标题：罗德海
教育及工作经历
1985年7月毕业于成都气象学院气象系[1]
1988年9月在中国科学院大气物理研究所获硕士学位
2002年10月至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
现为中国科学院大气物理研究所研究员、中国海洋大学博导。
自1988年以来，先后承担了5个重大课题（3个已结题）的研究，在国内外核心刊物上发表论文40余篇 ，专著两部。　
获得的荣誉
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。
主要研究领域
(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。
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,)，为阻塞和NAO问题的解决开辟了一个新的途径。
他在大气阻塞和低频流的动力学方面进行了深入的理论研究，提出了局地阻塞形成的包络Rossby波理论，在《气象学报》Vo153,No.3《近几年中国大气动力学的主要进展》一文中，对其成果给予了极高的评价，文中认为“中国学者则提出了Rossby孤波理论，既能反映偶极子阻塞的孤波特征，又能显示偶极子阻塞的哀减机制（频散作用），从而较好地解释了大气中偶极子阻塞形成过程和衰退机制”。
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)
国际论文
(28)D. Luoand 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. Diaoand 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 andD. 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
(22) Wang, Y., S. Li, andD. 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. Luoand T. Gong, 2006c: A possible mechanism for the eastward shift of interannual NAOaction centers in last three decades.Geophy. Res. Lett., 33, L24815, doi:10.1029 /2006G L027860.
(14)D. Luoand 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 andD. Luo,2006a: A new blocking index and its application: Blocking action in the Northern Hemisphere,J. Climate, 19, 4819-4839.
(12)D. Luoand 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 Schr&ouml;dinger equation for weakly nonlinear Rossby waves,Wave Motion,33,339-347..
(3)D. Luoand 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.