Tropospheric temperature trends: history of an ongoing controversy

被引:146
作者
Thorne, Peter W. [1 ,2 ]
Lanzante, John R. [3 ]
Peterson, Thomas C.
Seidel, Dian J. [4 ]
Shine, Keith P. [5 ]
机构
[1] Met Off Hadley Ctr, Exeter, Devon, England
[2] NOAA, Cooperat Inst Climate & Satellites, Natl Climat Data Ctr, Asheville, NC USA
[3] NOAA, Geophys Fluid Dynam Lab, Princeton, NJ USA
[4] NOAA, Air Resources Lab, Silver Spring, MD 20910 USA
[5] Univ Reading, Dept Meteorol, Reading, Berks, England
关键词
MICROWAVE SOUNDING UNIT; 63-STATION RADIOSONDE NETWORK; CLIMATE MODEL SIMULATIONS; AIR-TEMPERATURE; MSU CHANNEL-2; GLOBAL CHANGE; UNEXPLAINED DISCONTINUITY; TEMPORAL HOMOGENIZATION; VERTICAL STRUCTURE; MERGING PROCEDURE;
D O I
10.1002/wcc.80
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Changes in atmospheric temperature have a particular importance in climate research because climate models consistently predict a distinctive vertical profile of trends. With increasing greenhouse gas concentrations, the surface and troposphere are consistently projected to warm, with an enhancement of that warming in the tropical upper troposphere. Hence, attempts to detect this distinct 'fingerprint' have been a focus for observational studies. The topic acquired heightened importance following the 1990 publication of an analysis of satellite data which challenged the reality of the projected tropospheric warming. This review documents the evolution over the last four decades of understanding of tropospheric temperature trends and their likely causes. Particular focus is given to the difficulty of producing homogenized datasets, with which to derive trends, from both radiosonde and satellite observing systems, because of the many systematic changes over time. The value of multiple independent analyses is demonstrated. Paralleling developments in observational datasets, increased computer power and improved understanding of climate forcing mechanisms have led to refined estimates of temperature trends from a wide range of climate models and a better understanding of internal variability. It is concluded that there is no reasonable evidence of a fundamental disagreement between tropospheric temperature trends from models and observations when uncertainties in both are treated comprehensively. (c) 2010 Crown copyright WIREs Clim Change 2011 2 66-88 DOI: 10.1002/wcc.80
引用
收藏
页码:66 / 88
页数:23
相关论文
共 229 条
[1]   Analysis of spatial distribution in tropospheric temperature trends [J].
Agudelo, PA ;
Curry, JA .
GEOPHYSICAL RESEARCH LETTERS, 2004, 31 (22) :1-5
[2]   Checking for model consistency in optimal fingerprinting [J].
Allen, MR ;
Tett, SFB .
CLIMATE DYNAMICS, 1999, 15 (06) :419-434
[3]   Warming maximum in the tropical upper troposphere deduced from thermal winds [J].
Allen, Robert J. ;
Sherwood, Steven C. .
NATURE GEOSCIENCE, 2008, 1 (06) :399-403
[4]   Utility of radiosonde wind data in representing climatological variations of tropospheric temperature and baroclinicity in the western tropical Pacific [J].
Allen, Robert J. ;
Sherwood, Steven C. .
JOURNAL OF CLIMATE, 2007, 20 (21) :5229-5243
[5]  
Angell JK, 1988, J CLIMATE, V1, P1296, DOI 10.1175/1520-0442(1988)001<1296:VATITA>2.0.CO
[6]  
2
[7]  
ANGELL JK, 1975, MON WEATHER REV, V103, P1007, DOI 10.1175/1520-0493(1975)103<1007:EOTGCI>2.0.CO
[8]  
2
[9]  
ANGELL JK, 1977, MON WEATHER REV, V105, P375, DOI 10.1175/1520-0493(1977)105<0375:EOTGCI>2.0.CO
[10]  
2