FXCA20 KWBC 041816 PMDCA Tropical Discussion - International Desks NWS Weather Prediction Center College Park MD 216 PM EDT Mon May 04 2026 Forecast Bulletin 4 May 2026 at 1800 UTC: The Bahamas and Caribbean: A frontal boundary extending from the Atlantic into the Gulf is anticipated to enhance precipitation over the Bahamas and Cuba, starting today through Tuesday morning. An eastward-propagating upper-level trough over the eastern U.S. will also increase upper-level divergence, particularly over The Bahamas, promoting the development of thunderstorms and convective activity. A slight risk for severe weather exists from today through Tuesday morning for The Bahamas. Remnants of the frontal boundary will continue to bring light precipitation into the Bahamas and Cuba from Tuesday through Wednesday. Less precipitation and more stable conditions are anticipated from Wednesday through Thursday, as an upper-level ridge, reflected at mid-levels moves from Mexico into the Gulf. Elsewhere in the Caribbean, light precipitation due to diurnal heating, and local effects can be anticipated throughout the forecast period, producing daily accumulations between 05-15mm. As the upper-level trough, currently affecting the Bahamas, propagates and reaches the eastern Caribbean some shallow convection is expected over Hispaniola and Puerto Rico from Wednesday through Thursday; however, low levels of precipitable water will limit accumulations of rainfall. Mexico and Central America: Over most of Mexico, conditions are expected to remain fairly stable throughout the forecast period with a ridge dominating at mid- and upper-levels and low precipitable water prevailing in the region. Light precipitation can be expected today through Tuesday over the Yucatan Peninsula, and Belize, southwestern Mexico and portions of Guatemala, driven by low-level troughs advecting moisture into the region and enhancing low-level convergence. Rainfall and convective activity are anticipated every day over portions of Nicaragua, Costa Rica and Panama with deep moisture available in the region. The presence of low-level troughs will further enhance the advection of moisture from the Caribbean into the region. At mid-levels, the presence of a shortwave trough will enhance instability over Nicaragua and Costa Rica particularly on Tuesday. At upper-levels an increase in divergence is anticipated over Costa Rica, further increasing precipitation from Tuesday through Wednesday morning. Tropical South America: Heavy precipitation and thunderstorms are expected across the region each day. The main drivers of precipitation will be low-level convergence, moisture advection, orographic lifting, diurnal heating and local effects. Today through Tuesday morning the heaviest precipitation is anticipated over the western and central Amazon region, as a low-level trough over Peru enhances low-level moisture convergence over the region and deep moisture is advected in the area. Additionally, an enhanced upper-level divergence is anticipated along the periphery of the Bolivian High which will persist throughout the forecast period. From Tuesday through Wednesday, the presence of the ITCZ and the Near Equatorial Trough (NET) will bring the heaviest precipitation to the Amazon Delta, and Eastern Amazon region by increasing moisture convergence at low-levels. Additionally, the propagation of a low-level trough will bring precipitation into the Guianas. Light to moderate precipitation is likely to occur over the Pacific Coast of Colombia and Ecuador from Tuesday through Wednesday as a low-level trough promotes the advection of moisture from the Pacific into the region. The low-level winds, however, are expected to remain relatively weak limiting high accumulations of rain. Moisture advection from the Pacific into the coasts of Colombia and Ecuador will continue from Wednesday through Thursday, bringing more rainfall to the region. Moderate precipitation is also expected over the Amazon and portions of the Orinoquia region in Colombia from Tuesday through Wednesday due to the presence of a low-level trough and moisture advection in the region. Rivera-Torres...(WPC) $$