1977
DOI: 10.1016/0022-1694(77)90010-5
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A parametric approach to station weights

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Cited by 3 publications
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“…This method divides the catchment into a series of polygons surrounding each grid and area of the polygons becomes the weight of the grid. The influence of each grid to their respective districts will be quantified and can be an optimum solution for spatial averaging of weather data (Ramaseshan and Anant, 1977). The comparison of the area weighted district wise monthly rainfall, maximum and minimum temperature of the selected CMIP-5 models (GFDL-ESM2M, MIROC5 and NorESM1-M) with IMD historical data for the period 2006-2013 has been carried out using statistical tools like root mean square error (RMSE), D-index and Pearson correlation coefficient.…”
Section: Climatic Datamentioning
confidence: 99%
“…This method divides the catchment into a series of polygons surrounding each grid and area of the polygons becomes the weight of the grid. The influence of each grid to their respective districts will be quantified and can be an optimum solution for spatial averaging of weather data (Ramaseshan and Anant, 1977). The comparison of the area weighted district wise monthly rainfall, maximum and minimum temperature of the selected CMIP-5 models (GFDL-ESM2M, MIROC5 and NorESM1-M) with IMD historical data for the period 2006-2013 has been carried out using statistical tools like root mean square error (RMSE), D-index and Pearson correlation coefficient.…”
Section: Climatic Datamentioning
confidence: 99%