Impacts of uncertainties in European gridded precipitation observations on regional climate analysis

被引:217
作者
Prein, Andreas F. [1 ,2 ,3 ]
Gobiet, Andreas [3 ,4 ]
机构
[1] NCAR, MMM Mesoscale & Microscale Meteorol Lab, 3090 Ctr Green Dr, Boulder, CO 80301 USA
[2] NCAR, Res Applicat Lab, 3090 Ctr Green Dr, Boulder, CO 80301 USA
[3] Graz Univ, Wegener Ctr Climate & Global Change, Graz, Austria
[4] Cent Inst Meteorol & Geodynam ZAMG, Avalanche Warning Serv, Graz, Austria
基金
奥地利科学基金会; 美国国家科学基金会;
关键词
observation uncertainties; precipitation; undercatch correction; climate models; high resolution; EURO-CORDEX; extremes; MASS FLUX FRAMEWORK; PART I; SPATIAL INTERPOLATION; DAILY RAINFALL; MODEL; PARAMETERIZATION; RESOLUTION; SCALE; PERFORMANCE; MESOSCALE;
D O I
10.1002/joc.4706
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Gridded precipitation data sets are frequently used to evaluate climate models or to remove model output biases. Although precipitation data are error prone due to the high spatio-temporal variability of precipitation and due to considerable measurement errors, relatively few attempts have been made to account for observational uncertainty in model evaluation or in bias correction studies. In this study, we compare three types of European daily data sets featuring two Pan-European data sets and a set that combines eight very high-resolution station-based regional data sets. Furthermore, we investigate seven widely used, larger scale global data sets. Our results demonstrate that the differences between these data sets have the same magnitude as precipitation errors found in regional climate models. Therefore, including observational uncertainties is essential for climate studies, climate model evaluation, and statistical post-processing. Following our results, we suggest the following guidelines for regional precipitation assessments. (1) Include multiple observational data sets from different sources (e.g. station, satellite, reanalysis based) to estimate observational uncertainties. (2) Use data sets with high station densities to minimize the effect of precipitation undersampling (may induce about 60% error in data sparse regions). The information content of a gridded data set is mainly related to its underlying station density and not to its grid spacing. (3) Consider undercatch errors of up to 80% in high latitudes and mountainous regions. (4) Analyses of small-scale features and extremes are especially uncertain in gridded data sets. For higher confidence, use climate-mean and larger scale statistics. In conclusion, neglecting observational uncertainties potentially misguides climate model development and can severely affect the results of climate change impact assessments.
引用
收藏
页码:305 / 327
页数:23
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