Articles | Volume 28, issue 18
https://doi.org/10.5194/hess-28-4349-2024
https://doi.org/10.5194/hess-28-4349-2024
Research article
 | 
23 Sep 2024
Research article |  | 23 Sep 2024

Estimating the sensitivity of the Priestley–Taylor coefficient to air temperature and humidity

Ziwei Liu, Hanbo Yang, Changming Li, and Taihua Wang

Related authors

CAMELE: Collocation-Analyzed Multi-source Ensembled Land Evapotranspiration Data
Changming Li, Ziwei Liu, Wencong Yang, Zhuoyi Tu, Juntai Han, Sien Li, and Hanbo Yang
Earth Syst. Sci. Data, 16, 1811–1846, https://doi.org/10.5194/essd-16-1811-2024,https://doi.org/10.5194/essd-16-1811-2024, 2024
Short summary

Cited articles

Andreas, E. L. and Cash, B. A.: A new formulation for the Bowen ratio over saturated surfaces, J. Appl. Meteorol., 35, 1279–1289, https://doi.org/10.1175/1520-0450(1996)035<1279:anfftb>2.0.co;2, 1996. 
AsiaFlux: SWL:Suwa Lake Site, AsiaFlux [data set], http://asiaflux.net/index.php?page_id=1355, 2020. 
Assouline, S., Li, D., Tyler, S., Tanny, J., Cohen, S., Bou-Zeid, E., Parlange, M., and Katul, G. G.: On the variability of the Priestley-Taylor coefficient over water bodies, Water Resour. Res., 52, 150–163, https://doi.org/10.1002/2015wr017504, 2016. 
Bowen, I. S.: The ratio of heat losses by conduction and by evaporation from any water surface, Phys. Rev., 27, 779–787, https://doi.org/10.1103/PhysRev.27.779, 1926. 
Brutsaert, W. and Stricker, H.: An advection-aridity approach to estimate actual regional evapotranspiration, Water Resour. Res., 15, 443–450, 1979. 
Download
Short summary
The determination of the coefficient α in the Priestley–Taylor equation is empirical. Based on an atmospheric boundary layer model, we derived a physically clear and parameter-free expression to investigate the behavior of α. We showed that the temperature dominates changes in α and emphasized that the variation of α with temperature should be considered for long-term hydrological predictions. Our works advance and promote the most classical models in the field.
Share