| Fig. 1 and 2 reveal a view of the EASTPAC area that captures a well-
developed tropical cloud band. The intense convection within the band
implies a convergence of flow commonly associated with a sharp tropical
trough. Such bands in the eastern Pacific rarely develop further;
however, their presence indicates the position of a trough and an
associated sharp shift in wind direction that could be important for
operations aboard a ship transiting through the area. |