资源环境科技发展态势分析平台

The generalized complementary function to estimate actual evaporation, namely, the ratio of actual evaporation to Penman potential evaporation (E/E-Pen) as a function of the proportion of the radiation term in E-Pen (E-rad/E-Pen), has been increasingly recognized. Existing analytical forms of this generalized function present deficiencies because they are limited by improper boundary conditions resulting from inadequate understanding of physical constraints. In this study, its zero- and first-order boundary conditions were rigorously derived by adopting the physical constraints for E in Penman's combination theory, and a sigmoid feature of relationship between E/E-Pen and E-rad/E-Pen was derived. Minimum and maximum limits of E-rad/E-Pen were introduced based on the derived boundary conditions, and accordingly, a new sigmoid function was developed. By restricting it to be approximately equivalent to the linear advection-aridity (Brutsaert & Stricker, 1979, https://doi.org/10.1029/WR015i002p00443) function under normal environments, the new sigmoid function satisfies the upper limits of Penman's open water evaporation and Priestley-Taylor'sminimal advection evaporation in parallel. The sigmoid feature and the new sigmoid function were validated by tower-based data from FLUXNET. This work improves our understanding of the three-stage pattern of the complementary behavior, and the new function demonstrates a favorable potential for use in evaporation estimation.