What is the Priestley–Taylor wet-surface evaporation parameter? Testing four hypotheses

Authors

Richard D. Crago, Bucknell University
Jozsef Szilagyi, Budapest University of Technology and Economics, University of Nebraska-LincolnFollow
Russell J. Qualls, University of Idaho

Date of this Version

9-8-2023

Citation

Hydrol. Earth Syst. Sci., 27, 3205–3220, 2023 https://doi.org/10.5194/hess-27-3205-2023

Comments

Used by permission.

Abstract

This study compares four different hypotheses regarding the nature of the Priestley–Taylor parameter α. They are as follows:

1. α is a universal constant.
2. The Bowen ratio (H/LE, where H is the sensible heat flux, and LE is the latent heat flux) for equilibrium (i.e., saturated air column near the surface) evaporation is a constant times the Bowen ratio at minimal advection (Andreas et al., 2013).
3. Minimal advection over a wet surface corresponds to a particular relative humidity value.
4. α is a constant fraction of the difference from the minimum value of 1 to the maximum value of α proposed by Priestley and Taylor (1972).

Formulas for α are developed for the last three hypotheses. Weather, radiation, and surface energy flux data from 171 FLUXNET eddy covariance stations were used. The condition LE_ref=LE_p >0.90 was taken as the criterion for nearly saturated conditions (where LE_ref is the reference, and LE_p is the apparent potential evaporation rate from the equation by Penman, 1948). Daily and monthly average data from the sites were obtained. All formulations for α include one model parameter which is optimized such that the root mean square error of the target variable was minimized. For each model, separate optimizations were done for predictions of the target variables α, wet-surface evaporation (α multiplied by equilibrium evaporation rate) and actual evaporation (the latter using a highly successful version of the complementary relationship of evaporation). Overall, the second and fourth hypotheses received the best support from the data.