Daily reference evapotranspiration estimates by the Penman-Monteith equation in Southern Italy. Constant vs. variable canopy resistance

By Pasquale Steduto, M. Todorović, A. Caliandro, P. Rubino. 2003

69 citations recorded by the source corpus.

Subfields: Global and Planetary Change, Soil Science, Water Science and Technology

View Paper: https://www.semanticscholar.org/paper/84d852ab942726dc94e45862e1d0af367d9bdf78

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In Global and Planetary Change

In Soil Science

In Water Science and Technology

R. G. Allen

Citations in the corpus

A recommendation on standardized surface resistance for hourly calculation of reference ETo by the FAO56 Penman-Monteith method (2006, methodology): “…for daytime hourly periods is less than 70 s m 1 in the FAO-PM for the standardized height of 0.12 m for clipped grass, and that lower values for rs provide better agreement with ETo measurements (Allen et al., 1996; Ventura et al., 1999; Todorovic, 1999; Wright et al., 2000; Steduto et al., 2003).”
A simple parameterization of bulk canopy resistance from climatic variables for estimating hourly evapotranspiration (2006, methodology): “Results found by others authors (Steduto et al., 2003; Alves and Pereira, 2000; Rana et al., 1997) seem to show a linear relationship between these variables on an hourly basis.”
Parameterizing canopy resistance using mechanistic and semi‐empirical estimates of hourly evapotranspiration: critical evaluation for irrigated crops in the Mediterranean (2011, methodology): “Furthermore, Todorovic (1999) and then Steduto et al. (2003) did not clearly define the crop water situations in which the TD approach can be applied.”
Reference grass evapotranspiration with reduced data sets: Parameterization of the FAO Penman-Monteith temperature approach and the Hargeaves-Samani equation using local climatic variables (2020, methodology): “Former lysimeter grass ETo studies were developed focusing on the ET processes and their results contributed to improve the use of the PM-ETo equation, namely in advective environments (Berengena and Gavilán, 2005), and mainly proposing different day and night bulk surface resistances (Todorovic, 19”