FXCA20 KWBC 051559 PMDCA Tropical Discussion - International Desks NWS Weather Prediction Center College Park MD 1159 AM EDT Tue May 05 2026 Forecast Bulletin 4 May 2026 at 1600 UTC: The Bahamas and Caribbean: A frontal boundary extending from the Atlantic into The Bahamas will continue to favor low-level moisture convergence over the islands, maintaining precipitation in the region from today through Wednesday. Thunderstorms and convective activity are also expected, particularly early on Tuesday as a result of the instability generated by an eastward propagating upper-level trough, reflected at mid-levels. A slight risk for severe weather exists today over The Bahamas. On Wednesday, an upper-level high will propagate eastward from Mexico into the Gulf, bringing more stability to the region. Some upper-level diffluence is anticipated to happen along the periphery of the high causing some convection over eastern Cuba, the southern Bahamas, and Turks and Caicos. Over the eastern Caribbean, some shallow convection is likely from Wednesday through Thursday as the upper-level trough propagates, however a mid-level ridge in the Caribbean, and relatively dry air will limit precipitation in the region. Daily precipitation due to diurnal heating and local effects is likely throughout the forecast period. Mexico and Central America: Conditions are expected to remain fairly stable over Mexico through late Wednesday, with dry air prevailing in the region and a high at mid- and upper-levels. A more active precipitation pattern is expected Thursday into Friday, particularly over northeastern Mexico and along the Sierra Madre Oriental. This will happen as a frontal boundary approaches the southern United States and extends into northeastern Mexico, promoting low-level convergence in the area and increasing moisture in the region. At upper-levels, speed divergence is also expected, which combined with the presence of mid-level shortwave troughs will support convective activity and thunderstorms. The highest accumulations are anticipated to range from 20-45mm from Thursday through Friday over northeastern Mexico. Costa Rica and Panama will receive light to moderate precipitation throughout the forecast period. This rainfall pattern is linked to the conditions at lower-levels that will favor wind convergence and moisture advection, mainly from the Caribbean. The highest levels of rainfall accumulations are expected today through Wednesday, as a low-level trough propagates through the region advecting moisture, but lower accumulations are anticipated towards the end of the workweek as the precipitable water availability decreases. Tropical South America: Heavy precipitation is anticipated today through Wednesday morning over the Guianas, the Amazon Delta and the Eastern-to-Central Amazon Basin in Brazil. This precipitation is associated with the presence of the ITCZ and the NET that will promote low-level moisture convergence, while a propagating low-level trough advects moisture in the area. Upper-level diffluence is also anticipated along the periphery of the Bolivian High, promoting instability and the development of thunderstorms. Light to moderate precipitation is also expected today through Thursday over the Western Amazon Basin where a low-level trough will promote low-level convergence. Rainfall is also anticipated over the Pacific coast of Ecuador and Colombia throughout the forecast period with moisture being advected from the Pacific. With relatively weak winds at low-levels , accumulations are expected to remain on the lower end today through Wednesday. However, an increase in accumulations is likely from Wednesday through Thursday, with low-level flow perpendicular to the coast and the presence of a shortwave trough enhancing upper-level divergence. By the end of the forecast period, a drying trend is anticipated throughout the region, with most of the precipitation expected over the Eastern Amazon Basin, due to low-level convergence and over the Pacific coast due to moisture advection. Light rainfall and thunderstorms are likely over the rest of the region due to diurnal convection, moisture advection and local effects. Rivera-Torres...(WPC) $$