 A thick 10–20 m mantle of kaolinite rich (derivative of laterite) soil around the lake is stated to check flow into the lake and the theory is now that the lake is also rain fed; the lake water level is recorded to be higher at the end of the monsoon season.The average annual rainfall in the area is 2398 mm and mean annual temperature varies between 26.7 °C and 29.16 °C.Ground water table in the area is reported at depth of 3.89 m. After accounting for estimated evaporation loss of 5 MCM (million cubic metres) and water utilized for domestic use of 8 MCM (at a pumpage rate of 22 MLD), the two together account for about two-thirds of the inflow.