Spatial estimation of average daily precipitation using multiple linear regression by using topographic and wind speed variables in tropical climate

Complex topography and wind characteristics play important roles in rising air masses and in daily spatial distribution of the precipitations in complex region. As a result, its spatial discontinuity and behaviour in complex areas can affect the spatial distribution of precipitation. In this work, a...

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Main Authors: Mohd Talha, Anees, Abdullah, Khiruddin, M. Nawawi, M. N., Nik Ab Rahman, Nik Norulaini, Mt. Piah, Abd. Rahni, Syakir, M.I, Ali Khan, Mohammad Muqtada, Mohd. Omar, Abdul Kadir
Format: Indexed Article
Language:English
Published: 2018
Online Access:http://discol.umk.edu.my/id/eprint/7378/1/SPATIAL%20ESTIMATION%20OF%20AVERAGE%20DAILY%20PRECIPITATION%20USING.pdf
http://discol.umk.edu.my/id/eprint/7378/
https://journals.vgtu.lt/index.php/JEELM/article/view/6337
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Summary:Complex topography and wind characteristics play important roles in rising air masses and in daily spatial distribution of the precipitations in complex region. As a result, its spatial discontinuity and behaviour in complex areas can affect the spatial distribution of precipitation. In this work, a two-fold concept was used to consider both spatial discontinuity and topographic and wind speed in average daily spatial precipitation estimation using Inverse Distance Weighting (IDW) and Multiple Linear Regression (MLR) in tropical climates. First, wet and dry days were identified by the two methods. Then the two models based on MLR (Model 1 and Model 2) were applied on wet days to estimate the precipitation using selected predictor variables. The models were applied for month wise, season wise and year wise daily averages separately during the study period. The study reveals that, Model 1 has been found to be the best in terms of categorical statistics, R2 values, bias and special distribution patterns. However, it was found that sets of different predictor variables dominates in different months, seasons and years. Furthermore, necessities of other data for further enhancement of the results were suggested.