The Twentieth Century Reanalysis Project

被引:2698
|
作者
Compo, G. P. [1 ,2 ]
Whitaker, J. S. [2 ]
Sardeshmukh, P. D. [1 ,2 ]
Matsui, N. [1 ,2 ]
Allan, R. J. [3 ]
Yin, X. [4 ]
Gleason, B. E., Jr. [5 ]
Vose, R. S. [5 ]
Rutledge, G. [5 ]
Bessemoulin, P. [6 ]
Broennimann, S. [7 ,8 ]
Brunet, M. [9 ,12 ]
Crouthamel, R. I. [10 ]
Grant, A. N. [7 ]
Groisman, P. Y. [5 ,11 ]
Jones, P. D. [12 ]
Kruk, M. C. [4 ]
Kruger, A. C. [13 ]
Marshall, G. J. [14 ]
Maugeri, M. [15 ]
Mok, H. Y. [16 ]
Nordli, O. [17 ]
Ross, T. F. [18 ]
Trigo, R. M. [19 ]
Wang, X. L. [20 ]
Woodruff, S. D. [2 ]
Worley, S. J. [21 ]
机构
[1] Univ Colorado, CIRES, Climate Diagnost Ctr, Boulder, CO 80309 USA
[2] NOAA, Earth Syst Res Lab, Div Phys Sci, Boulder, CO USA
[3] Met Off, Hadley Ctr, ACRE Project, Exeter, Devon, England
[4] STG Inc, Asheville, NC USA
[5] NOAA, Natl Climat Data Ctr, Asheville, NC USA
[6] Meteo France, Toulouse, France
[7] ETH, Zurich, Switzerland
[8] Univ Bern, Oeschger Ctr Climate Change Res, CH-3012 Bern, Switzerland
[9] Univ Rovira & Virgili, Ctr Climate Change, Tarragona, Spain
[10] Int Environm Data Rescue Org, Deale, MD USA
[11] Univ Corp Atmospher Res, Boulder, CO USA
[12] Univ E Anglia, Climat Res Unit, Norwich NR4 7TJ, Norfolk, England
[13] S African Weather Serv, Pretoria, South Africa
[14] British Antarctic Survey, Cambridge CB3 0ET, England
[15] Univ Milan, Dipartimento Fis, Milan, Italy
[16] Hong Kong Observ, Hong Kong, Hong Kong, Peoples R China
[17] Norwegian Meteorol Inst, Oslo, Norway
[18] NOAA, Climate Database Modernizat Program, NCDC, Asheville, NC USA
[19] Univ Lisbon, Ctr Geofis, IDL, P-1699 Lisbon, Portugal
[20] Environm Canada, Toronto, ON, Canada
[21] Natl Ctr Atmospher Res, Boulder, CO 80307 USA
基金
美国国家科学基金会; 瑞士国家科学基金会;
关键词
data assimilation; Ensemble Kalman Filter; state estimation; surface pressure; sea-level pressure; ENSEMBLE KALMAN FILTER; MODEL-ERROR REPRESENTATION; DATA ASSIMILATION; LEVEL PRESSURE; SURFACE-TEMPERATURE; NORTHERN-HEMISPHERE; ATMOSPHERIC CIRCULATION; GLOBAL PRECIPITATION; GEOPOTENTIAL HEIGHT; DATA SET;
D O I
10.1002/qj.776
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The Twentieth Century Reanalysis (20CR) project is an international effort to produce a comprehensive global atmospheric circulation dataset spanning the twentieth century, assimilating only surface pressure reports and using observed monthly sea-surface temperature and sea-ice distributions as boundary conditions. It is chiefly motivated by a need to provide an observational dataset with quantified uncertainties for validations of climate model simulations of the twentieth century onall time-scales, with emphasis on the statistics of daily weather. It uses an Ensemble Kalman Filter data assimilation method with background 'first guess' fields supplied by an ensemble of forecasts from a global numerical weather prediction model. This directly yields a global analysis every 6 hours as the most likely state of the atmosphere, and also an uncertainty estimate of that analysis. The 20CR dataset provides the first estimates of global tropospheric variability, and of the dataset's time-varying quality, from 1871 to the present at 6-hourly temporal and 2 degrees spatial resolutions. Intercomparisons with independent radiosonde data indicate that the reanalyses are generally of high quality. The quality in the extratropical Northern Hemisphere throughout the century is similar to that of current three-day operational NWP forecasts. Intercomparisons over the second half-century of these surface-based reanalyses with other reanalyses that also make use of upper-air and satellite data are equally encouraging. It is anticipated that the 20CR dataset will be a valuable resource to the climate research community for both model validations and diagnostic studies. Some surprising results are already evident. For instance, the long-term trends of indices representing the North Atlantic Oscillation, the tropical Pacific Walker Circulation, and the Pacific-North American pattern are weak or non-existent over the full period of record. The long-term trends of zonally averaged precipitation minus evaporation also differ in character from those in climate model simulations of the twentieth century. Copyright (C) 2011 Royal Meteorological Society and Crown Copyright.
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页码:1 / 28
页数:28
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