000 AXNT20 KNHC 162321 TWDAT Tropical Weather Discussion NWS National Hurricane Center Miami FL 0005 UTC Sun Mar 17 2024 Tropical Weather Discussion for North America, Central America Gulf of Mexico, Caribbean Sea, northern sections of South America, and Atlantic Ocean to the African coast from the Equator to 31N. The following information is based on satellite imagery, weather observations, radar and meteorological analysis. Based on 1800 UTC surface analysis and satellite imagery through 2300 UTC. ...MONSOON TROUGH/ITCZ... The monsoon trough enters the Atlantic near 07N13W to 04N21W. The ITCZ then continues from 04N21W to 00N47W. Scattered moderate convection is S of 02N between 15W-42W. ...GULF OF MEXICO... A stationary front extends across the northern gulf from 30N85W to 29N96W. High pressure is centered over the SE gulf waters near 27N83W. Upper level diffluent flow is supporting scattered showers S of the front mainly S of 26N. Slight to moderate seas and light to moderate winds prevail across the basin. For the forecast, high pressure will move eastward across the Atlantic through Mon, and maintain a lingering ridge westward over the western Atlantic and into the central Gulf through Sun. A weakening front will drift N and dissipate tonight. A new cold front will move into the NW Gulf Sun evening and gradually shift S of the basin by Tue evening. Increasing wind and seas are expected behind the front Sun night through Tue. Fresh to locally strong winds will pulse near and to the NW of the Yucatan Peninsula each evening and into the early morning hours. ...CARIBBEAN SEA... The pressure gradient between subtropical ridging N of the area and low pressure over NW Colombia continue to support fresh to near-gale force winds in the south-central Caribbean and moderate to fresh speeds elsewhere. Seas are moderate in the 5-7 ft range over most of the region, except for rough seas to 10 ft off the coast of Colombia. Otherwise, aside from the Gulf of Honduras, gentle to moderate E to SE winds and slight seas are ongoing over the NW basin. For the forecast, high pressure located over the central subtropical Atlantic will slide eastward and into the eastern Atlantic through late Sun then remain stationary. The lingering ridge to the W will support fresh to strong winds across the south-central and portions of the southeast Caribbean through Tue. Afterward, winds will diminish to moderate to fresh speeds and prevail through the remainder forecast period, except for strong winds developing at night off Colombia. Otherwise, fresh trade winds will pulse to strong speeds across the Gulf of Honduras, the Windward Passage, and S of Hispaniola through Mon. A cold front will sink into the NW Caribbean Tue evening then stall from eastern Cuba to the NE Yucatan Wed and dissipate Wed night. ...ATLANTIC OCEAN... The subtropical Atlantic is under the influence of a broad surface ridge anchored by a 1020 mb high near 28N48W. The ridge is crossed by a weakening cold front over the E subtropical Atlantic, which extends from 31N23W to 21N38W. The ridge is providing mainly gentle to moderate NE to E winds S of 23N. Otherwise, the gradient between the ridge and lower pressure associated with a frontal boundary N of the area is supporting fresh to locally strong SW winds N of 29W along with moderate seas. For the forecast W of 55W, high pressure located over the central subtropical Atlantic will slide eastward and into the eastern Atlantic through Sun then becoming nearly stationary through Tue. A broad associated ridge will persist westward across the area through Mon. A cold front will enter the offshore waters of NE Florida Mon, reach from near Bermuda through the central Bahamas by Tue afternoon, then weaken as it reaches from the central Atlantic waters to northern Hispaniola by Thu morning. Fresh to strong S to SW winds are expected N of 27N and ahead of the front Sun night through Tue night, while fresh to near gale-force NW to N winds will follow the front Mon night through Tue evening. High pressure will settle across the area Wed through Thu. $$ ERA