A critical remark on the applicability of E‐OBS European gridded temperature data set for validating control climate simulations

The study compares daily maximum ( T max ) and minimum ( T min ) temperatures in two data sets interpolated from irregularly spaced meteorological stations to a regular grid: the European gridded data set (E‐OBS), produced from a relatively sparse network of stations available in the European Climate Assessment and Dataset (ECA&D) project, and a data set gridded onto the same grid from a high‐density network of stations in the Czech Republic (GriSt). We show that large differences exist between the two gridded data sets, particularly for T min . The errors tend to be larger in tails of the distributions. In winter, temperatures below the 10% quantile of T min , which is still far from the very tail of the distribution, are too warm by almost 2°C in E‐OBS on average. A large bias is found also for the diurnal temperature range. Comparison with simple average series from stations in two regions reveals that differences between GriSt and the station averages are minor relative to differences between E‐OBS and either of the two data sets. The large deviations between the two gridded data sets affect conclusions concerning validation of temperature characteristics in regional climate model (RCM) simulations. The bias of the E‐OBS data set and limitations with respect to its applicability for evaluating RCMs stem primarily from (1) insufficient density of information from station observations used for the interpolation, including the fact that the stations available may not be representative for a wider area, and (2) inconsistency between the radii of the areal average values in high‐resolution RCMs and E‐OBS. Further increases in the amount and quality of station data available within ECA&D and used in the E‐OBS data set are essentially needed for more reliable validation of climate models against recent climate on a continental scale.