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Aschonitis, Vassilis G; Papamichail, Dimitris; Demertzi, Kleoniki; Colombani, Nicolo; Mastrocicco, Micol; Ghirardini, Andrea; Castaldelli, Giuseppe; Fano, Elisa-Anna (2017): High resolution global grids of revised Priestley-Taylor and Hargreaves-Samani coefficients for assessing ASCE-standardized reference crop evapotranspiration and solar radiation, links to ESRI-grid files [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.868808, Supplement to: Aschonitis, VG et al. (2017): High-resolution global grids of revised Priestley-Taylor and Hargreaves-Samani coefficients for assessing ASCE-standardized reference crop evapotranspiration and solar radiation. Earth System Science Data, 9(2), 615-638, https://doi.org/10.5194/essd-9-615-2017

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Abstract:
The objective of the study is to provide global grids (0.5°) of revised annual coefficients for the Priestley-Taylor (P-T) and Hargreaves-Samani (H-S) evapotranspiration methods after calibration based on the ASCE (American Society of Civil Engineers)-standardized Penman-Monteith method (the ASCE method includes two reference crops: short-clipped grass and tall alfalfa). The analysis also includes the development of a global grid of revised annual coefficients for solar radiation (Rs) estimations using the respective Rs formula of H-S. The analysis was based on global gridded climatic data of the period 1950-2000. The method for deriving annual coefficients of the P-T and H-S methods was based on partial weighted averages (PWAs) of their mean monthly values. This method estimates the annual values considering the amplitude of the parameter under investigation (ETo and Rs) giving more weight to the monthly coefficients of the months with higher ETo values (or Rs values for the case of the H-S radiation formula). The method also eliminates the effect of unreasonably high or low monthly coefficients that may occur during periods where ETo and Rs fall below a specific threshold. The new coefficients were validated based on data from 140 stations located in various climatic zones of the USA and Australia with expanded observations up to 2016. The validation procedure for ETo estimations of the short reference crop showed that the P-T and H-S methods with the new revised coefficients outperformed the standard methods reducing the estimated root mean square error (RMSE) in ETo values by 40 and 25 %, respectively. The estimations of Rs using the H-S formula with revised coefficients reduced the RMSE by 28 % in comparison to the standard H-S formula. Finally, a raster database was built consisting of (a) global maps for the mean monthly ETo values estimated by ASCE-standardized method for both reference crops, (b) global maps for the revised annual coefficients of the P-T and H-S evapotranspiration methods for both reference crops and a global map for the revised annual coefficient of the H-S radiation formula and (c) global maps that indicate the optimum locations for using the standard P-T and H-S methods and their possible annual errors based on reference values. The database can support estimations of ETo and solar radiation for locations where climatic data are limited and it can support studies which require such estimations on larger scales (e.g. country, continent, world). The datasets produced in this study are archived in the PANGAEA database (this data set) and in the ESRN database (http://www.esrn-database.org or http://esrn-database.weebly.com).
Related to:
Allen, Richard G; Walter, Ivan A; Elliott, Ronald; Howell, Terry A; Itenfisu, Daniel; Jensen, Marvin E (2005): The ASCE standardized reference evapotranspiration equation. In: Allen RG, Walter IA, Elliott R, Howell T, Itenfisu D, Jensen M (eds.) Environmental and Water Resources Institute. Task Committee on Standardization of Reference Evapotranspiration of the Environmental and Water Resources Institute. University of Idaho, 70 pp, hdl:10013/epic.49050.d001
Hargreaves, George H; Samani, Zohrab A (1982): Estimating potential evapotranspiration. Journal of Irrigation and Drainage Division (ASCE), 108(IR3), 225-230
Hargreaves, George H; Samani, Zohrab A (1985): Reference crop evapotranspiration from ambient temperature. American Society of Agricultural Engineers, 12 pp, https://doi.org/10.13031/2013.26773
Hijmans, Robert J; Cameron, Susan E; Parra, J L; Jones, Peter G; Jarvis, A (2005): Very high resolution interpolated climate surfaces for global land areas. International Journal of Climatology, 25(15), 1965-1978, https://doi.org/10.1002/joc.1276
Priestley, C H B; Taylor, R J (1972): On the assessment of surface heat flux and evaporation using large-scale parameters. Monthly Weather Review, 100, 81-92
Sheffield, J; Goteti, G; Wood, Eric F (2006): Development of a 50-Year high-resolution global dataset of meteorological forcings for land surface modeling. Journal of Climate, 19(13), 3088-3111, https://doi.org/10.1175/JCLI3790.1
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
ORDINAL NUMBEROrd NoAschonitis, Vassilis GGeocode
File contentContentAschonitis, Vassilis G
Analytical methodMethodAschonitis, Vassilis G
CommentCommentAschonitis, Vassilis G
File nameFile nameAschonitis, Vassilis G
File formatFile formatAschonitis, Vassilis G
File sizeFile sizekByteAschonitis, Vassilis Gzipped
Uniform resource locator/link to fileURL fileAschonitis, Vassilis G
Size:
385 data points

Data

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1Re-adjusted Priestley-Taylor coefficient for short ref.crop ETo (rescaled ×100) (unitless)/(30 arc-sec)Re-calibration of Priestley-Taylor coefficient apt=1.26 for ETo method (Priestley and Taylor, 1972) using ASCE-EWRI method (Allen et al., 2005) for short ref.cropthe zip contains 1 raster (ESRI-grid) (partial weighted average of mean monthly values). For zero values use the closest non-zero value.ESRN-Database | 30arc-sec | apts1_30sESRI grid79287apts1_30s.zip
2Re-adjusted Priestley-Taylor coefficient for tall ref.crop ETo (rescaled ×100) (unitless)/(30 arc-sec)Re-calibration of Priestley-Taylor coefficient apt=1.26 for ETo method (Priestley and Taylor, 1972) using ASCE-EWRI method (Allen et al., 2005) for tall ref.cropthe zip contains 1 raster (ESRI-grid) (partial weighted average of mean monthly values). For zero values use the closest non-zero value.ESRN-Database | 30arc-sec | aptt1_30sESRI grid92835aptt1_30s.zip
3Re-adjusted Hargreaves-Samani coefficient for short ref.crop ETo (rescaled ×100,000) (unitless)/(30 arc-sec)Re-calibration of Hargreaves-Samani coefficient chs2=0.0023 for ETo method (Hargreaves and Samani, 1982, 1985) using ASCE-EWRI method (Allen et al., 2005) for short ref.cropthe zip contains 1 raster (ESRI-grid) (partial weighted average of mean monthly values). For zero values use the closest non-zero value.ESRN-Database | 30arc-sec | chs2s1_30sESRI grid102604chs2s1_30s.zip
4Re-adjusted Hargreaves-Samani coefficient for tall ref.crop ETo (rescaled ×100,000) (unitless)/(30 arc-sec)Re-calibration of Hargreaves-Samani coefficient chs2=0.0023 for ETo method (Hargreaves and Samani, 1982, 1985) using ASCE-EWRI method (Allen et al., 2005) for tall ref.cropthe zip contains 1 raster (ESRI-grid) (partial weighted average of mean monthly values). For zero values use the closest non-zero value.ESRN-Database | 30arc-sec | chs2t1_30sESRI grid122897chs2t1_30s.zip
5Hargeaves-Samani versus Priestley-Taylor (comparison between original methods versus ASCE-short) (DMADhp) (%)/(30 arc-sec)abs(madhs)-abs(madpt), higher negative values suggest better performance of original Hargreaves-Samani ETo method while higher positive values suggest better performance of original Priestley-Taylor ETo method using as reference the ASCE-shortthe zip contains 1 raster (ESRI-grid)ESRN-Database | 30arc-sec | dmadhp1_30sESRI grid83605dmadhp1_30s.zip
6Mean monthly ASCE-ETo for short reference crop (clipped grass) (mm/month)/(30 arc-sec)ASCE-EWRI method (Allen et al., 2005) using climatic data from Hijmans et al. (2005) and Sheffield et al. (2006)the zip contains 12 rasters (ESRI-grids) for each month (January is the first month)ESRN-Database | 30arc-sec | etos1_30sESRI grid784635etos1_30s.zip
7Mean monthly ASCE-ETo for tall reference crop (alfalfa) (mm/month)/(30 arc-sec)ASCE-EWRI method (Allen et al., 2005) using climatic data from Hijmans et al. (2005) and Sheffield et al. (2006)the zip contains 12 rasters (ESRI-grids) for each month (January is the first month)ESRN-Database | 30arc-sec | etot1_30sESRI grid958324etot1_30s.zip
8Re-adjusted coefficient for solar radiation formula of Hargreaves-Samani (rescaled ×1000) (unitless)/(30 arc-sec)Re-calibration of Hargreaves-Samani coefficient krs=0.16-0.19 for solar radiation formula (Hargreaves and Samani, 1982, 1985) using solar radiation data (from Sheffield et al., 2006)the zip contains 1 raster (ESRI-grid) (partial weighted average of mean monthly values)ESRN-Database | 30arc-sec | krs1_30sESRI grid44302krs1_30s.zip
9Expected Mean Annual Difference/Error (MAD%) between original Hargreaves-Samani ETo and ASCE-ETo for short ref.crop (%)/(30 arc-sec)100*[(Annual ETo H-S)-(Annual ETo ASCE-short)]/(Annual ETo ASCE-short), Annual ETo H-S is estimated with the typical value chs2=0.0023the zip contains 1 raster (ESRI-grid)ESRN-Database | 30arc-sec | madhs1_30sESRI grid79345madhs1_30s.zip
10Expected Mean Annual Difference/Error (MAD%) between original Priestley-Taylor ETo and ASCE-ETo for short ref.crop (%)/(30 arc-sec)100*[(Annual ETo P-T)-(Annual ETo ASCE-short)]/(Annual ETo ASCE-short), Annual ETo P-T is estimated with the typical value apt=1.26the zip contains 1 raster (ESRI-grid)ESRN-Database | 30arc-sec | madpt1_30sESRI grid77184madpt1_30s.zip
11Expected Mean Annual Difference/Error (MAD%) between original Hargreaves-Samani radiation formula versus solar radiation data (%)/(30 arc-sec)100*[(Annual RS of H-S)-(Annual RS data)]/(Annual RS data), Annual RS H-S is estimated with the typical value krs=0.17 and RS obtained from Sheffield et al. (2006)the zip contains 1 raster (ESRI-grid)ESRN-Database | 30arc-sec | madrs1_30sESRI grid57097madrs1_30s.zip
12Re-adjusted Priestley-Taylor coefficient for short ref.crop ETo (rescaled ×100) (unitless)/(2.5 arc-min)Re-calibration of Priestley-Taylor coefficient apt=1.26 for ETo method (Priestley and Taylor, 1972) using ASCE-EWRI method (Allen et al., 2005) for short ref.cropthe zip contains 1 raster (ESRI-grid) (partial weighted average of mean monthly values)ESRN-Database | 2-5arc-min | apts2_2-5mESRI grid4647apts2_2-5m.zip
13Re-adjusted Priestley-Taylor coefficient for tall ref.crop ETo (rescaled ×100) (unitless)/(2.5 arc-min)Re-calibration of Priestley-Taylor coefficient apt=1.26 for ETo method (Priestley and Taylor, 1972) using ASCE-EWRI method (Allen et al., 2005) for tall ref.cropthe zip contains 1 raster (ESRI-grid) (partial weighted average of mean monthly values)ESRN-Database | 2-5arc-min | aptt2_2-5mESRI grid5297aptt2_2-5m.zip
14Re-adjusted Hargreaves-Samani coefficient for short ref.crop ETo (rescaled ×100,000) (unitless)/(2.5 arc-min)Re-calibration of Hargreaves-Samani coefficient chs2=0.0023 for ETo method (Hargreaves and Samani, 1982, 1985) using ASCE-EWRI method (Allen et al., 2005) for short ref.cropthe zip contains 1 raster (ESRI-grid) (partial weighted average of mean monthly values)ESRN-Database | 2-5arc-min | chs2s2_2-5mESRI grid5434chs2s2_2-5m.zip
15Re-adjusted Hargreaves-Samani coefficient for tall ref.crop ETo (rescaled ×100,000) (unitless)/(2.5 arc-min)Re-calibration of Hargreaves-Samani coefficient chs2=0.0023 for ETo method (Hargreaves and Samani, 1982, 1985) using ASCE-EWRI method (Allen et al., 2005) for tall ref.cropthe zip contains 1 raster (ESRI-grid) (partial weighted average of mean monthly values)ESRN-Database | 2-5arc-min | chs2t2_2-5mESRI grid6535chs2t2_2-5m.zip
16Hargeaves-Samani versus Priestley-Taylor (comparison between original methods versus ASCE-short) (DMADhp) (%)/(2.5 arc-min)abs(madhs)-abs(madpt), higher negative values suggest better performance of original Hargreaves-Samani ETo method while higher positive values suggest better performance of original Priestley-Taylor ETo method using as reference the ASCE-shortthe zip contains 1 raster (ESRI-grid)ESRN-Database | 2-5arc-min | dmadhp2_2-5mESRI grid4660dmadhp2_2-5m.zip
17Mean monthly ASCE-ETo for short reference crop (clipped grass) (mm/month)/(2.5 arc-min)ASCE-EWRI method (Allen et al., 2005) using climatic data from Hijmans et al. (2005) and Sheffield et al. (2006)the zip contains 12 rasters (ESRI-grids) for each month (January is the first month)ESRN-Database | 2-5arc-min | etos2_2-5mESRI grid46007etos2_2-5m.zip
18Mean monthly ASCE-ETo for tall reference crop (alfalfa) (mm/month)/(2.5 arc-min)ASCE-EWRI method (Allen et al., 2005) using climatic data from Hijmans et al. (2005) and Sheffield et al. (2006)the zip contains 12 rasters (ESRI-grids) for each month (January is the first month)ESRN-Database | 2-5arc-min | etot2_2-5mESRI grid54320etot2_2-5m.zip
19Re-adjusted coefficient for solar radiation formula of Hargreaves-Samani (rescaled ×1000) (unitless)/(2.5 arc-min)Re-calibration of Hargreaves-Samani coefficient krs=0.16-0.19 for solar radiation formula (Hargreaves and Samani, 1982, 1985) using solar radiation data (from Sheffield et al., 2006)the zip contains 1 raster (ESRI-grid) (partial weighted average of mean monthly values)ESRN-Database | 2-5arc-min | krs2_2-5mESRI grid3036krs2_2-5m.zip
20Expected Mean Annual Difference/Error (MAD%) between original Hargreaves-Samani ETo and ASCE-ETo for short ref.crop (%)/(2.5 arc-min)100*[(Annual ETo H-S)-(Annual ETo ASCE-short)]/(Annual ETo ASCE-short), Annual ETo H-S is estimated with the typical value chs2=0.0023the zip contains 1 raster (ESRI-grid)ESRN-Database | 2-5arc-min | madhs2_2-5mESRI grid4467madhs2_2-5m.zip
21Expected Mean Annual Difference/Error (MAD%) between original Priestley-Taylor ETo and ASCE-ETo for short ref.crop (%)/(2.5 arc-min)100*[(Annual ETo P-T)-(Annual ETo ASCE-short)]/(Annual ETo ASCE-short), Annual ETo P-T is estimated with the typical value apt=1.26the zip contains 1 raster (ESRI-grid)ESRN-Database | 2-5arc-min | madpt2_2-5mESRI grid4499madpt2_2-5m.zip
22Expected Mean Annual Difference/Error (MAD%) between original Hargreaves-Samani radiation formula versus solar radiation data (%)/(2.5 arc-min)100*[(Annual RS of H-S)-(Annual RS data)]/(Annual RS data), Annual RS H-S is estimated with the typical value krs=0.17 and RS obtained from Sheffield et al. (2006)the zip contains 1 raster (ESRI-grid)ESRN-Database | 2-5arc-min | madrs2_2-5mESRI grid3493madrs2_2-5m.zip
23Re-adjusted Priestley-Taylor coefficient for short ref.crop ETo (rescaled ×100) (unitless)/(5 arc-min)Re-calibration of Priestley-Taylor coefficient apt=1.26 for ETo method (Priestley and Taylor, 1972) using ASCE-EWRI method (Allen et al., 2005) for short ref.cropthe zip contains 1 raster (ESRI-grid) (partial weighted average of mean monthly values)ESRN-Database | 5arc-min | apts3_5mESRI grid1336apts3_5m.zip
24Re-adjusted Priestley-Taylor coefficient for tall ref.crop ETo (rescaled ×100) (unitless)/(5 arc-min)Re-calibration of Priestley-Taylor coefficient apt=1.26 for ETo method (Priestley and Taylor, 1972) using ASCE-EWRI method (Allen et al., 2005) for tall ref.cropthe zip contains 1 raster (ESRI-grid) (partial weighted average of mean monthly values)ESRN-Database | 5arc-min | aptt3_5mESRI grid1532aptt3_5m.zip
25Re-adjusted Hargreaves-Samani coefficient for short ref.crop ETo (rescaled ×100,000) (unitless)/(5 arc-min)Re-calibration of Hargreaves-Samani coefficient chs2=0.0023 for ETo method (Hargreaves and Samani, 1982, 1985) using ASCE-EWRI method (Allen et al., 2005) for short ref.cropthe zip contains 1 raster (ESRI-grid) (partial weighted average of mean monthly values)ESRN-Database | 5arc-min | chs2s3_5mESRI grid1546chs2s3_5m.zip
26Re-adjusted Hargreaves-Samani coefficient for tall ref.crop ETo (rescaled ×100,000) (unitless)/(5 arc-min)Re-calibration of Hargreaves-Samani coefficient chs2=0.0023 for ETo method (Hargreaves and Samani, 1982, 1985) using ASCE-EWRI method (Allen et al., 2005) for tall ref.cropthe zip contains 1 raster (ESRI-grid) (partial weighted average of mean monthly values)ESRN-Database | 5arc-min | chs2t3_5mESRI grid1876chs2t3_5m.zip
27Hargeaves-Samani versus Priestley-Taylor (comparison between original methods versus ASCE-short) (DMADhp) (%)/(5 arc-min)abs(madhs)-abs(madpt), higher negative values suggest better performance of original Hargreaves-Samani ETo method while higher positive values suggest better performance of original Priestley-Taylor ETo method using as reference the ASCE-shortthe zip contains 1 raster (ESRI-grid)ESRN-Database | 5arc-min | dmadhp3_5mESRI grid1317dmadhp3_5m.zip
28Mean monthly ASCE-ETo for short reference crop (clipped grass) (mm/month)/(5 arc-min)ASCE-EWRI method (Allen et al., 2005) using climatic data from Hijmans et al. (2005) and Sheffield et al. (2006)the zip contains 12 rasters (ESRI-grids) for each month (January is the first month)ESRN-Database | 5arc-min | etos3_5mESRI grid13270etos3_5m.zip
29Mean monthly ASCE-ETo for tall reference crop (alfalfa) (mm/month)/(5 arc-min)ASCE-EWRI method (Allen et al., 2005) using climatic data from Hijmans et al. (2005) and Sheffield et al. (2006)the zip contains 12 rasters (ESRI-grids) for each month (January is the first month)ESRN-Database | 5arc-min | etot3_5mESRI grid15634etot3_5m.zip
30Re-adjusted coefficient for solar radiation formula of Hargreaves-Samani (rescaled ×1000) (unitless)/(5 arc-min)Re-calibration of Hargreaves-Samani coefficient krs=0.16-0.19 for solar radiation formula (Hargreaves and Samani, 1982, 1985) using solar radiation data (from Sheffield et al., 2006)the zip contains 1 raster (ESRI-grid) (partial weighted average of mean monthly values)ESRN-Database | 5arc-min | krs3_5mESRI grid950krs3_5m.zip
31Expected Mean Annual Difference/Error (MAD%) between original Hargreaves-Samani ETo and ASCE-ETo for short ref.crop (%)/(5 arc-min)100*[(Annual ETo H-S)-(Annual ETo ASCE-short)]/(Annual ETo ASCE-short), Annual ETo H-S is estimated with the typical value chs2=0.0023the zip contains 1 raster (ESRI-grid)ESRN-Database | 5arc-min | madhs3_5mESRI grid1264madhs3_5m.zip
32Expected Mean Annual Difference/Error (MAD%) between original Priestley-Taylor ETo and ASCE-ETo for short ref.crop (%)/(5 arc-min)100*[(Annual ETo P-T)-(Annual ETo ASCE-short)]/(Annual ETo ASCE-short), Annual ETo P-T is estimated with the typical value apt=1.26the zip contains 1 raster (ESRI-grid)ESRN-Database | 5arc-min | madpt3_5mESRI grid1281madpt3_5m.zip
33Expected Mean Annual Difference/Error (MAD%) between original Hargreaves-Samani radiation formula versus solar radiation data (%)/(5 arc-min)100*[(Annual RS of H-S)-(Annual RS data)]/(Annual RS data), Annual RS H-S is estimated with the typical value krs=0.17 and RS obtained from Sheffield et al. (2006)the zip contains 1 raster (ESRI-grid)ESRN-Database | 5arc-min | madrs3_5mESRI grid1029madrs3_5m.zip
34Re-adjusted Priestley-Taylor coefficient for short ref.crop ETo (rescaled ×100) (unitless)/(10 arc-min)Re-calibration of Priestley-Taylor coefficient apt=1.26 for ETo method (Priestley and Taylor, 1972) using ASCE-EWRI method (Allen et al., 2005) for short ref.cropthe zip contains 1 raster (ESRI-grid) (partial weighted average of mean monthly values)ESRN-Database | 10arc-min | apts4_10mESRI grid392apts4_10m.zip
35Re-adjusted Priestley-Taylor coefficient for tall ref.crop ETo (rescaled ×100) (unitless)/(10 arc-min)Re-calibration of Priestley-Taylor coefficient apt=1.26 for ETo method (Priestley and Taylor, 1972) using ASCE-EWRI method (Allen et al., 2005) for tall ref.cropthe zip contains 1 raster (ESRI-grid) (partial weighted average of mean monthly values)ESRN-Database | 10arc-min | aptt4_10mESRI grid447aptt4_10m.zip
36Re-adjusted Hargreaves-Samani coefficient for short ref.crop ETo (rescaled ×100,000) (unitless)/(10 arc-min)Re-calibration of Hargreaves-Samani coefficient chs2=0.0023 for ETo method (Hargreaves and Samani, 1982, 1985) using ASCE-EWRI method (Allen et al., 2005) for short ref.cropthe zip contains 1 raster (ESRI-grid) (partial weighted average of mean monthly values)ESRN-Database | 10arc-min | chs2s4_10mESRI grid450chs2s4_10m.zip
37Re-adjusted Hargreaves-Samani coefficient for tall ref.crop ETo (rescaled ×100,000) (unitless)/(10 arc-min)Re-calibration of Hargreaves-Samani coefficient chs2=0.0023 for ETo method (Hargreaves and Samani, 1982, 1985) using ASCE-EWRI method (Allen et al., 2005) for tall ref.cropthe zip contains 1 raster (ESRI-grid) (partial weighted average of mean monthly values)ESRN-Database | 10arc-min | chs2t4_10mESRI grid540chs2t4_10m.zip
38Hargeaves-Samani versus Priestley-Taylor (comparison between original methods versus ASCE-short) (DMADhp) (%)/(10 arc-min)abs(madhs)-abs(madpt), higher negative values suggest better performance of original Hargreaves-Samani ETo method while higher positive values suggest better performance of original Priestley-Taylor ETo method using as reference the ASCE-shortthe zip contains 1 raster (ESRI-grid)ESRN-Database | 10arc-min | dmadhp4_10mESRI grid380dmadhp4_10m.zip
39Mean monthly ASCE-ETo for short reference crop (clipped grass) (mm/month)/(10 arc-min)ASCE-EWRI method (Allen et al., 2005) using climatic data from Hijmans et al. (2005) and Sheffield et al. (2006)the zip contains 12 rasters (ESRI-grids) for each month (January is the first month)ESRN-Database | 10arc-min | etos4_10mESRI grid3903etos4_10m.zip
40Mean monthly ASCE-ETo for tall reference crop (alfalfa) (mm/month)/(10 arc-min)ASCE-EWRI method (Allen et al., 2005) using climatic data from Hijmans et al. (2005) and Sheffield et al. (2006)the zip contains 12 rasters (ESRI-grids) for each month (January is the first month)ESRN-Database | 10arc-min | etot4_10mESRI grid4550etot4_10m.zip
41Re-adjusted coefficient for solar radiation formula of Hargreaves-Samani (rescaled ×1000) (unitless)/(10 arc-min)Re-calibration of Hargreaves-Samani coefficient krs=0.16-0.19 for solar radiation formula (Hargreaves and Samani, 1982, 1985) using solar radiation data (from Sheffield et al., 2006)the zip contains 1 raster (ESRI-grid) (partial weighted average of mean monthly values)ESRN-Database | 10arc-min | krs4_10mESRI grid302krs4_10m.zip
42Expected Mean Annual Difference/Error (MAD%) between original Hargreaves-Samani ETo and ASCE-ETo for short ref.crop (%)/(10 arc-min)100*[(Annual ETo H-S)-(Annual ETo ASCE-short)]/(Annual ETo ASCE-short), Annual ETo H-S is estimated with the typical value chs2=0.0023the zip contains 1 raster (ESRI-grid)ESRN-Database | 10arc-min | madhs4_10mESRI grid366madhs4_10m.zip
43Expected Mean Annual Difference/Error (MAD%) between original Priestley-Taylor ETo and ASCE-ETo for short ref.crop (%)/(10 arc-min)100*[(Annual ETo P-T)-(Annual ETo ASCE-short)]/(Annual ETo ASCE-short), Annual ETo P-T is estimated with the typical value apt=1.26the zip contains 1 raster (ESRI-grid)ESRN-Database | 10arc-min | madpt4_10mESRI grid370madpt4_10m.zip
44Expected Mean Annual Difference/Error (MAD%) between original Hargreaves-Samani radiation formula versus solar radiation data (%)/(10 arc-min)100*[(Annual RS of H-S)-(Annual RS data)]/(Annual RS data), Annual RS H-S is estimated with the typical value krs=0.17 and RS obtained from Sheffield et al. (2006)the zip contains 1 raster (ESRI-grid)ESRN-Database | 10arc-min | madrs4_10mESRI grid304madrs4_10m.zip
45Re-adjusted Priestley-Taylor coefficient for short ref.crop ETo (rescaled ×100) (unitless)/(0.5 deg)Re-calibration of Priestley-Taylor coefficient apt=1.26 for ETo method (Priestley and Taylor, 1972) using ASCE-EWRI method (Allen et al., 2005) for short ref.cropthe zip contains 1 raster (ESRI-grid) (partial weighted average of mean monthly values)ESRN-Database | 0-5deg | apts5_0-5dESRI grid63apts5_0-5d.zip
46Re-adjusted Priestley-Taylor coefficient for tall ref.crop ETo (rescaled ×100) (unitless)/(0.5 deg)Re-calibration of Priestley-Taylor coefficient apt=1.26 for ETo method (Priestley and Taylor, 1972) using ASCE-EWRI method (Allen et al., 2005) for tall ref.cropthe zip contains 1 raster (ESRI-grid) (partial weighted average of mean monthly values)ESRN-Database | 0-5deg | aptt5_0-5dESRI grid69aptt5_0-5d.zip
47Re-adjusted Hargreaves-Samani coefficient for short ref.crop ETo (rescaled ×100,000) (unitless)/(0.5 deg)Re-calibration of Hargreaves-Samani coefficient chs2=0.0023 for ETo method (Hargreaves and Samani, 1982, 1985) using ASCE-EWRI method (Allen et al., 2005) for short ref.cropthe zip contains 1 raster (ESRI-grid) (partial weighted average of mean monthly values)ESRN-Database | 0-5deg | chs2s5_0-5dESRI grid71chs2s5_0-5d.zip
48Re-adjusted Hargreaves-Samani coefficient for tall ref.crop ETo (rescaled ×100,000) (unitless)/(0.5 deg)Re-calibration of Hargreaves-Samani coefficient chs2=0.0023 for ETo method (Hargreaves and Samani, 1982, 1985) using ASCE-EWRI method (Allen et al., 2005) for tall ref.cropthe zip contains 1 raster (ESRI-grid) (partial weighted average of mean monthly values)ESRN-Database | 0-5deg | chs2t5_0-5dESRI grid82chs2t5_0-5d.zip
49Hargeaves-Samani versus Priestley-Taylor (comparison between original methods versus ASCE-short) (DMADhp) (%)/(0.5 deg)abs(madhs)-abs(madpt), higher negative values suggest better performance of original Hargreaves-Samani ETo method while higher positive values suggest better performance of original Priestley-Taylor ETo method using as reference the ASCE-shortthe zip contains 1 raster (ESRI-grid)ESRN-Database | 0-5deg | dmadhp5_0-5dESRI grid60dmadhp5_0-5d.zip
50Mean monthly ASCE-ETo for short reference crop (clipped grass) (mm/month)/(0.5 deg)ASCE-EWRI method (Allen et al., 2005) using climatic data from Hijmans et al. (2005) and Sheffield et al. (2006)the zip contains 12 rasters (ESRI-grids) for each month (January is the first month)ESRN-Database | 0-5deg | etos5_0-5dESRI grid647etos5_0-5d.zip
51Mean monthly ASCE-ETo for tall reference crop (alfalfa) (mm/month)/(0.5 deg)ASCE-EWRI method (Allen et al., 2005) using climatic data from Hijmans et al. (2005) and Sheffield et al. (2006)the zip contains 12 rasters (ESRI-grids) for each month (January is the first month)ESRN-Database | 0-5deg | etot5_0-5dESRI grid728etot5_0-5d.zip
52Re-adjusted coefficient for solar radiation formula of Hargreaves-Samani (rescaled ×1000) (unitless)/(0.5 deg)Re-calibration of Hargreaves-Samani coefficient krs=0.16-0.19 for solar radiation formula (Hargreaves and Samani, 1982, 1985) using solar radiation data (from Sheffield et al., 2006)the zip contains 1 raster (ESRI-grid) (partial weighted average of mean monthly values)ESRN-Database | 0-5deg | krs5_0-5dESRI grid55krs5_0-5d.zip
53Expected Mean Annual Difference/Error (MAD%) between original Hargreaves-Samani ETo and ASCE-ETo for short ref.crop (%)/(0.5 deg)100*[(Annual ETo H-S)-(Annual ETo ASCE-short)]/(Annual ETo ASCE-short), Annual ETo H-S is estimated with the typical value chs2=0.0023the zip contains 1 raster (ESRI-grid)ESRN-Database | 0-5deg | madhs5_0-5dESRI grid59madhs5_0-5d.zip
54Expected Mean Annual Difference/Error (MAD%) between original Priestley-Taylor ETo and ASCE-ETo for short ref.crop (%)/(0.5 deg)100*[(Annual ETo P-T)-(Annual ETo ASCE-short)]/(Annual ETo ASCE-short), Annual ETo P-T is estimated with the typical value apt=1.26the zip contains 1 raster (ESRI-grid)ESRN-Database | 0-5deg | madpt5_0-5dESRI grid59madpt5_0-5d.zip
55Expected Mean Annual Difference/Error (MAD%) between original Hargreaves-Samani radiation formula versus solar radiation data (%)/(0.5 deg)100*[(Annual RS of H-S)-(Annual RS data)]/(Annual RS data), Annual RS H-S is estimated with the typical value krs=0.17 and RS obtained from Sheffield et al. (2006)the zip contains 1 raster (ESRI-grid)ESRN-Database | 0-5deg | madrs5_0-5dESRI grid52madrs5_0-5d.zip