“…The Shuttleworth-Wallace equation is used to estimate potential evapotranspiration considering crop residue and partial canopy cover effects (Ma et al, 2012). The model contains multiple crop growth modules including the DSSAT suite of crop modules (CROPGRO and CERES) and the HERMES module (Ma, Hoogenboom, Ahuja, Nielsen, & Ascough, 2005;Sima et al, 2020). The CROPGRO has detailed simulation of soybean phenology, yield components, N 2 fixation, and environmental stresses (Boote, Jones, & Hoogenboom, 1998;Jones et al, 2003) and has been evaluated under elevated CO 2 conditions (Alagarswamy, Boote, Allen, & Jones, 2006).…”