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{{short description|Category 4 Atlantic hurricane in 1930}}
{{Infobox Hurricane
{{Infobox weather event
| Name=Dominican Republic Hurricane (Hurricane San Zenon)
| name = Hurricane Two <br>Hurricane San Zenón
| Type=hurricane
| image = 1930 Dominican Republic Hurricane Weather Analysis.JPG
| Year=1930
| caption = [[Surface weather analysis]] of the hurricane just before landfall in the Dominican Republic on September 3
| Basin=Atl
| formed = {{start-date|August 29, 1930}}
| Image location=1930 Dominican Republic Hurricane Weather Analysis.JPG
| dissipated = {{end-date|September 17, 1930}}
| Image name=[[Surface weather analysis]] of the hurricane
}}{{Infobox weather event/NWS
| Formed= {{start-date|August 29, 1930}}
| winds = 135
| Dissipated= {{end-date|September 17, 1930}}
| pressure = 933
| 1-min winds=135
}}{{Infobox weather event/Effects
| Pressure=933
| year = 1930
| Damages=50
| fatalities = 2,000–8,000
| Inflated=1
| damage = 50000000
| Fatalities=2,000–8,000
| Areas=[[Dominican Republic]], [[Haiti]], [[Cuba]], [[Florida]], [[North Carolina]]
| areas = [[Dominican Republic]], [[Haiti]], [[Cuba]], [[Florida]], [[North Carolina]]
| refs =
| Hurricane season=[[1930 Atlantic hurricane season]]
}}{{Infobox weather event/Footer
| season = [[1930 Atlantic hurricane season]]
}}
}}


The '''1930 Dominican Republic Hurricane''', also known as '''Hurricane San Zenon''', is the fifth [[List of deadliest Atlantic hurricanes|deadliest]] [[North Atlantic tropical cyclone|Atlantic hurricane]] on record. The second of three known tropical cyclones in the [[1930 Atlantic hurricane season]], the hurricane was first observed on August 29 to the east of the [[Lesser Antilles]]. The cyclone was a small but intense [[Saffir-Simpson Hurricane Scale|Category 4 hurricane]], killing as many as 8,000&nbsp;people when it crossed the [[Dominican Republic]].
The '''1930 Dominican Republic hurricane''', also known as '''Hurricane San Zenón''', was a small but intense and deadly [[tropical cyclone]] that severely impacted areas of the [[Greater Antilles]], particularly the [[Dominican Republic]], where an estimated 2,000 to&nbsp;8,000 people died. The second of three known tropical cyclones in the [[1930 Atlantic hurricane season]], the system was first observed on August&nbsp;29 to the east of the [[Lesser Antilles]], and made [[landfall]] in the Dominican Republic at Category&nbsp;4 strength on the modern [[Saffir-Simpson Scale]]. Later, it also struck [[Cuba]] and the [[U.S. state]]s of [[Florida]] and [[North Carolina]], with less severe effects.


==Meteorological history==
==Meteorological history==
{{storm path|1930 Dominican Republic hurricane track.png}}
{{storm path|1930 Dominican Republic hurricane track.png}}
The system is estimated to have formed on August&nbsp;29 about halfway between the Lesser Antilles and the [[Cape Verde]] islands, although there were indications it may have formed closer to the African coast a few days earlier. Moving westward, the system slowly intensified, with its track and path based mainly on continuity. It is estimated to have become a hurricane on August&nbsp;31 about 385&nbsp;miles (620&nbsp;km) east of [[Guadeloupe]].<ref name="meta">{{cite web|author =Chris Landsea|year=2010|title=Documentation of Atlantic Tropical Cyclones Changes in HURDAT|publisher=Hurricane Research Division|accessdate=2011-07-31|url=http://www.aoml.noaa.gov/hrd/hurdat/metadata_1926-30.html#1930_02| archiveurl= https://web.archive.org/web/20110628232555/http://www.aoml.noaa.gov/hrd/hurdat/metadata_1926-30.html| archivedate= 28 June 2011 <!--DASHBot-->| deadurl= no|display-authors=etal}}</ref> Operationally, the hurricane was first observed on September 1, while the storm was passing through the [[Lesser Antilles]] as an intensifying hurricane. Based on north winds in [[Dominica]] and south winds in [[Barbados]], 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 to [[Saint Lucia]], and based on additional ship and island reports, the [[NOAA|National Weather Bureau]] issued storm warnings for the southern coasts of [[Puerto Rico]] and [[Hispaniola]].<ref name="mwr">{{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}}</ref>
The system is estimated to have formed on August&nbsp;29 about halfway between the Lesser Antilles and the [[Cape Verde]] islands, although there were indications it may have formed closer to the African coast a few days earlier. Moving westward, the system slowly intensified, with its track and path based mainly on continuity. It is estimated to have become a hurricane on August&nbsp;31 about {{convert|385|mi|km}} east of [[Guadeloupe]].<ref name="meta">{{cite web|author =Chris Landsea|year=2010|title=Documentation of Atlantic Tropical Cyclones Changes in HURDAT|publisher=Hurricane Research Division|accessdate=2011-07-31|url=http://www.aoml.noaa.gov/hrd/hurdat/metadata_1926-30.html#1930_02| archiveurl= https://web.archive.org/web/20110628232555/http://www.aoml.noaa.gov/hrd/hurdat/metadata_1926-30.html| archivedate= 28 June 2011 | url-status= live|display-authors=etal}}</ref> Operationally, the hurricane was first observed on September&nbsp;1, while the storm was passing through the [[Lesser Antilles]] as an intensifying hurricane. Based on north winds in [[Dominica]] and south winds in [[Barbados]], 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 to [[Saint Lucia]], and based on additional ship and island reports, the [[NOAA|National Weather Bureau]] issued storm warnings for the southern coasts of [[Puerto Rico]] and [[Hispaniola]].<ref name="mwr">{{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}}</ref>


After passing over or near Dominica, the hurricane entered the [[Caribbean Sea]] with winds of {{convert|100|mi/h|km/h|abbr=on}}, the equivalence of a Category&nbsp;2 hurricane on the [[Saffir-Simpson hurricane scale]].<ref name="mwr"/> On September&nbsp;2, the hurricane passed about 60&nbsp;mi (95&nbsp;km) southwest of [[Puerto Rico]] as it intensified into a major hurricane. Due to the storm's small size, winds on the island were below hurricane force. Continuing slowly west-northwestward, the hurricane continued to intensify as it approached the [[Dominican Republic]]. Captain Thomas Evans of the SS ''Coamo'' of the Porto Rico Line, its crew and passengers all survived being buffeted by the storm for seven hours and passing through the eye. He reported a barometric pressure of {{convert|933|mbar|inHg|abbr=on}} and a detailed description of its near capsizing off the coast of the Dominican Republic to ''[[The New York Times]]'' when they arrived in San Juan on September 4. The ''New York Times'' published the story on September 5 as "Steamer Outrides Storm's Full Fury: Caught in Vortex of Hurricane, Coamo Tilts Periously as Gail Strips Decks".<ref>https://www.nytimes.com/1930/09/05/archives/steamer-outrides-storms-full-fury-caught-in-vortex-of-hurricane.html</ref> A steamship just offshore recorded winds of {{convert|150|mph|km/h|abbr=on}}, and also provided data to estimate the [[radius of maximum wind]]s at 8&nbsp;mi (13&nbsp;km). At 1800&nbsp;[[Coordinated Universal Time|UTC]] on September&nbsp;3, it made [[landfall (meteorology)|landfall]] near [[Santo Domingo]], Dominican Republic with a minimum central pressure of {{convert|933|mbar|inHg|abbr=on}}. As it was still intensifying up until landfall, the peak winds were estimated at {{convert|155|mi/h|km/h|abbr=on}}, although it is possible it attained [[List of Category 5 Atlantic hurricanes|Category 5]] status.<ref name="meta"/> The worst of the hurricane occurred in a {{convert|2|mi|km|adj=on}} diameter of its landfall location.<ref name="mwr"/>
After passing over or near Dominica, the hurricane entered the [[Caribbean Sea]] with winds of {{convert|100|mi/h|km/h|abbr=on}}, the equivalence of a Category&nbsp;2 hurricane on the [[Saffir-Simpson hurricane scale]].<ref name="mwr"/> On September&nbsp;2, the hurricane passed about {{convert|60|mi|km|abbr=on}} southwest of [[Puerto Rico]] as it intensified into a major hurricane. Due to the storm's small size, winds on the island were below hurricane force. Continuing slowly west-northwestward, the hurricane continued to intensify as it approached the [[Dominican Republic]]. Captain Thomas Evans of the SS ''Coamo'' of the [[Porto Rico Line]], its crew and passengers all survived being buffeted by the storm for seven hours and passing through the eye. He reported a barometric pressure of {{convert|933|mbar|inHg|abbr=on}} and a detailed description of its near capsizing off the coast of the Dominican Republic to ''[[The New York Times]]'' when they arrived in San Juan on September&nbsp;4. The ''New York Times'' published the story on September&nbsp;5 as "Steamer Outrides Storm's Full Fury: Caught in Vortex of Hurricane, Coamo Tilts Periously as Gail Strips Decks".<ref>{{Cite news|url=https://www.nytimes.com/1930/09/05/archives/steamer-outrides-storms-full-fury-caught-in-vortex-of-hurricane.html|title = STEAMER OUTRIDES STOrm's FULL FURY; Caught in Vortex of Hurricane, Coamo Tilts Perilously as Gale Strips Decks|newspaper = The New York Times|date = 5 September 1930}}</ref> A steamship just offshore recorded winds of {{convert|150|mph|km/h|abbr=on}}, and also provided data to estimate the [[radius of maximum wind]]s at {{convert|8|mi|km|abbr=on}}. At 1800&nbsp;[[Coordinated Universal Time|UTC]] on September&nbsp;3, it made [[landfall (meteorology)|landfall]] near [[Santo Domingo]], Dominican Republic with a minimum central pressure of {{convert|933|mbar|inHg|abbr=on}}. As it was still intensifying up until landfall, the peak winds were estimated at {{convert|155|mi/h|km/h|abbr=on}}, although it is possible it attained [[List of Category 5 Atlantic hurricanes|Category 5]] status.<ref name="meta"/> The worst of the hurricane occurred in a {{convert|2|mi|km|adj=on}} diameter of its landfall location.<ref name="mwr"/>


The mountainous terrain of [[Hispaniola]] rapidly weakened the hurricane, and by about 12&nbsp;hours after moving ashore the winds decreased to tropical storm status. It quickly emerged into the [[Windward Passage]] and moved westward to the south of the Cuban coastline. On September&nbsp;6 the storm crossed western Cuba before recurving northeastward into the [[Gulf of Mexico]] with winds of {{convert|40|mph|km/h|abbr=on}}. It strengthened slightly, moving ashore near [[Tampa, Florida]], with 45&nbsp;mph (75&nbsp;km/h) winds. While crossing the state, it weakened to tropical depression status, although it re-intensified after moving into the western Atlantic Ocean. By September&nbsp;12, it again attained hurricane status to the southeast of the Carolinas. After brushing the [[Outer Banks]] of North Carolina with winds of 70&nbsp;mph (110&nbsp;km/h), the hurricane turned eastward and reached a secondary peak intensity of 100&nbsp;mph (160&nbsp;km/h) to the north of [[Bermuda]]. It gradually weakened, deteriorating to tropical storm status on September&nbsp;16 and dissipating the next day to the west of the [[Azores]]. The remnants merged with a system that later affected the Azores and Ireland.<ref name="meta"/>
The mountainous terrain of [[Hispaniola]] rapidly weakened the hurricane, and by about 12&nbsp;hours after moving ashore the winds decreased to tropical storm status. It quickly emerged into the [[Windward Passage]] and moved westward to the south of the Cuban coastline. On September&nbsp;6 the storm crossed western Cuba before recurving northeastward into the [[Gulf of Mexico]] with winds of {{convert|40|mph|km/h|abbr=on}}. It strengthened slightly, moving ashore near [[Tampa, Florida]], with {{convert|45|mph|km/h|abbr=on}} winds. While crossing the state, it weakened to tropical depression status, although it re-intensified after moving into the western Atlantic Ocean. By September&nbsp;12, it again attained hurricane status to the southeast of the Carolinas. After brushing the [[Outer Banks]] of North Carolina with winds of {{convert|70|mph|km/h|abbr=on}}, the hurricane turned eastward and reached a secondary peak intensity of {{convert|100|mph|km/h|abbr=on}} to the north of [[Bermuda]]. It gradually weakened, deteriorating to tropical storm status on September&nbsp;16 and dissipating the next day to the west of the [[Azores]]. The remnants merged with a system that later affected the Azores and Ireland.<ref name="meta"/>


==Impact==
==Impact==
Winds of {{convert|80|to|100|mi/h|km/h|abbr=on}} were reported on [[Dominica]], with winds of hurricane-force winds reported across the [[Lesser Antilles]].<ref name="mwr"/> The hurricane wrecked crops across the island and destroyed every ship at the harbor, killing two&nbsp;people.<ref>{{cite news|author=Staff Writer|agency=Associated Press|title=Two Dead in Dominica|newspaper=The Milwaukee Journal|date=1930-09-06|accessdate=2011-07-31|url=https://news.google.com/newspapers?id=XaBQAAAAIBAJ&sjid=9iEEAAAAIBAJ&pg=2385,4607849&dq=dominica+crops&hl=en}}{{Dead link|date=May 2022 |bot=InternetArchiveBot |fix-attempted=yes }}</ref> Rough seas also occurred along the coast of [[Saint Kitts]], and a ship recorded a pressure of {{convert|969|mbar|inHg|abbr=on}} near the island.<ref name="jms92">{{cite news |title=First Caribbean Hurricane of the Season Reported |work=The Daily Gleaner |agency=The Daily Gleaner |issue=175 |volume=96 |date=1930-09-02 |location=Kingston, Jamaica |page=1|via=NewspaperArchive.com}}</ref>
{{Deadliest Atlantic hurricanes|align=right}}
Winds of {{convert|80|to|100|mi/h|km/h|abbr=on}} were reported on [[Dominica]], with winds of hurricane-force winds reported across the [[Lesser Antilles]].<ref name="mwr"/> The hurricane wrecked crops across the island and destroyed every ship at the harbor, killing two&nbsp;people.<ref>{{cite news|author =Staff Writer|agency=Associated Press|title=Two Dead in Dominica|newspaper=The Milwaukee Journal|date=1930-09-06|accessdate=2011-07-31|url=https://news.google.com/newspapers?id=XaBQAAAAIBAJ&sjid=9iEEAAAAIBAJ&pg=2385,4607849&dq=dominica+crops&hl=en}}</ref> Rough seas also occurred along the coast of [[Saint Kitts]], and a ship recorded a pressure of {{convert|969|mbar|inHg|abbr=on}} near the island.<ref name="jms92">{{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?img=19751730&firstvisit=true&src=search&currentResult=6&currentPage=0}}{{Dead link|date=February 2019 |bot=InternetArchiveBot |fix-attempted=yes }}</ref>


In southern [[Puerto Rico]], the winds reached less than hurricane force,<ref name="meta"/> which 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|abbr=on}} in [[Cabo Rojo, Puerto Rico|Cabo Rojo]] on the southwestern portion of the island, while the minimum amount was under {{convert|1|in|mm|abbr=on}} at a location in the center of the southern coastline. Rainfall reached over {{convert|2|in|mm|abbr=on}} along the northern coast, with totals varying from {{convert|1|to|4|in|mm|abbr=on}} in the mountainous interior. The precipitation was considered generally beneficial, due to previously dry conditions across the island.<ref name="mwr"/>
In southern [[Puerto Rico]], the winds reached less than hurricane force,<ref name="meta"/> which 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|abbr=on}} in [[Cabo Rojo, Puerto Rico|Cabo Rojo]] on the southwestern portion of the island, while the minimum amount was under {{convert|1|in|mm|abbr=on}} at a location in the center of the southern coastline. Rainfall reached over {{convert|2|in|mm|abbr=on}} along the northern coast, with totals varying from {{convert|1|to|4|in|mm|abbr=on}} in the mountainous interior. The precipitation was considered generally beneficial, due to previously dry conditions across the island.<ref name="mwr"/>


On September 3 the storm was a Category 4 when it struck the [[Dominican Republic]] capital city of [[Santo Domingo]],{{Atlantic hurricane best track}} leaving a path of destruction around {{convert|20|mi|km|abbr=on}} wide. Wind gusts in the city were estimated from {{convert|150|to|200|mph|km/h}};<ref name="ldb-truj">{{cite book|last=De Besault|first=Lawrence |title=President Trujillo - His Work and the Dominican Republic|year=2007|publisher=READ BOOKS|isbn=1-4067-4641-X|pages=265–6}}</ref> a gust of {{convert|180|mph|km/h|abbr=on}} was recorded by a [[Pan American World Airways|Pan-American Airways]] [[anemometer]] before it was blown away. Similarly, another observation in the capital city recorded winds of {{convert|100|mph|km/h|abbr=on}} before the roof it was on was damaged.<ref name="mwr"/> It was estimated as among the strongest hurricanes on record to strike the country.<ref name="meta"/> Three entire districts of the city were almost completely destroyed, and an [[Associated Press]] report indicated "there was [scarcely] a wreck of a wall left standing".<ref name="ap904"/> Overall, the hurricane leveled about half of the entire city.<ref name="ap94a">{{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?img=31953439&firstvisit=true&src=search&currentResult=4&currentPage=0}}{{Dead link|date=February 2019 |bot=InternetArchiveBot |fix-attempted=yes }}</ref> Due to its small nature, villagers 75&nbsp;mi (120&nbsp;km) from the landfall location had no knowledge of the storm. Heavy rainfall from the storm flooded the [[Ozama River]] and increased its flow to {{convert|15|mi/h|km/h|abbr=on}}, which prevented boats from traversing the river.<ref name="1930apps"/> The passage of the hurricane caused severe damage estimated at $15–$50&nbsp;million, with the storm considered a major disaster in the area. The [[International Red Cross and Red Crescent Movement|Red Cross]] estimated 2,000&nbsp;people died in the city, with an additional 8,000 injured.<ref name="mwr"/> However, the death toll may never be known, and historians estimate the hurricane left between 2,000 and 8,000 killed.<ref name="deadliest">{{cite web|author1=Edward N. Rappaport |author2=Jose Fernandez-Partagas |author3=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?| archiveurl= https://web.archive.org/web/20070526172740/http://www.nhc.noaa.gov/pastdeadlyapp1.shtml| archivedate= 26 May 2007 <!--DASHBot-->| deadurl= no}}</ref>
On September&nbsp;3 the storm was a Category 4 when it struck the [[Dominican Republic]] capital city of [[Santo Domingo]],{{Atlantic hurricane best track}} leaving a path of destruction around {{convert|20|mi|km|abbr=on}} wide. Wind gusts in the city were estimated from {{convert|150|to|200|mph|km/h}};<ref name="ldb-truj">{{cite book|last=De Besault|first=Lawrence |title=President Trujillo - His Work and the Dominican Republic|year=2007|publisher=READ BOOKS|isbn=978-1-4067-4641-9|pages=265–6}}</ref> a gust of {{convert|180|mph|km/h|abbr=on}} was recorded by a [[Pan American World Airways|Pan-American Airways]] [[anemometer]] before it was blown away. Similarly, another observation in the capital city recorded winds of {{convert|100|mph|km/h|abbr=on}} before the roof it was on was damaged.<ref name="mwr"/> It was estimated as among the strongest hurricanes on record to strike the country.<ref name="meta"/> Three entire districts of the city were almost completely destroyed, and an [[Associated Press]] report indicated "there was [scarcely] a wreck of a wall left standing".<ref name="ap904"/> Overall, the hurricane leveled about half of the entire city.<ref name="ap94a">{{cite news |title=Storm Dead at 300 |url=https://www.newspapers.com/clip/33500344/ |accessdate=2019-07-03 |work=Marshfield News-Herald |agency=Associated Press |issue=145 |volume=10 |date=1930-09-04 |location=Marshfield, Wisconsin|via=Newspapers.com}}</ref> Due to its small nature, villagers {{convert|75|mi|km|abbr=on}} from the landfall location had no knowledge of the storm. Heavy rainfall from the storm flooded the [[Ozama River]] and increased its flow to {{convert|15|mi/h|km/h|abbr=on}}, which prevented boats from traversing the river.<ref name="1930apps"/> The passage of the hurricane caused severe damage estimated at $15–$50&nbsp;million, with the storm considered a major disaster in the area. The [[International Red Cross and Red Crescent Movement|Red Cross]] estimated 2,000&nbsp;people died in the city, with an additional 8,000 injured.<ref name="mwr"/> Historians estimate the hurricane left between 2,000 and 8,000 killed.<ref name="deadliest">{{cite web|author1=Edward N. Rappaport |author2=Jose Fernandez-Partagas |author3=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?| archiveurl= https://web.archive.org/web/20070526172740/http://www.nhc.noaa.gov/pastdeadlyapp1.shtml| archivedate= 26 May 2007 | url-status= live}}</ref>


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.<ref name="mwr"/> Effects in the mountainous areas included downed trees and crop damage.<ref name="1930apps"/> In [[Haiti]], the hurricane produced locally gusty winds and heavy amounts of rainfall, though exact damage details for the nation are unknown.<ref name="ap904"/> Despite crossing the island of [[Cuba]], no damage or deaths were reported there. Upon moving through the U.S. state of [[Florida]], the storm remained severely weakened; during its passage a pressure of {{convert|1006|mbar|inHg|abbr=on}} was reported in [[Tampa, Florida|Tampa]], the lowest pressure in the state. The threat of the hurricane prompted the [[NOAA|National Weather Bureau]] to issue [[tropical cyclone warnings and watches|storm warnings]] from [[Southport, North Carolina]] through the [[Virginia Capes]]. The strongest winds remained offshore, with minor damage reported along the [[Outer Banks]]. On [[Cape Lookout (North Carolina)|Cape Lookout]], the hurricane downed 12 small-frame buildings and damaged the city's [[United States Coast Guard|Coast Guard]] headquarters. Power outages were also reported, leaving some areas on the Outer Banks isolated from communication to the outside world.<ref name="1930apps">{{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}}</ref>
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.<ref name="mwr"/> Effects in the mountainous areas included downed trees and crop damage.<ref name="1930apps"/> In [[Haiti]], the hurricane produced locally gusty winds and heavy amounts of rainfall, though exact damage details for the nation are unknown.<ref name="ap904"/> Despite crossing the island of [[Cuba]], no damage or deaths were reported there. Upon moving through the U.S. state of [[Florida]], the storm remained severely weakened; during its passage a pressure of {{convert|1006|mbar|inHg|abbr=on}} was reported in [[Tampa, Florida|Tampa]], the lowest pressure in the state. The threat of the hurricane prompted the [[NOAA|National Weather Bureau]] to issue [[tropical cyclone warnings and watches|storm warnings]] from [[Southport, North Carolina]] through the [[Virginia Capes]]. The strongest winds remained offshore, with minor damage reported along the [[Outer Banks]]. On [[Cape Lookout (North Carolina)|Cape Lookout]], the hurricane downed 12 small-frame buildings and damaged the city's [[United States Coast Guard|Coast Guard]] headquarters. Power outages were also reported, leaving some areas on the Outer Banks isolated from communication to the outside world.<ref name="1930apps">{{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}}</ref>
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==Aftermath==
==Aftermath==
[[Image:Wea02216.jpg|right|thumb|Destruction after the 1930 Dominican Republic Hurricane]]
[[Image:Wea02216.jpg|right|thumb|Destruction after the 1930 Dominican Republic Hurricane]]
Relief work in the [[Dominican Republic]] began immediately after the hurricane, personally organized by the then-new [[List of Presidents of the Dominican Republic|President]] [[Rafael Leónidas Trujillo]]. The president deployed the entire nation's military within 24&nbsp;hours of the passage of the hurricane. By the day after its passage, lack of food had become a problem, and large numbers of robberies had occurred.<ref name="ap904">{{cite news|author=Associated Press|date=1930-09-04|title=Santo Domingo Destroyed|accessdate=2007-04-13|url=http://www.thehurricanearchive.com/Viewer.aspx?img=5080006&firstvisit=true&src=search&currentResult=1&currentPage=0}}{{Dead link|date=February 2019 |bot=InternetArchiveBot |fix-attempted=yes }}</ref> The winds downed all communications inside of the city,<ref name="1930apps"/> leaving damage details unknown until communications were partially restored a day after its landfall. The city plant of the newspaper [[La Opinión]] was destroyed, with three staff members killed; the remaining workers transmitted a damage story to offices in New York City, and included a plea for disaster assistance. The [[Red Cross]] office in [[Washington, D.C.]], sent [[United States dollar|$]]15,000 (in 1930&nbsp;dollars, roughly $211,000 in 2015 dollars) in aid a day after the hurricane struck.<ref name="ap904"/>
Relief work in the [[Dominican Republic]] began immediately after the hurricane, personally organized by the then-new [[List of Presidents of the Dominican Republic|President]] [[Rafael Leónidas Trujillo]]. The president deployed the entire nation's military within 24&nbsp;hours of the passage of the hurricane. By the day after its passage, lack of food had become a problem, and large numbers of robberies had occurred.<ref name="ap904">{{cite news |title=Santo Doming Leveled by Hurricane; Believe 900 Dead, Injured in Hurricane |url=https://www.newspapers.com/clip/33500967/ |accessdate=2019-07-03 |work=Ironwood Daily Globe |agency=Associated Press |issue=245 |volume=11 |date=1930-09-04 |location=Ironwood, Michigan |page=1|via=Newspapers.com}}</ref> The winds downed all communications inside of the city,<ref name="1930apps"/> leaving damage details unknown until communications were partially restored a day after its landfall. The city plant of the newspaper [[La Opinión]] was destroyed, with three staff members killed; the remaining workers transmitted a damage story to offices in New York City, and included a plea for disaster assistance. The [[Red Cross]] office in [[Washington, D.C.]], sent {{inflation|US|15,000|1930|fmt=eq|orig=yes|cursign=US$|r=-4}} in aid a day after the hurricane struck.<ref name="ap904"/>


==See also==
==See also==
{{Portal|Tropical cyclones}}
{{Portal|Tropical cyclones}}
* [[Hurricane David]] (1979) – hit the Dominican Republic at Category&nbsp;5 intensity
* [[List of Atlantic hurricanes]]
* [[Effects of Hurricane Georges in the Dominican Republic]] (1988)
* [[List of deadliest Atlantic hurricanes]]
* [[Hurricanes in Hispaniola]]
* [[List of Category 4 Atlantic hurricanes]]
* [[List of Cuba hurricanes]]
* [[List of Florida hurricanes (1900–1949)]]


==References==
==References==
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==External links==
==External links==
* [http://www.aoml.noaa.gov/general/lib/lib1/nhclib/mwreviews/1930.pdf Monthly Weather Review]
* [http://www.aoml.noaa.gov/general/lib/lib1/nhclib/mwreviews/1930.pdf Monthly Weather Review]

{{Category 4 Atlantic hurricanes}}


{{DEFAULTSORT:1930 Dominican Republic Hurricane}}
{{DEFAULTSORT:1930 Dominican Republic Hurricane}}
[[Category:1930–1939 Atlantic hurricane seasons|Dominician Republic]]
[[Category:1930s Atlantic hurricane seasons|Dominician Republic]]
[[Category:Cape Verde hurricanes|1930 Dominican Republic]]
[[Category:Cape Verde hurricanes|1930 Dominican Republic]]
[[Category:Category 4 Atlantic hurricanes|1930]]
[[Category:Category 4 Atlantic hurricanes|1930]]
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[[Category:Hurricanes in Cuba|1930]]
[[Category:Hurricanes in Cuba|1930]]
[[Category:Hurricanes in Florida|1930]]
[[Category:Hurricanes in Florida|1930]]
[[Category:1930 natural disasters in the United States|Dominican Republic Hurricane, 1930]]
[[Category:1930 in the Dominican Republic|Dominican Republic Hurricane, 1930]]
[[Category:1930 in the Dominican Republic|Dominican Republic Hurricane, 1930]]
[[Category:1930 in the Caribbean|Dominican Republic Hurricane, 1930]]
[[Category:1930 in the Caribbean|Dominican Republic Hurricane, 1930]]

Latest revision as of 14:31, 11 December 2023

Hurricane Two
Hurricane San Zenón
Surface weather analysis of the hurricane just before landfall in the Dominican Republic on September 3
Meteorological history
FormedAugust 29, 1930 (1930-08-29)
DissipatedSeptember 17, 1930 (1930-09-18)
Category 4 major hurricane
1-minute sustained (SSHWS/NWS)
Highest winds155 mph (250 km/h)
Lowest pressure933 mbar (hPa); 27.55 inHg
Overall effects
Fatalities2,000–8,000
Damage$50 million (1930 USD)
Areas affectedDominican Republic, Haiti, Cuba, Florida, North Carolina
IBTrACSEdit this at Wikidata

Part of the 1930 Atlantic hurricane season

The 1930 Dominican Republic hurricane, also known as Hurricane San Zenón, was a small but intense and deadly tropical cyclone that severely impacted areas of the Greater Antilles, particularly the Dominican Republic, where an estimated 2,000 to 8,000 people died. The second of three known tropical cyclones in the 1930 Atlantic hurricane season, the system was first observed on August 29 to the east of the Lesser Antilles, and made landfall in the Dominican Republic at Category 4 strength on the modern Saffir-Simpson Scale. Later, it also struck Cuba and the U.S. states of Florida and North Carolina, with less severe effects.

Meteorological history

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Map plotting the storm's track and intensity, according to the Saffir–Simpson scale
Map key
  Tropical depression (≤38 mph, ≤62 km/h)
  Tropical storm (39–73 mph, 63–118 km/h)
  Category 1 (74–95 mph, 119–153 km/h)
  Category 2 (96–110 mph, 154–177 km/h)
  Category 3 (111–129 mph, 178–208 km/h)
  Category 4 (130–156 mph, 209–251 km/h)
  Category 5 (≥157 mph, ≥252 km/h)
  Unknown
Storm type
triangle Extratropical cyclone, remnant low, tropical disturbance, or monsoon depression

The system is estimated to have formed on August 29 about halfway between the Lesser Antilles and the Cape Verde islands, although there were indications it may have formed closer to the African coast a few days earlier. Moving westward, the system slowly intensified, with its track and path based mainly on continuity. It is estimated to have become a hurricane on August 31 about 385 miles (620 km) east of Guadeloupe.[1] Operationally, the hurricane was first observed on September 1, while the storm was passing through the Lesser Antilles as an intensifying hurricane. Based on north winds in Dominica and south winds in Barbados, 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 to Saint Lucia, and based on additional ship and island reports, the National Weather Bureau issued storm warnings for the southern coasts of Puerto Rico and Hispaniola.[2]

After passing over or near Dominica, the hurricane entered the Caribbean Sea with winds of 100 mph (160 km/h), the equivalence of a Category 2 hurricane on the Saffir-Simpson hurricane scale.[2] On September 2, the hurricane passed about 60 mi (97 km) southwest of Puerto Rico as it intensified into a major hurricane. Due to the storm's small size, winds on the island were below hurricane force. Continuing slowly west-northwestward, the hurricane continued to intensify as it approached the Dominican Republic. Captain Thomas Evans of the SS Coamo of the Porto Rico Line, its crew and passengers all survived being buffeted by the storm for seven hours and passing through the eye. He reported a barometric pressure of 933 mbar (27.6 inHg) and a detailed description of its near capsizing off the coast of the Dominican Republic to The New York Times when they arrived in San Juan on September 4. The New York Times published the story on September 5 as "Steamer Outrides Storm's Full Fury: Caught in Vortex of Hurricane, Coamo Tilts Periously as Gail Strips Decks".[3] A steamship just offshore recorded winds of 150 mph (240 km/h), and also provided data to estimate the radius of maximum winds at 8 mi (13 km). At 1800 UTC on September 3, it made landfall near Santo Domingo, Dominican Republic with a minimum central pressure of 933 mbar (27.6 inHg). As it was still intensifying up until landfall, the peak winds were estimated at 155 mph (249 km/h), although it is possible it attained Category 5 status.[1] The worst of the hurricane occurred in a 2-mile (3.2 km) diameter of its landfall location.[2]

The mountainous terrain of Hispaniola rapidly weakened the hurricane, and by about 12 hours after moving ashore the winds decreased to tropical storm status. It quickly emerged into the Windward Passage and moved westward to the south of the Cuban coastline. On September 6 the storm crossed western Cuba before recurving northeastward into the Gulf of Mexico with winds of 40 mph (64 km/h). It strengthened slightly, moving ashore near Tampa, Florida, with 45 mph (72 km/h) winds. While crossing the state, it weakened to tropical depression status, although it re-intensified after moving into the western Atlantic Ocean. By September 12, it again attained hurricane status to the southeast of the Carolinas. After brushing the Outer Banks of North Carolina with winds of 70 mph (110 km/h), the hurricane turned eastward and reached a secondary peak intensity of 100 mph (160 km/h) to the north of Bermuda. It gradually weakened, deteriorating to tropical storm status on September 16 and dissipating the next day to the west of the Azores. The remnants merged with a system that later affected the Azores and Ireland.[1]

Impact

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Winds of 80 to 100 mph (130 to 160 km/h) were reported on Dominica, with winds of hurricane-force winds reported across the Lesser Antilles.[2] The hurricane wrecked crops across the island and destroyed every ship at the harbor, killing two people.[4] Rough seas also occurred along the coast of Saint Kitts, and a ship recorded a pressure of 969 mbar (28.6 inHg) near the island.[5]

In southern Puerto Rico, the winds reached less than hurricane force,[1] which caused minor to moderate damage to plantations. Rainfall across the island was dispersed unusually; the maximum amount on the island was over 6 in (150 mm) in Cabo Rojo on the southwestern portion of the island, while the minimum amount was under 1 in (25 mm) at a location in the center of the southern coastline. Rainfall reached over 2 in (51 mm) along the northern coast, with totals varying from 1 to 4 in (25 to 102 mm) in the mountainous interior. The precipitation was considered generally beneficial, due to previously dry conditions across the island.[2]

On September 3 the storm was a Category 4 when it struck the Dominican Republic capital city of Santo Domingo,[6] leaving a path of destruction around 20 mi (32 km) wide. Wind gusts in the city were estimated from 150 to 200 miles per hour (240 to 320 km/h);[7] a gust of 180 mph (290 km/h) was recorded by a Pan-American Airways anemometer before it was blown away. Similarly, another observation in the capital city recorded winds of 100 mph (160 km/h) before the roof it was on was damaged.[2] It was estimated as among the strongest hurricanes on record to strike the country.[1] Three entire districts of the city were almost completely destroyed, and an Associated Press report indicated "there was [scarcely] a wreck of a wall left standing".[8] Overall, the hurricane leveled about half of the entire city.[9] Due to its small nature, villagers 75 mi (121 km) from the landfall location had no knowledge of the storm. Heavy rainfall from the storm flooded the Ozama River and increased its flow to 15 mph (24 km/h), which prevented boats from traversing the river.[10] The passage of the hurricane caused severe damage estimated at $15–$50 million, with the storm considered a major disaster in the area. The Red Cross estimated 2,000 people died in the city, with an additional 8,000 injured.[2] Historians estimate the hurricane left between 2,000 and 8,000 killed.[11]

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.[2] Effects in the mountainous areas included downed trees and crop damage.[10] In Haiti, the hurricane produced locally gusty winds and heavy amounts of rainfall, though exact damage details for the nation are unknown.[8] Despite crossing the island of Cuba, no damage or deaths were reported there. Upon moving through the U.S. state of Florida, the storm remained severely weakened; during its passage a pressure of 1,006 mbar (29.7 inHg) was reported in Tampa, the lowest pressure in the state. The threat of the hurricane prompted the National Weather Bureau to issue storm warnings from Southport, North Carolina through the Virginia Capes. The strongest winds remained offshore, with minor damage reported along the Outer Banks. On Cape 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.[10]

Aftermath

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Destruction after the 1930 Dominican Republic Hurricane

Relief work in the Dominican Republic began immediately after the hurricane, personally organized by the then-new President Rafael Leónidas Trujillo. The president deployed the entire nation's military within 24 hours of the passage of the hurricane. By the day after its passage, lack of food had become a problem, and large numbers of robberies had occurred.[8] The winds downed all communications inside of the city,[10] leaving damage details unknown until communications were partially restored a day after its landfall. The city plant of the newspaper La Opinión was destroyed, with three staff members killed; the remaining workers transmitted a damage story to offices in New York City, and included a plea for disaster assistance. The Red Cross office in Washington, D.C., sent US$15,000 (equivalent to US$270,000 in 2023) in aid a day after the hurricane struck.[8]

See also

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References

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  1. ^ a b c d e Chris Landsea; et al. (2010). "Documentation of Atlantic Tropical Cyclones Changes in HURDAT". Hurricane Research Division. Archived from the original on 28 June 2011. Retrieved 2011-07-31.
  2. ^ a b c d e f g h F. Eugene Hartwell (1930). "The Santo Domingo Hurricane of September 1 to 5, 1930" (PDF). Weather Bureau Office in San Juan, Puerto Rico. Retrieved 2007-04-04.
  3. ^ "STEAMER OUTRIDES STOrm's FULL FURY; Caught in Vortex of Hurricane, Coamo Tilts Perilously as Gale Strips Decks". The New York Times. 5 September 1930.
  4. ^ Staff Writer (1930-09-06). "Two Dead in Dominica". The Milwaukee Journal. Associated Press. Retrieved 2011-07-31.[permanent dead link]
  5. ^ "First Caribbean Hurricane of the Season Reported". The Daily Gleaner. Vol. 96, no. 175. Kingston, Jamaica. The Daily Gleaner. 1930-09-02. p. 1 – via NewspaperArchive.com.
  6. ^ "Atlantic hurricane best track (HURDAT version 2)" (Database). United States National Hurricane Center. April 5, 2023. Retrieved September 4, 2024. Public Domain This article incorporates text from this source, which is in the public domain.
  7. ^ De Besault, Lawrence (2007). President Trujillo - His Work and the Dominican Republic. READ BOOKS. pp. 265–6. ISBN 978-1-4067-4641-9.
  8. ^ a b c d "Santo Doming Leveled by Hurricane; Believe 900 Dead, Injured in Hurricane". Ironwood Daily Globe. Vol. 11, no. 245. Ironwood, Michigan. Associated Press. 1930-09-04. p. 1. Retrieved 2019-07-03 – via Newspapers.com.
  9. ^ "Storm Dead at 300". Marshfield News-Herald. Vol. 10, no. 145. Marshfield, Wisconsin. Associated Press. 1930-09-04. Retrieved 2019-07-03 – via Newspapers.com.
  10. ^ a b c d Various (1930). "Appendices to the Santo Domingo Hurricane of September 1 to 5, 1930" (PDF). Weather Bureau Office. Retrieved 2007-04-12.
  11. ^ Edward N. Rappaport; Jose Fernandez-Partagas; Jack Beven (1997). "The Deadliest Atlantic Tropical Cyclones, 1492-1996". NOAA. Archived from the original on 26 May 2007. Retrieved 2007-04-12.
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