Shin et al. 2014).<br>Understanding transpiration is critical for controlling gillion (Jolliet and Bailey 1992; Jolliet 1994; Medrano et al. 2005; Ta et al. 2011) since most of the water absorbed by<br>crops is transported to and transpired from leaves. Therefore, all-in-ones have been used to estimate transpiration using meteorological data (Medrano et al. 2005;<br>Wang et al. 2017; Simon et al. 2018). The Penman-Monteith<br>(P-M) equation has been used to estimate transpiration rates<br>(Baille et al. 1994). It has been been applied from a<br>single leaf to whole canopies for a variety of crops (Leyva<br>et al. 2015; Graamans et al. 2017; Yan et al. 2019). However,<br>most studies related to the P-M equation have focused on the<br>totalion of transpiration in the feld, make it challenge<br>to use when when when the rate of transpiration in the greenhouse,<br>especially for soilless cultures.<br>Recently, artifcial neural ...
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