Debitele medii zilnice vor fi relativ staționare, cu tendință de 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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