Consistency of modelled and observed temperature trends in the tropical troposphere

被引:199
作者
Santer, B. D. [1 ]
Thorne, P. W. [2 ]
Haimberger, L. [3 ]
Taylor, K. E. [1 ]
Wigley, T. M. L. [4 ]
Lanzante, J. R. [5 ]
Solomon, S. [6 ]
Free, M. [7 ]
Gleckler, P. J. [1 ]
Jones, P. D. [8 ]
Karl, T. R. [9 ]
Klein, S. A. [1 ]
Mears, C. [10 ]
Nychka, D. [4 ]
Schmidt, G. A. [11 ]
Sherwood, S. C. [12 ]
Wentz, F. J. [10 ]
机构
[1] Lawrence Livermore Natl Lab, PCMDI, Livermore, CA 94550 USA
[2] Hadley Ctr, UK Meteorol Off, Exeter EX1 3PB, Devon, England
[3] Univ Vienna, Dept Meteorol & Geophys, A-1090 Vienna, Austria
[4] Natl Ctr Atmospher Res, Boulder, CO 80307 USA
[5] Natl Ocean & Atmospher Adm, Geophys Fluid Dynam Lab, Princeton, NJ 08542 USA
[6] Natl Ocean & Atmospher Adm, Earth Syst Res Lab, Div Chem Sci, Boulder, CO 80305 USA
[7] NOAA, Air Resources Lab, Silver Spring, MD 20910 USA
[8] Univ E Anglia, Sch Environm Sci, Climat Res Unit, Norwich NR4 7TJ, Norfolk, England
[9] Natl Ocean & Atmospher Adm, Natl Climat Data Ctr, Asheville, NC 28801 USA
[10] Remote Sensing Syst, Santa Rosa, CA 95401 USA
[11] NASA, Goddard Inst Space Studies, New York, NY 10025 USA
[12] Yale Univ, New Haven, CT 06520 USA
关键词
tropospheric temperature changes; climate model evaluation; statistical significance of trend differences; tropical lapse rates; differential warming of surface and temperature;
D O I
10.1002/joc.1756
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
A recent report of the U.S. Climate Change Science Program (CCSP) identified a 'potentially serious inconsistency' between modelled and observed trends in tropical lapse rates (Karl et al., 2006). Early versions of Satellite and radiosonde datasets suggested that the tropical surface had warmed more than the troposphere, while climate models consistently showed tropospheric amplification of surface warming in response to human-caused increases in well-mixed greenhouse gases (GHGs). We revisit such comparisons here using new observational estimates of surface and tropospheric temperature changes. We find that there is no longer a serious discrepancy between modelled and observed trends in tropical lapse rates. This emerging reconciliation of models and observations has two primary explanations. First, because of changes in the treatment of buoy and satellite information, new surface temperature datasets yield slightly reduced tropical warming relative to earlier versions. Second, recently developed satellite and radiosonde datasets show larger warming of the tropical lower troposphere. In the case of a new satellite dataset from Remote Sensing Systems (RSS), enhanced warming is due to an improved procedure of adjusting for inter-satellite biases. When the RSS-derived tropospheric temperature trend is compared with four different observed estimates of surface temperature change, the surface warming is invariably amplified in the tropical troposphere, consistent with model results. Even if we use data from a second satellite dataset with smaller tropospheric warming than in RSS, observed tropical lapse rate trends are not significantly different from those in all other model simulations. Our results contradict a recent claim that all simulated temperature trends in the tropical troposphere and in tropical lapse rates are inconsistent with observations. This claim was based on use of older radiosonde and satellite datasets, and on two methodological errors: the neglect of observational trend uncertainties introduced by interannual climate variability, and application of an inappropriate statistical 'consistency test'. Copyright (c) 2008 Royal Meteorological Society
引用
收藏
页码:1703 / 1722
页数:20
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