An ecological change on the planet the most flighty parameter is precipitation. It causes minor and real changes in the climatic changes. The time and space analyzed on the data and the spatial and temporal patterns are introduced in the required manner. For the unpredictable data to be predicted by using the spatial interpolation techniques. The major spatial interpolation methods are categorized based on the simple and complex mathematical modeling. Those studies involve interpolation techniques such as ordinary Krigging, inverse distance weighted (IDW), Spline, etc., Most of the techniques studied the hydrological modeling and deliver hydro mapping (Younghun Jung and Venkatesh Merwade 2015). Various techniques are used for the hydrological mapping. This study involved comparing the statistical interpolation with precipitation and temperature. The cumulative values in the dataset taken from the year 2001 to the year 2013 used in the study. The monthly and the yearly mean square value calculated using the spatial interpolation techniques (Dhamodarn and Shruthi 2016). The main objective of the study is to find the topographical features and provides high-resolution climate maps using mathematical modeling. In the result of comparing the above interpolation methods in the result will produce the high-resolution climate maps and generate the geographical patterns. Based on the study will produce climate change in the environment like disaster, flood, landslide. The comparative study of interpolation methods and mean variation can be resulted and used for the further implementation of spatial climatic condition and decision support system to the society. The area has undergone the study is Adyar river, situated in latitude 13.0012° N, Longitude 80.2565° E. Inverse Distance Weighted interpolation methods are analyzed by using the Geostatistical tool ArcGIS.