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Crop evapotranspiration : guidelines for computing crop water requirements

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TLDR
In this paper, an updated procedure for calculating reference and crop evapotranspiration from meteorological data and crop coefficients is presented, based on the FAO Penman-Monteith method.
Abstract
(First edition: 1998, this reprint: 2004). This publication presents an updated procedure for calculating reference and crop evapotranspiration from meteorological data and crop coefficients. The procedure, first presented in FAO Irrigation and Drainage Paper No. 24, Crop water requirements, in 1977, allows estimation of the amount of water used by a crop, taking into account the effect of the climate and the crop characteristics. The publication incorporates advances in research and more accurate procedures for determining crop water use as recommended by a panel of high-level experts organised by FAO in May 1990. The first part of the guidelines includes procedures for determining reference crop evapotranspiration according to the FAO Penman-Monteith method. These are followed by updated procedures for estimating the evapotranspiration of different crops for different growth stages and ecological conditions.

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References
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A Penman for All Seasons

TL;DR: In this article, ten forms of the Penman combination evapotranspiration equation are reviewed and compared with lysimeter estimates at three locations, including three locations in the US.
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Comparison of aerodynamic and energy budget estimates of fluxes over a pine forest

TL;DR: In this paper, the authors show that profile gradients fall consistently short of independent energy-balance estimates by a factor of 2 to 3 in unstable and near-neutral conditions (Richardson number, Ri, in the range −0·4 to +0·01), whereas for Ri > + 0·02 no similar discrepancy is detected.
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Potential evapotranspiration estimates by the approximate energy balance method of Penman

TL;DR: The energy balance approximation of Penman, used to estimate potential evapotranspiration, was tested for daily estimates on 37 days during 1956 and 1957 as mentioned in this paper, and the absolute values of the Penman estimates were much too small.
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Transport of Gases To and From Grass and Grass-Like Surfaces

TL;DR: In this article, a radioactive vapour of thorium-B (lead-212) has been used to measure the vertical flux of a gas to grass and similar surfaces in a wind tunnel, as a function of the difference in vapour concentration between the air and the surface.
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Estimation of soil heat flux from net radiation during the growth of alfalfa

TL;DR: In this paper, the authors used spectral vegetation indices to estimate soil heat flux from net radiation measurements and found that the spectral vegetation index was well-fitted by a linearly decreasing function of a near-IR to Red ratio over two regrowth cycles.
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