A gridded monthly upper-air data set from 1918 to 1957
- 147 Downloads
Significant efforts have been devoted in recent years towards extending observation-based three-dimensional atmospheric data sets back in time. Such data sets form an important basis for a better understanding of the climate system. Here we present a new monthly three-dimensional global data set that is based on historical upper-air data and surface data. We use statistical reconstruction techniques, calibrated using ERA-40 data, to obtain gridded data from the numerous, but scattered and heterogeneous historical upper-air observations. In contrast to previous work, in which we used hemispheric principal components on both the predictor and the predictand side to reconstruct spatially complete fields back to 1880, we restrict the procedure to places and times where upper-air observations are available. Each grid column (consisting of four variables at six levels) is then reconstructed independently using only predictor variables in the vicinity (i.e., only local stationarity is required rather than stationary large-scale patterns). The product, termed REC2, is a gridded, global monthly data set of geopotential height, temperature, and u and v wind from 850 to 100 hPa back to 1918. The data set is sparse (i.e., many grid cells are empty), but provides an alternative to large-scale reconstructions as it allows for non-stationary teleconnections. We show the results of several validation experiments, compare our new data set with a number of existing data sets, and demonstrate that it is suitable for analysing large-scale climate variability on interannual time-scales.
KeywordsRoot Mean Square Error Total Ozone Lower Stratosphere Calibration Period Interannual Time Scale
This work was supported by the Swiss National Science Foundation, Project “Past climate variability from an upper-level perspective”. We also gratefully acknowledge the support of the Swiss National Centre of Competence in Research on Climate (NCCR-Climate), funded by the Swiss National Science Foundation. We wish to thank Gil Compo, Jeff Whitaker and Prashant Sardeshmukh (University of Colorado and NOAA) for providing 20CR data, ECMWF for providing the ERA-40 data and the Hadley Centre of the UK MetOffice for providing the HadCRUT3v and the HadSLP2 data sets.
- Compo GP et al (2010) The twentieth century reanalysis project. Q J R Meteorol Soc (submitted)Google Scholar
- Cook BI, Seager R, Miller RL (2010) Atmospheric circulation anomalies during two persistent North American droughts: 1932–1939 and 1948–1957. Clim Dyn (online first). doi: 10.1007/s00382-010-0807-1
- Griesser T, Brönnimann S, Grant A, Ewen T, Stickler A, Comeaux J (2010) Reconstruction of global monthly upper-level temperature and geopotential height fields back to 1880. J Clim (ealy online release). doi: 10.1175/2010JCLI3056.1
- Jones PD, Wigley TML, Briffa KR (1987) Monthly mean pressure reconstructions for Europe (back to 1780) and North America (to 1858). U.S. Dept. of Energy Carbon Dioxide Research Division, Technical Report TRO37, 99 ppGoogle Scholar
- Luterbacher J, Xoplaki E, Dietrich D, Rickli R, Jacobeit J, Beck C, Gyalistras D, Schmutz C, Wanner H (2002) Reconstruction of sea level pressure fields over the Eastern North Atlantic and Europe back to 1500. Clim Dyn 18:545–561Google Scholar
- Simmons AJ, Jones PD, da Costa Bechtold V, Beljaars ACM, Kallberg PW, Saarinen S, Uppala SM, Viterbo P, Wedi N (2004) Comparison of trends and low-frequency variability in CRU, ERA-40 and NCEP/NCAR analyses of surface air temperature. J Geophys Res 109:D24115. doi: 10.1029/2004JD005306 CrossRefGoogle Scholar