EXPERIÊNCIA DE BALANÇO HÍDRICO DE THORNTHWAITE EM BACIA DE DRENAGEM

SANDRA BAPTISTA DA CUNHA

Resumo


A study of hidric balance using the method of Thornthwaite is presented for two distinct altimetric areas of upper Rio Grande, Rio de Janeiro State, based on data covering a period of eleven years (1967/1977). The influence of altitude over the values of temperature and precipitation in areas of the river basin is shown. The interpretation of the hydric balances is made in relation to geology, soils and vegetation cover. From the hydric point of view the region is characterized by high hydric indices and in the proximity of the watershed by high levels of excess water in soil.


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