1967•JAWRA Journal of the American Water Resources AssociationRequires access

MEASURING EVAPOTRANSPIRATION FROM VEGETATION‐FILLED PRAIRIE POTHOLES IN NORTH DAKOTA1

W. S. Eisenlohr

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Abstract

Abstract Many prairie potholes in North Dakota are filled with emergent aquatic vegetation. The paper describes briefly how evapotranspiration losses were determined for such potholes using a mass‐transfer equation in which the coefficient was evaluated by means of a water budget. Vegetation, by its presence, reduces evaporation below the normal from a free water surface so much that the total seasonal (May ‐ October) evapotranspiration loss is less than the normal evaporation loss from a pothole clear of vegetation.

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What this paper is about

Abstract Many prairie potholes in North Dakota are filled with emergent aquatic vegetation. The paper describes briefly how evapotranspiration losses were determined for such potholes using a mass‐transfer equation in which the coefficient was evaluated by means of a water budget. Vegetation, by its presence, reduces evaporation below the normal from a free water surface so much that the total seasonal (May ‐ October) evapotranspiration loss is less than the normal evaporation loss from a pothole clear of vegetation.

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Available abstract

Abstract Many prairie potholes in North Dakota are filled with emergent aquatic vegetation. The paper describes briefly how evapotranspiration losses were determined for such potholes using a mass‐transfer equation in which the coefficient was evaluated by means of a water budget. Vegetation, by its presence, reduces evaporation below the normal from a free water surface so much that the total seasonal (May ‐ October) evapotranspiration loss is less than the normal evaporation loss from a pothole clear of vegetation.

Key concepts: Evapotranspiration, Vegetation (pathology), Hydrology (agriculture), Pothole (geology), Environmental science, Evaporation, Geology, Ecology

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