MEASURING EVAPOTRANSPIRATION FROM VEGETATION‐FILLED PRAIRIE POTHOLES IN NORTH DAKOTA1
W. S. Eisenlohr
Abstract
W. S. Eisenlohr
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.
OpenAlex reports 4 citations for this work. Citation counts describe recorded attention and do not establish research quality.
A contribution statement is not available in the OpenAlex record.
Method details are not available in the OpenAlex metadata.
Findings are not separately available in the OpenAlex metadata.
Limitations are not available in the OpenAlex metadata.
Application details are not available in the OpenAlex metadata.
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