Abstract
The Bowen ratiolenergy balance method using periodic reversal of the psychrometers to remove systematic errors is evaluated. Temperature and vapour‐pressure differences can be measured with accuracies of ±0.005 °C and ±1 Pa, respectively. For a 3‐m vertical separation of the psychrometers and the Bowen ratio (ß), 0 < ß < 4, the probable relative error in the forest evapotranspiration (E) is < ±15% if the temperature and vapour‐pressure gradients are large, and ranges from ±10 to ± 60% if the gradients are small. The error in E is from two to five times these values for ß < 0. Measurements of E made with the Bowen ratiolenergy balance method are compared with those made concurrently with an eddy correlation/energy balance method, a stomatal diffusion resistance method and a soil water balance method. Agreement is generally within ±20% and frequently within ±10%, well within the errors associated with the methods. © Taylor & Francis Group, LLC.
Cite
CITATION STYLE
Spittlehouse, D. L., & Black, T. A. (1980). Evaluation of the bowen ratio/energy balance method for determining forest evapotranspiration. Atmosphere - Ocean, 18(2), 98–116. https://doi.org/10.1080/07055900.1980.9649081
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