Debitele medii zilnice vor fi relativ staționare.
Sunt posibile creşteri de niveluri şi debite pe unele râuri din zonele de deal şi munte, ca urmare a cedării apei din stratul de zăpadă.
Formațiunile de gheață (gheață la mal, pod de gheață, năboi) vor fi în restrângere, diminuare și eliminare.
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