“…These profiles have proved to be fruitful measurements for diverse applications. Downwelling irradiances at various wavelengths have been implied in the analysis of the bio-optical behavior of the global ocean [ 4 ] and the dynamics of dissolved organic matter [ 5 , 6 ], and for the validation of space-based ocean color measurements and products [ 7 , 8 , 9 , 10 , 11 , 12 , 13 ]. Besides, E d and PAR have been widely used to understand particulate organic carbon fluxes and export [ 14 , 15 , 16 ], to study phytoplankton dynamics [ 17 , 18 , 19 , 20 , 21 , 22 , 23 , 24 , 25 ], and to improve numerical and radiative-transfer models [ 26 , 27 ].…”