4.6 Review

The Twentieth Century Reanalysis Project

期刊

出版社

WILEY
DOI: 10.1002/qj.776

关键词

data assimilation; Ensemble Kalman Filter; state estimation; surface pressure; sea-level pressure

资金

  1. Queensland Climate Change Centre of Excellence
  2. UK Joint Department of Energy and Climate Change and Department for Environment, Food and Rural Affairs (DECC/Defra) [DECC/Defra GA01101]
  3. National Science Foundation
  4. Swiss National Science Foundation
  5. US Department of Energy, Office of Science Innovative and Novel Computational Impact on Theory and Experiment (DOE INCITE)
  6. Office of Biological and Environmental Research (BER)
  7. NOAA Climate Goal
  8. Office of Science of the US Department of Energy [DE-AC02-05CH11231, DE-AC05-00OR22725]
  9. NERC [bas0100023] Funding Source: UKRI
  10. Natural Environment Research Council [bas0100023] Funding Source: researchfish

向作者/读者索取更多资源

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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