人物經(jīng)歷
學(xué)習(xí)經(jīng)歷
1982年9月-1985年7月，成都?xì)庀髮W(xué)院 (現(xiàn)成都信息工程大學(xué))氣象系，本科學(xué)習(xí)
1985年9月-1988年9月，中國(guó)科學(xué)院大氣物理研究所，碩士研究生
工作經(jīng)歷
1988年9月-1997年5月，成都?xì)庀髮W(xué)院氣象研究所，副研究員，研究員（1995年）
1997年5月-2002年10月，中國(guó)海洋大學(xué)海洋環(huán)境學(xué)院，教授（期間獲在職博士學(xué)位），博士生導(dǎo)師
2002年10月-2003年10月，加拿大多倫多大學(xué)物理系，訪問(wèn)教授。
2003年10月-2007年10月，中國(guó)海洋大學(xué)海洋環(huán)境學(xué)院，教授，博士生導(dǎo)師
2007年10月-2008年1月，香港城市大學(xué)，訪問(wèn)教授
2008年1月-2010年11月，中國(guó)海洋大學(xué)海洋環(huán)境學(xué)院，教授，博士生導(dǎo)師
2010年11月-至今，中國(guó)科學(xué)院大氣物理研究所，研究員，博士生導(dǎo)師
自1988年以來(lái)，先后承擔(dān)了5個(gè)重大課題（3個(gè)已結(jié)題）的研究，在國(guó)內(nèi)外核心刊物上發(fā)表論文40余篇 ，專(zhuān)著兩部。
研究領(lǐng)域
(1)大氣動(dòng)力學(xué): 阻塞和北大西洋振蕩(NAO)的動(dòng)力學(xué)和觀測(cè)資料研究，風(fēng)暴路徑動(dòng)力學(xué)和觀測(cè)資料研究。
(2)海洋動(dòng)力學(xué)：大洋環(huán)流，中高緯度地區(qū)海洋-大氣年代際相互作用，海洋渦旋的動(dòng)力學(xué)及與大尺度海洋環(huán)流的相互作用。
通過(guò)一定的數(shù)學(xué)技巧巧妙地將行星尺度波與天氣尺度波聯(lián)系起來(lái)，在國(guó)際上提出和建立了大氣阻塞和北大西洋濤動(dòng)(NAO)形成的行星尺度波與天氣尺度波相互作用新的解析理論，并在國(guó)際刊物上發(fā)表了一系列論文(Quart. J. Royal Meteoro. Soc.,2005a, J. Atmos. Sci., 2005b-e,2006, 2007a-c,)，為阻塞和NAO問(wèn)題的解決開(kāi)辟了一個(gè)新的途徑。
他在大氣阻塞和低頻流的動(dòng)力學(xué)方面進(jìn)行了深入的理論研究，提出了局地阻塞形成的包絡(luò)Rossby波理論，在《氣象學(xué)報(bào)》Vo153,No.3《近幾年中國(guó)大氣動(dòng)力學(xué)的主要進(jìn)展》一文中，對(duì)其成果給予了極高的評(píng)價(jià)，文中認(rèn)為“中國(guó)學(xué)者則提出了Rossby孤波理論，既能反映偶極子阻塞的孤波特征，又能顯示偶極子阻塞的哀減機(jī)制（頻散作用），從而較好地解釋了大氣中偶極子阻塞形成過(guò)程和衰退機(jī)制”。
擔(dān)任職務(wù)
以下國(guó)際刊物的審稿人
<<J. Atmos. Sci.>>, <<J. Climate>>, <<Quart. J. Roy. Meteoro. Soc.>>, <<Geophys. Res. Lett.>>, <<J. Geophys. Res.>>等
主持項(xiàng)目
(1) 國(guó)家自然科學(xué)基金項(xiàng)目“北大西洋濤動(dòng)的動(dòng)力學(xué)研究”，2006.1~2008.12 (35萬(wàn))
(2) 國(guó)家杰出青年科學(xué)基金，物理海洋學(xué)，2004.1~2007.12 (100萬(wàn)).
(3) 泰山學(xué)者特聘教授獎(jiǎng)勵(lì)基金，2006.1-2011.12 (50萬(wàn))
國(guó)際論文
(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 Schrödinger 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.
