留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名
邮箱
手机号码
标题
留言内容
验证码

IPCC AR4 模式对热带气旋热力控制因子的模拟评估

余锦华 唐盛 吴立广 施能

余锦华, 唐盛, 吴立广, 施能. IPCC AR4 模式对热带气旋热力控制因子的模拟评估[J]. 海洋学报, 2011, 33(6): 39-54.
引用本文: 余锦华, 唐盛, 吴立广, 施能. IPCC AR4 模式对热带气旋热力控制因子的模拟评估[J]. 海洋学报, 2011, 33(6): 39-54.
YU Jin-hua, TANG Sheng, WU Li-guang, SHI Neng. Assessments on simulation of thermodynamic parameters of tropical cyclone in IPCC-AR4 Models[J]. Haiyang Xuebao, 2011, 33(6): 39-54.
Citation: YU Jin-hua, TANG Sheng, WU Li-guang, SHI Neng. Assessments on simulation of thermodynamic parameters of tropical cyclone in IPCC-AR4 Models[J]. Haiyang Xuebao, 2011, 33(6): 39-54.

IPCC AR4 模式对热带气旋热力控制因子的模拟评估

基金项目: 公益性行业(气象)科研专项(GYHY200806009);"973"项目(2009CB421503);国家自然科学基金(40775060)。

Assessments on simulation of thermodynamic parameters of tropical cyclone in IPCC-AR4 Models

  • 摘要: 海平面温度是影响热带气旋活动重要的大尺度环境热力控制因子,根据1948-1999年热带地区(30°S-30°N)海平面温度(SST)的气候场、线性趋势、年代际变化与年际变化的空间结构特征,分别就24个IPCC AR4模式的模拟性能进行评估。结果表明,虽然24个IPCC AR4模式对SST气候场的模拟性能都比较好,但大部分模式输出的SST系统性偏低于观测分析场(ERSST)。所有模式热带区域平均SST都表现出与ERSST相一致的增暖趋势,但各模式与ERSST的这一趋势强度差异明显。综合考虑SST线性趋势及年代际变化的空间结构,24个IPCC AR4模式中,有6个模式的模拟性能较差,其空间型态与ERSST相差很大,不应作为模式集成的对象,它们是INM CM3_0, MRI_CGCM2, INGV_ECHAM4,UKMO_HADCM3,NCAR_PCM1,MPI_ECHAM5。前5个空间型态与ERSST最接近的模式依次是:CGCM3.1_T47,GISS ER,MIROC_HIRES,GFDL CM2_1,GFDL CM2_0。对西北太平洋、北大西洋以及南海地区6~10月热带气旋主要活动海域SST进行了评估,相对来说,模式对北大西洋和南海海域SST不论是线性趋势还是年代际变化的模拟都好于西北太平洋。北大西洋有18个模式年代际序列与ERSST的相关较高。在西北太平洋,UKMO_HADGEM1和MPI_ECHAM5的年际变化序列与ERSST的相关达到0.05的显著性水平;在南海,年际变化模拟最好的模式是UKMO_HADCM3。
  • YU J-H, WANG Y. Response of tropical cyclone potential intensity over the north Indian Ocean to global warming[J]. Geophys Res Lett, 2009, 36:L03709, doi: 10.1029/2008GL036742.
    EMANUEL K A, SUNDARAJAN R, WILLIAMS J. Hurricane and global warming: Results from downscaling IPCC AR4 simulations[J]. Bull Amer Meteor Soc, 2008,89:347-367.
    KNUTSON T R, SIRUTIS J J, GARMNER S T, et al. Simulated reduction in Atlantic hurricane frequency under twenty-first-century warming conditions[J]. Nature Geoscience, 2008,doi: 10.1038/ngeo202.
    MEEHL G A, COVEY C, DELWORTH T, et al. THE WCRP CMIP3 multimodel dataset: A new era in climate change research[J]. Bull Amer Meteor Soc, 2007,88: 1383-1394.
    SZOEKE S P , XIE S P. The tropical eastern Pacific seasonal cycle: Assessment of errors and mechanisms in IPCC AR4 coupled ocean atmosphere general circulation models[J]. J Clim, 2008, 21: 2573-2590.
    CAI W, COWAN T. Trends in Southern Hemisphere Circulation in IPCC AR4 Models over 1950-99: Ozone depletion versus greenhouse forcing[J].J Clim, 2007,20:681-693.
    CAI W, SULLIVAN A, COWAN T. How rare are the 2006-2008 positive Indian Ocean Dipole events? An IPCC AR4 climate model perspective[J]. Geophy Res Lett, 2009,36: L08702, doi: 10.1029/2009GL037982.
    LIN J, KILADIS G N, MAPES B E,et al. Tropical intraseasonal variability in 14 IPCC AR4 Climate Models. Part Ⅰ: Convective Signals[J]. J Clim, 2006, 19: 2665-2690.
    ACHUTARAO K, SSERBER K R. Simulation of the El Niño Southern Oscillation: Results from the Coupled Model Inter comparison Project[J]. Clim Dyn, 2002,19:191-209.
    ACHUTARAO K, SPERBER K R. ENSO simulation in coupled ocean-atmosphere models: are the current models better? [J]. Clim Dyn, 2006,27: 1-15.
    SUN Y, DING Y-H.An assessment on the performance of IPCC AR4 climate models in simulating interdecadal variations of the East Asian summer monsoon[J].Acta Meteorogica Sinica, 2008,22: 472-488.
    AIGUO D, MEEHL G A, WASHINGTON W M. Climate changes in the 21st Century over the Asia-Pacific region simulated by the NCAR CSM and PCM[J].Advances in Atmospheric Sciences, 2001: 18:639-658.
    KRIPALANI R H, OH J H, CHAUDHARI H S. Response of the East Asian summer monsoon to doubled atmospheric CO2: Coupled climate model simulations and projections under IPCC AR4[J]. Theor Appl Climatol, 2007, 87: 1-28.
    KRRIPALANI R H, OH J H, KULKARNI A,et al. South Asian summer monsoon precipitation variability: Coupled climate model simulations and projections under IPCC AR4[J]. Theor Appl Climatol, 2007, 90: 133-159.
    祝亚丽,王会军. 基于IPCC AR4耦合模式的南极涛动和北极涛动的模拟及未来变化预估[J].气象学报,2008,66(6):993-1004.
    蔡怡 ,王彰贵, 乔方利.全球变暖背景下最近40 a太平洋海温变化数值模拟[J].海洋学报,2008,30(5):9-16.
    MALKUS B S, RIEHL H. On the dynamics and energy transformation in steady-state hurricanes[J]. Tellus, 1960, 12: 1-20.
    SCHADE L R. Tropical cyclone intensity and sea surface temperature[J]. J Atmos Sci, 2000, 57: 3122-3130.
    SAUNDERS M A,HARRIS A R. Statistical evidence links of exceptional 1995 Atlantic hurricane season to record sea warming[J]. Geophys Res Lett, 1997, 24: 1255-1258.
    EMANUEL K A. The dependence of hurricane intensity on climate[J]. Nature, 1987,42: 483-485.
    EMANUEL K A. Thermodynamic control of hurricane intensity[J]. Nature, 1999,401: 665-669.
    HOLLAND G J. The maximum potential intensity of tropical cyclones[J]. J Atmos Sci, 1997,54: 2519-2541.
    HENDERSON-SELLERS A, co-authors. Tropical cyclones and global climate change: A POST-IPCC assessment[J]. Bull Amer Meteor Soc, 1998,79: 19-38.
    LATIF M, KEENLYSIDE N,BADER J. Tropical sea surface temperature, vertical shear, and hurricane development[J]. Geophy Res Lett, 2007,34: L01710, doi: 10.1029/2006GL027969.
    GOLDENBERG S B, SHAPIRO L J. Physical mechanisms for the association of El Niño and West African rainfall with Atlantic major hurricane activity [J]. J Clim, 1996, 9: 1169-1187.
    GOLDENBERG S B, LANDSEA C W,MESTAS-NUNEZ A M,et al. The Recent increase in Atlantic hurricane activity: causes and implications[J]. Science, 2001,293: 474-479.
    VECCHI G A,SODEN B J. Increased tropical Atlantic wind shear in model projections of global warming[J]. Geophys. Res. Lett., 2007,34, L08702, doi: 10.1029/2006GL028905.
    SOBEL A H, HELD I M. The ENSO signal in tropical tropospheric temperature[J]. J Clim, 2002, 15: 2702-2706.
    SHEN W, TULEYA R E,GINIS I. A sensitivity study of thermodynamic environment on GFDL model hurricane intensity: Implications for global warming[J]. J Clim, 2000, 1 3: 109-121.
    TANG B, NEELIN J. ENSO Influence on Atlantic hurricanes via tropospheric warming[J]. Geophys Res Lett, 2004, 31, L24204, doi: 10.1029/2004GL021072.
    SMITH T M , REYNOLDS R W. Improved extended reconstruction of SST (1954-1997)[J]. J Clim, 2004,17: 2466-2477.
    CAMARGO S J , SOBEL A H. Western North Pacific tropical cyclone intensity and ENSO[J]. J Clim, 2005,18(15):2996-3006.
    STATOSHI L, MATSUURA T. ENSO and Western North Pacific tropical cyclone activity simulated in a CGCM[J]. Clim Dyn, 2008, 30: 815-830.
    WANG, CHAN J. How strong ENSO events affect tropical storm activity over the western North Pacific[J]. J Clim, 2002, 15: 1643-1658.
    JANICO S. Impact of warm ENSO events on atmospheric circulation and convection over the tropical Atlantic and West Africa[J]. Ann Geophysicae, 1997,15: 471-475.
    YUKIMOTO S, NODA A,KITOH A, et al. The New Meteorological Research Institute Coupled GCM (MRI-CGCM2)-Model climate and variability[J]. Meteo Geophys, 2001,51: 47-88.
    FLATO G M, BOER G J, LEE W G, et al. The canadian centre for climate modelling and analysis global coupled model and its climate[J]. Climate Dyn,2000, 16: 427-450.
    周学鸣,魏应植,吴陈锋.夏季西太平洋台风频数异常与ENSO事件的关系及大气环流异常特征[J].热带气象学报,2006,22:35-40.
    HOERLING M P , HURRELL J W,XU T. Tropical origins for recent North Atlantic climate change[J]. Science, 2001,292:90-92.
    MUTHUVEL C,BELL G D. Tropical multidecadal and interannual climate variability in the NCEP-NCAR Reanalysis[J]. J Clim, 2004,17: 1777-1802.
    MESTAS-NUEZ M A,ENFIELD D B. Rotated global modes of non-ENSO sea surface temperature variability[J]. J Clim, 1999,12:2734-2746.
    MESTAS-NUEZ M A, ENFIELD D B. Eastern equatorial Pacific SST variability: ENSO and non-ENSO components and their climatic associations[J]. J Clim, 2001,14:391-402.
    GARREAUD R, BATTISTI D S. Interannual and interdecadal (ENSO-like) variability in the Southern Hemisphere tropospheric circulation[J]. J Clim, 1999, 12:2113-2123.
    ZHANG Y, WALLACE J M, BATTISTI D S. ENSO-like interdecadal variability[J]. J Clim, 1997,10: 1004-1020.
  • 加载中
计量
  • 文章访问数:  1307
  • HTML全文浏览量:  3
  • PDF下载量:  1130
  • 被引次数: 0
出版历程
  • 收稿日期:  2009-08-21
  • 修回日期:  2010-06-07

目录

    /

    返回文章
    返回