The hydrological cycle refers to the continuous movement of water on, above and below the surface of the earth. It mainly involves the processes of evaporation, condensation, precipitation, infiltration, percolation, interception and runoff/overland flows. The main source of energy that drives the cycle is solar energy and therefore the main changes in energy involve changes in temperature. When surface water is heated, it gains energy and changes from liquid state to gaseous state. This results in a cooling effect to the surrounding region (Arctic Climatology and Meteorology) Transpiration also contributes in adding water vapor in the atmosphere; this is referred ...
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