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Different regions of the world have different geomorphologic characteristics. This, therefore, means that measurements of certain hydrological variables of other regions may not be directly applied to other areas. As the result, any successful hydrological experiment conducted in one place may not conclusively imply success elsewhere. Two simple methods have demonstrated that surface run-off water has contributed to stream flow or increased in water level. These methods have limitation to when rain storms from tropical convective clouds are occurring both over head the river and also within the vicinity. The first method involves rainfall that has fallen in areas where …
