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Abstract
The use of recession coefficient in the assessment of glacier and snowmelt runoff with regard to temperature is dealt with. The variability of this coefficient due to various factors is pointed out.
Résumé
Le rôle du coefficent de tarissement dans l'écoulement provenant du glacier et de la couverture neigeuse est examiné, en soulignant sa variabilité en relation aux plusieurs facteurs.