2000
DOI: 10.1016/s0168-1923(00)00170-2
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Simultaneous estimation of daily solar radiation and humidity from observed temperature and precipitation: an application over complex terrain in Austria

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Cited by 347 publications
(228 citation statements)
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“…Climate data used in this study were derived from Daymet, a collection of algorithms and computer software designed to interpolate and extrapolate daily meteorological observations at weather stations to produce gridded estimates of daily weather parameters (Thornton et al 1997, Thornton et al 1999, Thornton et al 2000. Daymet raster layers were derived from the native NetCDF file format in ArcGIS and were clipped using 2500-meter buffers surrounding case-control locations using the Buffer and Intersect tools.…”
Section: Climatementioning
confidence: 99%
“…Climate data used in this study were derived from Daymet, a collection of algorithms and computer software designed to interpolate and extrapolate daily meteorological observations at weather stations to produce gridded estimates of daily weather parameters (Thornton et al 1997, Thornton et al 1999, Thornton et al 2000. Daymet raster layers were derived from the native NetCDF file format in ArcGIS and were clipped using 2500-meter buffers surrounding case-control locations using the Buffer and Intersect tools.…”
Section: Climatementioning
confidence: 99%
“…Climatic influences are difficult to assess in mountainous areas, however, because complex topography produces steep gradients in the biophysical environment, and climatemonitoring stations are sparsely distributed, particularly at the highest elevations. (Thornton et al, 2000;Daly et al, 2008).…”
Section: Introductionmentioning
confidence: 99%
“…113819'W, elevation 846 m), but these may not accurately reflect the precipitation at the research site. Daily solar radiation was calculated using the Mountain Climate Simulator (Thornton et al 2000). Soil organic carbon, bulk density and fractions of sand, silt and clay at depths of 0 to 5, 5 to 15, 15 to 30, 30 to 45, 45 to 60, 60 to 90, 90 to 120, 120 to 150, 150 to 180 and 180 to 210 cm are calculated based on observation (Table 1) using linear interpolation and setting values for depths lower than 110 cm equal to the 80Á 110 cm layer.…”
Section: Modification Calibration and Simulationsmentioning
confidence: 99%