“…Crop data can be estimated using acquired earth observation (EO) data, along the crop growth cycle, at time intervals suitable for the detection of changes in crop phenology (D'Urso & Calera Belmonte, 2006;Vilar, 2015;Vilar et al, 2015;Navarro et al, 2016;Rolim et al, 2016). Presently, the availability of free and open access to high spatial resolution EO data with a short revisit time allows for accurate crop parameter estimation as well as crop growth cycle characterization, improving the identification of each growth cycle stage, which is often imperceptible when lower temporal resolution data are used (El Hajj et al, 2009;D'Urso et al, 2010;Ramme et al, 2010;Johann et al, 2013;Johann et al, 2016;Navarro et al, 2016;Rolim et al, 2016;Grzegozewski et al, 2017;Toureiro et al, 2017). EO methodologies have been widely used for crop evapotranspiration (ETc) and IWR estimation because of the reflective properties of vegetation that allow one to estimate crop biophysical parameters and plant processes such as transpiration (Neale et al, 1989;Calera Belmonte et al, 2005;D'Urso et al, 2010;Paço et al, 2014;Vuolo et al, 2015;Ferreira et al, 2016;Oliveira et al, 2016).…”