Remotely sensed observations were used to expand the study's spatial and temporal extent and explore the behavior of sea surface temperature (SST),  currents, and winds, during the upwelling event. SST anomalies exhibited a cold tongue of seawater extending from the north-eastern coast of the Yucatan Peninsula all the way until Isla Aguada in southern Campeche, reaching a minimum SSTa during July 19th (Fig. \ref{574610}.a1). Near the coast, the bathymetric restriction off northern Campeche (20-21°N, 91°W) presented warmer anomalies during all the time of the event, and it is clear that during the time of the survey (Fig. \ref{574610}.c1), this phenomenon was weakening and retracting, showing smoother SSTa with positive values off Campeche and low-negative values off Yucatan.  Off Campeche, currents and winds are most of the time south-westward and easterly flows, respectively, and during the dates inspected this was no different (Fig. \ref{574610}.middle and lower panels).