Daily precipitation‐downscaling techniques in three Chinese regions

Four methods of statistical downscaling of daily precipitation were evaluated on three catchments located in southern, eastern, and central China. The evaluation focused on seasonal variation of statistical properties of precipitation and indices describing the precipitation regime, e.g., maximum length of dry spell and maximum 5‐day precipitation, as well as interannual and intra‐annual variations of precipitation. The predictors used in this study were mean sea level pressure, geopotential heights at 1000, 850, 700, and 500 hPa, and specific humidity as well as horizontal winds at 850, 700, and 500 hPa levels from the NCEP/NCAR reanalysis with 2.5° × 2.5° resolution for 1961–2000. The predictand was daily precipitation from 13 stations. Two analogue methods, one using principal components analysis (PCA) and the other Teweles‐Wobus scores (TWS), a multiregression technique with a weather generator producing precipitation (SDSM) and a fuzzy‐rule‐based weather‐pattern‐classification method (MOFRBC), were used. Temporal and spatial properties of the predictors were carefully evaluated to derive the optimum setting for each method, and MOFRBC and SDSM were implemented in two modes, with and without humidity as predictor. The results showed that (1) precipitation was most successfully downscaled in the southern and eastern catchments located close to the coast, (2) winter properties were generally better downscaled, (3) MOFRBC and SDSM performed overall better than the analogue methods, (4) the modeled interannual variation in precipitation was improved when humidity was added to the predictor set, and (5), the annual precipitation cycle was well captured with all methods.

[1]  R. Reynolds,et al.  The NCEP/NCAR 40-Year Reanalysis Project , 1996, Renewable Energy.

[2]  Chong-Yu Xu,et al.  Seasonality properties of four statistical-downscaling methods in central Sweden , 2007 .

[3]  A Monthly Atmospheric Circulation Classification and Its Relationship with Climate in Harbin ∗ , 2007 .

[4]  Deliang Chen,et al.  Using statistical downscaling to quantify the GCM-related uncertainty in regional climate change scenarios: A case study of Swedish precipitation , 2006 .

[5]  Jia Liwe A Monthly Atmospheric Circulation Classification and Its Relationship with Climate in Harbin , 2006 .

[6]  Deliang Chen,et al.  Statistical downscaling of climate scenarios over Scandinavia , 2005 .

[7]  Chong-Yu Xu,et al.  Statistical precipitation downscaling in central Sweden with the analogue method , 2005 .

[8]  Z. Qiang,et al.  Stochastic modeling of daily precipitation in China , 2004 .

[9]  Deliang Chen,et al.  Statistical downscaling and scenario construction of precipitation in Scania, southern Sweden , 2004 .

[10]  András Bárdossy,et al.  Statistical comparison of European circulation patterns and development of a continental scale classification , 2003 .

[11]  H. Juang,et al.  2×CO2 Eastern Asia regional responses in the RSM/CCM3 modeling system , 2003 .

[12]  Association between winter temperature in China and upper air circulation over East Asia revealed by canonical correlation analysis , 2003 .

[13]  Christian W. Dawson,et al.  Multi-site simulation of precipitation by conditional resampling , 2003 .

[14]  C. Obled,et al.  Quantitative precipitation forecasts: a statistical adaptation of model outputs through an analogues sorting approach , 2002 .

[15]  A. Bárdossy,et al.  Multivariate stochastic downscaling model for generating daily precipitation series based on atmospheric circulation , 2002 .

[16]  B. Beckmann,et al.  Statistical downscaling relationships for precipitation in the Netherlands and North Germany , 2002 .

[17]  Christian W. Dawson,et al.  SDSM - a decision support tool for the assessment of regional climate change impacts , 2002, Environ. Model. Softw..

[18]  Deliang Chen,et al.  Comparison of climate change scenarios for Sweden based on statistical and dynamical downscaling of monthly precipitation , 2001 .

[19]  J. Gregory,et al.  A comparison of extreme European daily precipitation simulated by a global and a regional climate model for present and future climates , 2001 .

[20]  A. Bárdossy,et al.  Generating of areal precipitation series in the upper neckar catchment , 2001 .

[21]  H. Hersbach Decomposition of the Continuous Ranked Probability Score for Ensemble Prediction Systems , 2000 .

[22]  Michael D. Dettinger,et al.  STREAMFLOW CHANGES IN THE SIERRA NEVADA, CALIFORNIA, SIMULATED USING A STATISTICALLY DOWNSCALED GENERAL CIRCULATION MODEL SCENARIO OF CLIMATE CHANGE , 2000 .

[23]  L. Hay,et al.  A comparison of downscaled and raw GCM output: implications for climate change scenarios in the San Juan River basin, Colorado , 1999 .

[24]  D. Wilks,et al.  The weather generation game: a review of stochastic weather models , 1999 .

[25]  H. Storch,et al.  The Analog Method as a Simple Statistical Downscaling Technique: Comparison with More Complicated Methods , 1999 .

[26]  Chong-yu Xu From GCMs to river flow: a review of downscaling methods and hydrologic modelling approaches , 1999 .

[27]  I. Simmonds,et al.  Atmospheric Water Vapor Flux and Its Association with Rainfall over China in Summer , 1999 .

[28]  Xin-Zhong Liang,et al.  The Monsoon Rainband over China and Relationships with the Eurasian Circulation , 1999 .

[29]  T. Wigley,et al.  Downscaling general circulation model output: a review of methods and limitations , 1997 .

[30]  Lucien Duckstein,et al.  Fuzzy rule-based classification of atmospheric circulation patterns , 1995 .

[31]  D. Yihui,et al.  Monsoons over China , 1993 .

[32]  A. Bárdossy,et al.  SPACE-TIME MODEL FOR DAILY RAINFALL USING ATMOSPHERIC CIRCULATION PATTERNS , 1992 .

[33]  A. H. Murphy A Note on the Ranked Probability Score , 1971 .

[34]  Edward S. Epstein,et al.  A Scoring System for Probability Forecasts of Ranked Categories , 1969 .