001: Derivation of a higher order nonlinear Schrödinger equation for weakly nonlinear Rossby waves, Wave Motion, 33,339-347..
(3) D. Luo and Y. Lu, 2000: The influence of negative viscosity on wind-driven ocean circulation in a subtropical basin, J. Phys. Ocean.,30,916-932 .
(2) D. Luo, 2000: Planetary-scale baroclinic envelope Rossby solitons in a two- layer model and their interaction with synoptic-scale eddies. Dyn. Atmos. Oceans, 32, 27-74.
(1) D. Luo, 1999, Near-resonantly topographically forced envelope Rossby solitons in a barotropic flow. Geophys. Astrophys. Fluid Dyn., 90, 161-188.
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