Hemispheric and large-scale land-surface air temperature variations: An extensive revision and an update to 2010

被引:583
作者
Jones, P. D. [1 ,3 ]
Lister, D. H. [1 ]
Osborn, T. J. [1 ]
Harpham, C. [1 ]
Salmon, M. [1 ]
Morice, C. P. [2 ]
机构
[1] Univ E Anglia, Climat Res Unit, Sch Environm Sci, Norwich NR4 7TJ, Norfolk, England
[2] Met Off Hadley Ctr, Exeter EX1 3PB, Devon, England
[3] King Abdulaziz Univ, Dept Meteorol, Ctr Excellence Climate Change Res, Jeddah 21413, Saudi Arabia
关键词
DENSITY; TRENDS;
D O I
10.1029/2011JD017139
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
This study is an extensive revision of the Climatic Research Unit (CRU) land station temperature database that has been used to produce a grid-box data set of 5 degrees latitude x 5 degrees longitude temperature anomalies. The new database (CRUTEM4) comprises 5583 station records of which 4842 have enough data for the 1961-1990 period to calculate or estimate the average temperatures for this period. Many station records have had their data replaced by newly homogenized series that have been produced by a number of studies, particularly from National Meteorological Services (NMSs). Hemispheric temperature averages for land areas developed with the new CRUTEM4 data set differ slightly from their CRUTEM3 equivalent. The inclusion of much additional data from the Arctic (particularly the Russian Arctic) has led to estimates for the Northern Hemisphere (NH) being warmer by about 0.1 degrees C for the years since 2001. The NH/Southern Hemisphere (SH) warms by 1.12 degrees C/0.84 degrees C over the period 1901-2010. The robustness of the hemispheric averages is assessed by producing five different analyses, each including a different subset of 20% of the station time series and by omitting some large countries. CRUTEM4 is also compared with hemispheric averages produced by reanalyses undertaken by the European Centre for Medium-Range Weather Forecasts (ECMWF): ERA-40 (1958-2001) and ERA-Interim (1979-2010) data sets. For the NH, agreement is good back to 1958 and excellent from 1979 at monthly, annual, and decadal time scales. For the SH, agreement is poorer, but if the area is restricted to the SH north of 60 degrees S, the agreement is dramatically improved from the mid-1970s.
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相关论文
共 46 条
[21]  
JONES PD, 1994, J CLIMATE, V7, P1794, DOI 10.1175/1520-0442(1994)007<1794:HSATVA>2.0.CO
[22]  
2
[23]   Surface air temperature and its changes over the past 150 years [J].
Jones, PD ;
New, M ;
Parker, DE ;
Martin, S ;
Rigor, IG .
REVIEWS OF GEOPHYSICS, 1999, 37 (02) :173-199
[24]   Estimation of global temperature trends: what's important and what isn't [J].
Jones, Phil D. ;
Wigley, T. M. L. .
CLIMATIC CHANGE, 2010, 100 (01) :59-69
[25]   THE US HISTORICAL CLIMATOLOGY NETWORK MONTHLY TEMPERATURE DATA, VERSION 2 [J].
Menne, Matthew J. ;
Williams, Claude N., Jr. ;
Vose, Russell S. .
BULLETIN OF THE AMERICAN METEOROLOGICAL SOCIETY, 2009, 90 (07) :993-1007
[26]  
Nicholls N., 1996, International Journal of Climatology, V16, P705, DOI 10.1002/(SICI)1097-0088(199606)16:6<705::AID-JOC30>3.0.CO
[27]  
2-S
[28]   Comment on "Unresolved issues with the assessment of multidecadal global land surface temperature trends" by Roger A. Pielke Sr. et al. [J].
Parker, David E. ;
Jones, Phil ;
Peterson, Thomas C. ;
Kennedy, John .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2009, 114
[29]   First difference method: Maximizing station density for the calculation of long-term global temperature change [J].
Peterson, TC ;
Karl, TR ;
Jamason, PF ;
Knight, R ;
Easterling, DR .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1998, 103 (D20) :25967-25974
[30]  
Razuvaev V., 2009, NATO SCI PEACE SEC C, V1, P7