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- W3008126056 abstract "Abstract Crago et al. published two papers in Water Resources Research in 2016 and 2018, respectively, which discussed recent generalized complementary evaporation relationships; they recommended that the lower boundary condition of the Generalized Nonlinear Advection‐Aridity (GNAA) model proposed by Brutsaert (2015, https://doi.org/10.1002/2015WR017720 ) should be modified to y = 0 at x = x min , where x min ∈[0,1]. First, it is shown herein that the rescaled complementary relationship (CR) y = X, proposed by Crago et al., does not advance the analysis forward, but that instead the rescaling is tantamount to a reversion to an earlier linear and more traditional asymmetric complementary model, in which the parameter b is a function of x min . In fact, at x min = 0, y = X the rescaled formulation becomes physically unrealistic. The second part of this comment deals with the extended quartic form of GNAA model. The nature of the adjustable parameter c in this extended formulation is further explored, and it is shown that while its lower limit is −1, calibration with actual data can result in values in excess of 2. Such calibration allows then the estimation of x min as a function of c, that is, x min = f (c). This way, in addition to satisfying the original four boundary conditions, the extended GNAA model also satisfies the boundary condition of y = 0 at x = x min . The physical variables affecting the nature of the parameter c and its relationship with E po /E pmax will require further investigation." @default.
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- W3008126056 date "2020-03-01" @default.
- W3008126056 modified "2023-10-15" @default.
- W3008126056 title "Comment on Two Papers About the Generalized Complementary Evaporation Relationships by Crago et al." @default.
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- W3008126056 doi "https://doi.org/10.1029/2019wr026292" @default.
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