- 1930 Dominican Republic hurricane
Infobox Hurricane
Name=Dominican Republic Hurricane (Hurricane San Zenon)
Type=hurricane
Year=1930
Basin=Atl
Image location=1930 Dominican Republic Hurricane Weather Analysis.jpg
Surface weather analysis of the hurricane
Formed=August 25, 1930
Dissipated=September 17, 1930
1-min winds=130
Pressure=933
Da
Inflated=1
Fatalities=2,000-8,000
Areas=Dominican Republic ,Haiti ,Cuba ,Florida
Hurricane season=1930 Atlantic hurricane season The 1930 Dominican Republic Hurricane, also known as Hurricane San Zenon is the fifth deadliest
Atlantic hurricane on record. The second of two known tropical cyclones in the1930 Atlantic hurricane season , the hurricane was first observed on August 25 near theCape Verde islands. The hurricane was a small but intense Category 4 hurricane during the1930 Atlantic hurricane season , and killed as many as 8,000 people when it crossedHispaniola .Meteorological history
The cyclone was first observed on August 25 as a tropical storm to the south of the
Cape Verde islands, likely having developed from atropical wave . It gradually intensified,cite web|author=Chris Landsea|date=2005-06-28|title=The Atlantic Hurricane Database Reanalysis for 1911 to 1930|publisher=Hurricane Research Division/NOAA |accessdate=2007-04-04|url=http://www.aoml.noaa.gov/hrd/hurdat/presentations/irr-19111930.ppt|format=PPT] and with a ridge to its north and a strong westerly flow, the storm tracked nearly due westward.cite web|author=F.A. Young|date=1930-09-01|title=Weather Map of the North Atlantic Ocean|publisher=United States Weather Bureau|accessdate=2007-04-04|url=http://docs.lib.noaa.gov/rescue/mwr/058/mwr-058-09-c8.pdf] On August 31, the storm attained hurricane status while located about 385 miles (620 km) east ofGuadeloupe .cite web| author=NHC Hurricane Research Division|title=Atlantic hurricane best track|publisher=NOAA| date=2006-02-17 |accessdate=2007-04-04|url=http://www.aoml.noaa.gov/hrd/hurdat/easyhurdat_5105.html] Operationally, the hurricane was first observed on September 1, while the storm was passing through theLesser Antilles as an intensifying hurricane. Based on north winds inDominica to south winds inBarbados , the evidence of the circulation prompted an observer to report, " [there are] evidences of an approaching hurricane." Cautionary advice was immediately sent out from Barbados toSaint Lucia , and based on additional ship and island reports, the National Weather Bureau issued storm warnings for the southern coasts ofPuerto Rico andHispaniola .cite web|author=F. Eugene Hartwell|year=1930|title=The Santo Domingo Hurricane of September 1 to 5, 1930|publisher=Weather Bureau Office in San Juan, Puerto Rico|accessdate=2007-04-04|url=http://docs.lib.noaa.gov/rescue/mwr/058/mwr-058-09-0362.pdf]After passing over or near Dominica, the hurricane entered the
Caribbean Sea with winds of 100 mph, the equivalence of a Category 2 hurricane on theSaffir-Simpson hurricane scale . A small cyclone, the hurricane continued west-northwestward, passing just south ofPuerto Rico on September 2 after attaining major hurricane status. After passing by the island, its forward motion decelerated to a forward speed of about 8 mph. This allowed the hurricane to continue to intensify, despite its proximity to land. At 1800 UTC on September 3, the hurricane made landfall nearSanto Domingo ,Dominican Republic with peak winds of 150 mph and a pressure of 933 mbar. The worst of the hurricane occurred in a 20 mile diameter of its landfall location.The mountainous terrain of
Hispaniola rapidly weakened the hurricane, and by about 6 hours after moving ashore the winds decreased to tropical storm status. The cyclone spent less than 12 hours over theWindward Passage before striking southeasternCuba with winds of 60 mph on September 4. It briefly emerged into the Caribbean Sea on September 5, but moved back ashore as it continued to weaken on its west-northwest direction. On September 6, the tropical storm reached theGulf of Mexico with winds of 40 mph. It slowly recurved northeastward, and on September 9 struck nearTampa, Florida without restrengthening. After crossing the state, the storm reorganized over theGulf Stream as it accelerated northeastward, and on September 12 again attained hurricane status about 95 miles (155 km) southeast ofCape Fear ,North Carolina . On September 13, the hurricane turned eastward, and attained a secondary peak intensity of 100 mph the following day about 310 miles (500 km) north ofBermuda . The hurricane gradually weakened over the northAtlantic Ocean and on September 17 dissipated to the west of theAzores Islands.Impact
Winds of 80 to 100 mph were reported on
Dominica , with winds of hurricane force winds reported across theLesser Antilles . Initial damage reports immediately following the storm were scarce, though ship reports indicated damage was heaviest on Dominica. There, the hurricane caused severe damage to crops and buildings across the island, particularly in the capital city ofRoseau . The hurricane killed 20 people on the island.cite news|author=The Daily Gleaner|date=1930-09-04|title=Threatening Hurricane Turns from the Island|accessdate=2007-04-13|url=http://www.thehurricanearchive.com/Viewer.aspx?
] Rough seas also occurred along the coast ofSaint Kitts , and a ship recorded a pressure of 969 mbar near the island.cite news|author=Jamaica Weather Service|date=1930-09-02|title=First Caribbean Hurricane of the Season Reported|publisher=The Daily Gleaner|accessdate=2007-04-12|url=http://www.thehurricanearchive.com/Viewer.aspx?
]In southern
Puerto Rico , the winds caused minor to moderate damage to plantations. Rainfall across the island was dispersed unusually; the maximum amount on the island was over convert|6|in|mm in Cabo Rojo on the southwestern portion of the island, while the minimum amount was under convert|1|in|mm at a location in the center of the southern coastline. Rainfall reached over convert|2|in|mm inches along the northern coast, with totals varying from convert|1|in|mm to convert|4|in|mm in the mountainous interior. The precipitation was considered generally beneficial, due to previously dry conditions across the island.Upon striking the
Dominican Republic capital city ofSanto Domingo , the hurricane left a path of destruction around convert|20|mi|km wide. While just offshore the hurricane destroyed several boats through the combination of strong winds and rough seas. Wind gusts in the city were estimated from convert|150|mph|km/h to convert|200|mph|km/h; a gust of convert|180|mph|km/h was recorded by a Pan-American Airwaysanemometer before it was blown away. Similarly, another observation in the capital city recorded winds of convert|100|mph|km/h before the roof it was on was damaged. Three entire districts of the city were almost completely destroyed, and anAssociated Press report indicated there was " [scarcely] a wreck of a wall left standing". Overall, the hurricane leveled about half of the entire city.cite news|author=Associated Press|accessdate=2007-04-14|title=Santo Domingo President Heads Relief Work|date=1930-09-04|url=http://www.thehurricanearchive.com/Viewer.aspx?
] Due to its small nature, villagers 75 miles (120 km) from the landfall location had no knowledge of the storm. Heavy rainfall from the storm flooded theOzama River and increased its flow to 15 mph, which prevented boats from traversing the river. The passage of the hurricane caused severe damage estimated at $15–$50 million (1930 USD), with the storm considered a major disaster in the area. An estimate by the Red Cross estimated 2,000 perished in the city, with an additional 8,000 injured. However, the death toll may never be known, and historians estimate the hurricane left between 2,000 to 8,000 killed.cite web|author=Edward N. Rappaport, Jose Fernandez-Partagas, and Jack Beven|year=1997|title=The Deadliest Atlantic Tropical Cyclones, 1492-1996|publisher=NOAA |accessdate=2007-04-12|url=http://www.nhc.noaa.gov/pastdeadlyapp1.shtml?]Minor effects were reported away from the coast; the mountainous terrain of
Hispaniola greatly weakened the hurricane, which prevented significant amounts of further deaths or damage. Effects in the mountainous areas included downed trees and crop damage. InHaiti , the hurricane produced locally gusty winds and heavy amounts of rainfall, though exact damage details for the nation are unknown. Despite crossing the island ofCuba , no damage or deaths were reported there. Upon moving through theU.S. state ofFlorida , the storm remained severely weakened; during its passage a pressure of 1006 mbar was reported in Tampa, the lowest pressure in the state. The threat of the hurricane prompted the National Weather Bureau to issue storm warnings fromSouthport, North Carolina through theVirginia Capes . The strongest winds remained offshore, with minor damage reported along theOuter Banks . OnCape Lookout , the hurricane downed 12 small-frame buildings and damaged the city's Coast Guard headquarters. Power outages were also reported, leaving some areas on the Outer Banks isolated from communication to the outside world.cite web|author=Various|year=1930|title=Appendices to the Santo Domingo Hurricane of September 1 to 5, 1930|publisher=Weather Bureau Office|accessdate=2007-04-12|url=http://www.aoml.noaa.gov/general/lib/lib1/nhclib/mwreviews/1930.pdf]Aftermath
Relief work in the
Dominican Republic began immediately after the hurricane, with PresidentRafael Leónidas Trujillo personally organizing relief work. The president deployed the entire nation's military within 24 hours of the passage of the hurricane. By the day after the hurricane, lack of food had become a problem, and large numbers of robberies had occurred.cite news|author=Associated Press|date=1930-09-04|title=Santo Domingo Destroyed|accessdate=2007-04-13|url=http://www.thehurricanearchive.com/Viewer.aspx?
] The winds downed all communications inside of the city, leaving damage details unknown until communications were partially restored a day after its landfall. The city plant of the newspaperLa Opinión was destroyed, with three staff members killed; the remaining workers transmitted a damage story to offices inNew York City , and included a plea for disaster assistance. TheRed Cross office inWashington, D.C. sent $15,000 (1930 USD) in aid on the day after the hurricane struck.ee also
*
List of Atlantic hurricanes
*List of deadliest Atlantic hurricanes External links
* [http://www.aoml.noaa.gov/general/lib/lib1/nhclib/mwreviews/1930.pdf Monthly Weather Review]
References
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