Abstract

Abstract. The CHASE-PL (Climate change impact assessment for selected sectors in Poland) Forcing Data–Gridded Daily Precipitation & Temperature Dataset–5 km (CPLFD-GDPT5) consists of 1951–2013 daily minimum and maximum air temperatures and precipitation totals interpolated onto a 5 km grid based on daily meteorological observations from the Institute of Meteorology and Water Management (IMGW-PIB; Polish stations), Deutscher Wetterdienst (DWD, German and Czech stations), and European Climate Assessment and Dataset (ECAD) and National Oceanic and Atmosphere Administration–National Climatic Data Center (NOAA-NCDC) (Slovak, Ukrainian, and Belarusian stations). The main purpose for constructing this product was the need for long-term aerial precipitation and temperature data for earth-system modelling, especially hydrological modelling. The spatial coverage is the union of the Vistula and Oder basins and Polish territory. The number of available meteorological stations for precipitation and temperature varies in time from about 100 for temperature and 300 for precipitation in the 1950s up to about 180 for temperature and 700 for precipitation in the 1990s. The precipitation data set was corrected for snowfall and rainfall under-catch with the Richter method. The interpolation methods were kriging with elevation as external drift for temperatures and indicator kriging combined with universal kriging for precipitation. The kriging cross validation revealed low root-mean-squared errors expressed as a fraction of standard deviation (SD): 0.54 and 0.47 for minimum and maximum temperature, respectively, and 0.79 for precipitation. The correlation scores were 0.84 for minimum temperatures, 0.88 for maximum temperatures, and 0.65 for precipitation. The CPLFD-GDPT5 product is consistent with 1971–2000 climatic data published by IMGW-PIB. We also confirm good skill of the product for hydrological modelling by performing an application using the Soil and Water Assessment Tool (SWAT) in the Vistula and Oder basins. Link to the data set: doi:10.4121/uuid:e939aec0-bdd1-440f-bd1e-c49ff10d0a07.

Highlights

  • High-resolution aerial precipitation and air temperature data are becoming more and more desired as input or verification data for distributed earth-system modelling

  • The CHASE-PL (Climate change impact assessment for selected sectors in Poland) Forcing Data– Gridded Daily Precipitation & Temperature Dataset–5 km (CPLFD-GDPT5) consists of 1951–2013 daily minimum and maximum air temperatures and precipitation totals interpolated onto a 5 km grid based on daily meteorological observations from the Institute of Meteorology and Water Management (IMGW-PIB; Polish stations), Deutscher Wetterdienst (DWD, German and Czech stations), and European Climate Assessment and Dataset (ECAD) and National Oceanic and Atmosphere Administration–National Climatic Data Center (NOAA-NCDC) (Slovak, Ukrainian, and Belarusian stations)

  • In this study we show the workflow for constructing the CHASE-PL (Climate change impact assessment for selected sectors in Poland) Forcing Data–Gridded Daily Precipitation & Temperature Dataset–5 km (CPLFD-GDPT5) product

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Summary

Introduction

High-resolution aerial precipitation and air temperature data are becoming more and more desired as input or verification data for distributed earth-system modelling. Global data sets which include (sub-)daily gridded precipitation and temperature (Sheffield et al, 2006; Dee et al, 2011; Schamm et al, 2014; Weedon et al, 2014) are available in a range of spatial resolutions, with typically highest resolution of 0.25 × 0.25◦, which is equivalent to 28 × 28 km at the Equator and 28 × 14 km at 60◦ north Numerous applications of these data sets are found for large-scale hydrological modelling (Haddeland et al, 2011; Li et al, 2013; Abbaspour et al, 2015). We believe that the workflow presented can be a guideline for other regional meteorological interpolation studies

Temporal and spatial representation of the CPLFD-GDPT5
Source data
No-data filtering and quality check
Rainfall and snowfall under-catch correction
Interpolation
Temperature kriging
Precipitation kriging
Cross validation
Cross validation of precipitation
Cross validation of temperature
Consistency with climatic data
Applicability
Findings
Conclusions
Full Text
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