摘要：Water balance in Căliman Mountains. The water balance from the
largest and most expanded volcanic massif in Romania was calculated using the
equation developed by M.I. Lvovici in 1974: Xo = Yo + Zo; Xo = So + Wo = So +
(Uo + Z o). The assessment of the balance components was based on data from 12
hydrometric stations, four meteorological stations and eight pluviometric stations.
The range of years for which the multilingual average values were calculated was
1961-2010. The correlations between the main balance components and the
altitude of the relief allowed the identification of the areas where their spatial
distribution has similar peculiarities. The spatial distribution of the main
components of the water balance was made on altitude intervals and hydrographic
basins. For each element of the balance sheet, maps have been prepared, which
allowed valuation of the values corresponding to the main river basins in the
studied region (Someş, Mureş and Siret).
