“…SIF has a small‐amplitude signal, so it was not possible to observe it until very recently. SIF observations have been shown to be directly pertinent to estimate crop photosynthesis (Guanter et al, 2014) and yield (Guan et al, 2016), GPP across ecosystems (Lee et al, 2015; Yang et al, 2015; Zhang, Xiao, Jin, et al, 2016), water stress (Guan et al, 2015; Konings et al, 2017; Sun et al, 2015; Zhang, Xiao, Guanter, et al, 2016), biosphere‐atmosphere interactions (Green et al, 2017), surface turbulent fluxes (Alemohammad et al, 2017), and phenology, especially in northern latitudes where vegetation indices and their seasonality are polluted by the snow albedo (Jeong et al, 2017). One other advantage of SIF is that it responds to only the PAR absorbed by chlorophyll of the canopy, whereas typical optical (absorbed photosynthetic active radiation) APAR or fPAR products reflect the PAR absorbed by the entire canopy (nonphotosynthetic and photosynthetic; Song et al, 2013).…”