Debitele medii zilnice vor fi relativ staționare, exceptând cursurile mijlocii și inferioare ale râurilor mari din vestul țării, unde vor fi în ușoară scădere.
Formațiunile de gheață (gheață la maluri, năboi, pod de gheață, sloiuri) existente pe majoritatea râurilor vor fi în extindere şi intensificare, putând determina, în evoluția lor, variații de niveluri și debite.
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