用户名: 密码: 验证码:
大气温度反馈的机理及其对全球增暖的贡献
详细信息    查看全文 | 推荐本文 |
  • 英文篇名:Air temperature feedback and its contribution to global warming
  • 作者:胡晓明 ; 蔡鸣 ; 杨崧 ; Sergio ; A.SEJAS
  • 英文作者:Hu X;Cai M;Yang S;Sejas S A;
  • 关键词:全球变暖 ; 大气温度反馈 ; 地表能量收支
  • 中文刊名:JDXK
  • 英文刊名:Scientia Sinica(Terrae)
  • 机构:中山大学大气科学学院;广东省气候变化与自然灾害研究重点实验室;Department of Earth,Ocean and Atmospheric Sciences,Florida State University;中山大学地球气候与环境系统研究院;NASA Langley Research Center,Climate Science Branch;
  • 出版日期:2019-02-20
  • 出版单位:中国科学:地球科学
  • 年:2019
  • 期:v.49
  • 基金:国家重大科学研究计划项目(编号:2014CB953904);; 广东省自然科学基金项目(编号:2017A030310571);; 中央高校基本科研业务费专项资金项目(编号:17LGPY21)资助
  • 语种:中文;
  • 页:JDXK201902010
  • 页数:19
  • CN:02
  • ISSN:11-5842/P
  • 分类号:120-138
摘要
大气和地表之间热辐射交换引起的地气温度耦合(即大气温度反馈)是影响地表能量收支平衡的重要因子.文章旨在阐述大气温度反馈机理,讨论影响其强度和空间分布的主要因子;并以全球变暖为例,论述大气温度反馈如何与外强迫和气候反馈过程耦合最终对全球增暖产生贡献.基于ERA-Interim再分析资料,利用地表反馈响应分析方法,计算大气温度反馈核,以此来阐述大气温度反馈的物理机制及其强度的空间分布与气候态温度、水汽和云水含量空间分布的关系,以及全球增暖加速期间大气温度反馈对全球平均表面温度增加的贡献.分析表明大气温度反馈过程主要通过与气候系统外强迫和内部过程的耦合作用,将各独立过程引起的地表能量收支异常信号放大.研究结果表明大气温度反馈显著放大了CO_2浓度升高、冰雪融化、水汽含量增加和海洋热量吸收减缓引起的地表增暖,削弱了云量增加引起的地表降温效应.同时,也放大了地表潜热通量增加造成的地表冷却效应.从全球平均结果来看,全球快速变暖前后,尽管外强迫和气候系统内部过程引起的全球平均总地面直接能量通量扰动为负,但大气温度反馈造成的全球平均总地面能量通量扰动却为正,且后者幅度远大于前者,这导致全球平均总地面净能量通量扰动正异常.由此可见,大气温度反馈对全球变暖起到了至关重要的作用.
        
引文
丁守国,赵春生,石广玉.2005.近20年全球总云量变化趋势分析.应用气象学报,16:670-677
    李崇银,翁衡毅,高晓清.2003.全球增暖的另一可能原因初探.大气科学,27:789-797
    李建平,任荣彩,齐义泉.2013.亚洲区域海-陆-气相互作用对全球和亚洲气候变化的作用研究进展.大气科学,37:518-538
    李立娟,王斌,周天军.2007.外强迫因子对二十世纪全球变暖的综合影响.科学通报,52:1820-1825
    吕达仁.1996.中层大气与全球变化.科技导报,14:31-34
    郑彬,施春华.2006.全球平流层下部降温及其对纬向风的影响.气象科技,34:538-541
    Adler R F,Huffman G J,Chang A,Ferraro R,Xie P P,Janowiak J,Rudolf B,Schneider U,Curtis S,Bolvin D,Gruber A,Susskind J,Arkin P,Nelkin E.2003.The version-2 global precipitation climatology project(GPCP)monthly precipitation analysis(1979-present).J Hydrometeorol,4:1147-1167
    Albrecht B A.1989.Aerosols,cloud microphysics,and fractional cloudiness.Science,245:1227-1230
    Auer I,B?hm R,Jurkovic A,Lipa W,Orlik A,Potzmann R,Sch?ner W,Ungersb?ck M,Matulla C,Briffa K,Jones P,Efthymiadis D,Brunetti M,Nanni T,Maugeri M,Mercalli L,Mestre O,Moisselin JM,Begert M,Müller-Westermeier G,Kveton V,Bochnicek O,Stastny P,Lapin M,Szalai S,Szentimrey T,Cegnar T,Dolinar M,Gajic-Capka M,Zaninovic K,Majstorovic Z,Nieplova E.2007.HISTALP-Historical instrumental climatological surface time series of the Greater Alpine Region.Int J Climatol,27:17-46
    Brasseur G,Hitchman M H.1988.Stratospheric response to trace gas perturbations:Changes in ozone and temperature distributions.Science,240:634-637
    Cai M,Lu J H.2007.Dynamical greenhouse-plus feedback and polar warming amplification.Part II:meridional and vertical asymmetries of the global warming.Clim Dyn,29:375-391
    Cai M,Lu J H.2009.A new framework for isolating individual feedback processes in coupled general circulation climate models.Part II:Method demonstrations and comparisons.Clim Dyn,32:887-900
    Cai M,Tung K K.2012.Robustness of dynamical feedbacks from radiative forcing:2%solar versus 2×CO2experiments in an idealized GCM.J Atmos Sci,69:2256-2271
    Dai A,Karl T R,Sun B,Trenberth K E.2006.Recent trends in cloudiness over the United States:A tale of monitoring inadequacies.Bull Amer Meteorol Soc,87:597-606
    Dee D P,Uppala S M,Simmons A J,Berrisford P,Poli P,Kobayashi S,Andrae U,Balmaseda M A,Balsamo G,Bauer P,Bechtold P,Beljaars A C M,van de Berg L,Bidlot J,Bormann N,Delsol C,Dragani R,Fuentes M,Geer A J,Haimberger L,Healy S B,Hersbach H,Hólm E V,Isaksen L,K?llberg P,K?hler M,Matricardi M,McNally A P,Monge-Sanz B M,Morcrette J J,Park B K,Peubey C,de Rosnay P,Tavolato C,Thépaut J N,Vitart F.2011.The ERA-Interim reanalysis:Configuration and performance of the data assimilation system.Q J R Meteorol Soc,137:553-597
    Eastman R,Warren S G.2013.A 39-yr survey of cloud changes from land stations worldwide 1971-2009:long-term trends,relation to aerosols,and expansion of the tropical belt.J Clim,26:1286-1303
    Fu Q,Liou K N.1993.Parameterization of the radiative properties of cirrus clouds.J Atmos Sci,50:2008-2025
    Guan X,Huang J,Guo R,Lin P.2015a.The role of dynamically induced variability in the recent warming trend slowdown over the Northern Hemisphere.Sci Rep,5:12669
    Guan X,Huang J,Guo R,Yu H,Lin P,Zhang Y.2015b.Role of radiatively forced temperature changes in enhanced semi-arid warming in the cold season over east Asia.Atmos Chem Phys,15:13777-13786
    Hall A,Manabe S.1999.The role of water vapor feedback in unperturbed climate variability and global warming.J Clim,12:2327-2346
    Hansen J,Ruedy R,Sato M,Lo K.2010.Global surface temperature change.Rev Geophys,48:RG4004
    Hansen J,Sato M,Ruedy R.1997.Radiative forcing and climate response.J Geophys Res,102:6831-6864
    Held I M,Soden B J.2000.Water vapor feedback and global warming.Annu Rev Energy Environ,25:441-475
    Held I M,Soden B J.2006.Robust responses of the hydrological cycle to global warming.J Clim,19:5686-5699
    Holland M M,Bitz C M.2003.Polar amplification of climate change in coupled models.Clim Dyn,21:221-232
    Hu X,Li Y,Yang S,Deng Y,Cai M.2017.Process-based decomposition of the decadal climate difference between 2002-13and 1984-95.J Clim,30:4373-4393
    Huang J,Xie Y,Guan X,Li D,Ji F.2017.The dynamics of the warming hiatus over the Northern Hemisphere.Clim Dyn,48:429-446
    IPCC.2013.Climate change 2013.In:Stocker T F,Qin D,Plattner G K,Tignor M,Allen S K,Boschung J,Nauels A,Xia Y,Bex V,Midgley P M,eds.The Physical Science Basis.Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change.Cambridge:Cambridge University Press.1535
    IPCC.2007:Climate change 2007.In:Solomon S,Qin D,Manning M.Chen Z,Marquis M,Averyt K B,Tignor M,Miller H L,eds.The Physical Science Basis,Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change.Cambridge:Cambridge University Press
    Jones P D,Moberg A.2003.Hemispheric and large-scale surface air temperature variations:An extensive revision and an update to2001.J Clim,16:206-223
    Kaiser D P.1998.Analysis of total cloud amount over China,1951-1994.In:Proceedings of the Ninth Symposium on Global Change Studies.American Meteorological Society.Boston.168-171
    Lu J H,Cai M.2009.A new framework for isolating individual feedback processes in coupled general circulation climate models.Part I:Formulation.Clim Dyn,32:873-885
    Maugeri M,Bagnati Z,Brunetti M,Nanni T.2001.Trends in Italian total cloud amount,1951-1996.Geophys Res Lett,28:4551-4554
    Polyakov I V,Alekseev G V,Bekryaev R V,Bhatt U,Colony R L,Johnson M A,Karklin V P,Makshtas A P,Walsh D,Yulin A V.2002.Observationally based assessment of polar amplification of global warming.Geophys Res Lett,29:25-1-25-4
    Qian Y,Kaiser D P,Leung L R,Xu M.2006.More frequent cloud-free sky and less surface solar radiation in China from 1955 to 2000.Geophys Res Lett,33:L01812
    Ramanathan V.1977.Interactions between ice-albedo,lapse-rate and cloud-top feedbacks:An analysis of the nonlinear response of a GCM climate model.J Atmos Sci,34:1885-1897
    Ramanathan V,Carmichael G.2008.Global and regional climate changes due to black carbon.Nat Geosci,1:221-227
    Rudolf B,Hauschild H,Rueth W,Schneider U.1994.Terrestrial precipitation analysis:Operational method and required density of point measurements.In:Desbois M,Désalmand F,eds.Global Precipitations and Climate Change.NATO ASI Series(Series I:Global Environmental Change),vol 26.Berlin:Springer
    Schneider E K,Kirtman B P,Lindzen R S.1999.Tropospheric water vapor and climate sensitivity.J Atmos Sci,56:1649-1658
    Sejas S A,Cai M.2016.Isolating the temperature feedback loop and its effects on surface temperature.J Atmos Sci,73:3287-3303
    Shell K M,Kiehl J T,Shields C A.2008.Using the radiative kernel technique to calculate climate feedbacks in NCAR’s community atmospheric model.J Clim,21:2269-2282
    Simmons A J,Jones P D,da Costa Bechtold V,Beljaars A C M,K?llberg P W,Saarinen S,Uppala S M,Viterbo P,Wedi N.2004.Comparison of trends and low-frequency variability in CRU,ERA-40,and NCEP/NCAR analyses of surface air temperature.JGeophys Res,109:D24115
    Soden B J,Held I M,Colman R C,Shell K M,Kiehl J T,Shields C A.2008.Quantifying climate feedbacks using radiative kernels.J Clim,21:3504-3520
    Stephens G L,Li J,Wild M,Clayson C A,Loeb N,Kato S,L’Ecuyer T,Stackhouse P W,Lebsock M,Andrews T.2012a.An update on Earth’s energy balance in light of the latest global observations.Nat Geosci,5:691-696
    Stephens G L,Wild M,Stackhouse Jr P W,L’Ecuyer T,Kato S,Henderson D S.2012b.The global character of the flux of downward longwave radiation.J Clim,25:2329-2340
    Sun B,Groisman P Y.2000.Cloudiness variations over the former Soviet Union.Int J Climatol,20:1097-1111
    Taylor P C,Cai M,Hu A,Meehl J,Washington W,Zhang G J.2013.Adecomposition of feedback contributions to polar warming amplification.J Clim,26:7023-7043
    Trenberth K E,Fasullo J,Smith L.2005.Trends and variability in column-integrated atmospheric water vapor.Clim Dyn,24:741-758
    Tyndall J.1861.On the absorption and radiation of heat by gases and vapours.Philos Mag,22:169-194,273-285
    Wang K C,Dickinson R E.2013.Global atmospheric downward longwave radiation at the surface from ground-based observations,satellite retrievals,and reanalyses.Rev Geophys,51:150-185
    Wetherald R T,Manabe S.1988.Cloud feedback processes in a general circulation model.J Atmos Sci,45:1397-1416
    Wu Z,Huang N E,Long S R,Peng C K.2007.On the trend,detrending,and variability of nonlinear and nonstationary time series.Proc Natl Acad Sci USA,104:14889-14894

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700