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实验室固定成员

 

    

    罗德海,男,1963年生,博士,研究员(二级),博士生导师

    现主要从事大气动力学,海洋动力学和气候动力学的研究工作,

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模式,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-b2010a-b)为阻塞和NAO问题的解决开辟了一个

新的途径。

    

    同时利用我们的理论模式理论上证明在强的大西洋storm trackCO2增多)强迫作用下,NAO能从正位相转换成负位相,从而使CO2所引起北半球的增暖能得到部分抑制(J. Atmos. Sci., 2011)

 

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国家政府津贴获得者,青岛市拔尖人才

2003山东省高等学校学科带头人

2003国家杰出青年科学基金获得者

2005山东省泰山学者特聘教授

 

学习和工作经历:

19829-19857月,成都气象学院 (现成都信息工程学院)气象系,本科学习

19859-19889月,中国科学院大气物理研究所,硕士研究生

19889-19975月,成都气象学院气象研究所,副研究员,研究员(1995年)

19975-200210月,中国海洋大学海洋环境学院,教授(期间获在职博士学位),博士生导师

200210-200310月,加拿大多伦多大学物理系,访问教授。

200310-200710月,中国海洋大学海洋环境学院,教授,博士生导师

200710-20081月,香港城市大学,访问教授

20081-201011月,中国海洋大学海洋环境学院,教授,博士生导师

201011-至今,中国科学院大气物理研究所,研究员,博士生导师

 

现主持的基金项目:

国家自然科学基金项目尺度相互作用与中高纬度地区大气低频模态的动力学

20111-201312月(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。

 

学术团体兼职:

<<气象学报>>编委, <<中国科学-地球科学>>编委

 

以下国际刊物的审稿人:

<<J. Atmos. Sci.>>, <<J. Climate>>, <<Quart. J. Roy. Meteoro. Soc.>>, <<Geophys. Res. Lett.>>,

<<J. Geophys. Res.>>等。

 

1999年后部分代表性国际论文(SCI):

(35) D. Luo, Y. Yao, S. Feldstein and S. Lee, 2012: Regime transition of the North Atlantic Oscillation and

        extreme cold events over Europe: The winter of 2011/2012.

(34) D. Luo and S. Ren, 2012: Impact of the SST-wind stress coupling on thedynamics and stability of ocean

        current inside and outside SST frontal zones, Dyn. Atmos. Oceans (in revision)

(33) Jiang, Z., M. Mu and D. Luo, 2012: Dynamics of North Atlantic Oscillations identified by using the

        conditional nonlinear optimal perturbation method. J. Atmos. Sci. (in revision)

(32) T. Gong, S. Feldstein and D. Luo, 2012: A simple GCM model study on the relationship between ENSO

        and the Southern Annular Mode. J. Atmos. Sci. (submitted)

(31) D. Luo, J. Cha, S. Lee and S. Feldstein, 2012: The North Atlantic Oscillation and the North Atlantic jet

        variability: A dynamical link. J. Atmos. Sci. (submitted)

(30) D. Luo, and J. Cha, 2012: The North Atlantic Oscillation and the North Atlantic jet variability:

        Precursors to NAO regimes and transitions. J. Atmos. Sci. (in revision)

(29) D. Luo, J. Cha and S. Feldstein, 2012b: Weather regime transitions and the interannual variability of

        the North Atlantic Oscillation. Part II: Dynamical processes. J. Atmos. Sci. (in press)

(28) D. Luo, J. Cha and S. Feldstein, 2012a: Weather regime transitions and the interannual variability of

        the North Atlantic Oscillation. Part I: A likely connection. J. Atmos. Sci. (in press)

(27) D. Luo, Y. Diaoand S. B. Feldstein,2011:  The variability of the Atlantic storm track activity and North

        Atlantic Oscillations: A link between intraseasonal and interannual variability, J. Atmos. Sci., 68,

        577-601.

(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., 67, 2827-2853

(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., 67, 2805-2826.

(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.,67, 2854-2870

(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. 643232-3243.

(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 NAOaction

        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.633056-3065.

(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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