The storm was first noted around 500 miles (805 km) northeast of San Juan,Puerto Rico.[2] It then continued in a unusual and rare southwest direction before striking the island of Saint Kitts as a intense hurricane. The last observation occurred some 130 mi (210 km) north of Blanquilla,on March 9.[1]
Since the beginning of the basin's record in 1851,no tropical cyclone has occurred within a month before or after the formation of the hurricane. Only 3 hurricanes have been observed earlier into the calendar year,with all of them occurring in January. The earliest hurricane proceeding the formation of the storm occurred in mid-May of 1951.[1]
Meteorological history
Map plotting the storm's track and intensity,according to the Saffir–Simpson scale
The first observation of the storm was by a ship on March 6, at 12:00 UTC. Since the storm was already a intense tropical storm upon discovery, it attained hurricane status just 12 hours later. As the hurricane continued towards the southwest, it steadily intensified despite the hostile conditions that are typically present throughout the March equinox. Later that day on March 7, the hurricane intensified into a Category 2 with sustained winds of 100 mph (160 km/h). Peak intensity occurred around this time, roughly 30 miles (42 km) east of Saint Martin where their aneroid recorded a pressure of 988mbar (29.2inHg).[3] Shortly afterwards, the hurricane made its first and only landfall in Saint Kitts.[1]
Around 2 am local, Nevis recorded a minimum barometric pressure of 984mbar (29.1inHg). It held steady for half an hour, and occurred well outside the storm's center. The winds were reportedly of "hurricane force" at the time measurement, too.[4]Basseterre, St. Kitts also recorded a pressure of 991mbar (29.3inHg) that morning, outside the center.[5] In Antigua, roughly 70 miles (113 km) from the cyclone, it stood at 1,003mbar (29.6inHg). At 3 am, Saint Tomas had a reading of 1,009mbar (29.8inHg).[5]
After passing through the Leeward Islands, the hurricane began gradually weakening. It then fell below hurricane status at 06:00 UTC, March 9. The storm was lasted noted by ship before dissipating a couple hours later.[1][5] However, in the absence of modern satellite and other remote-sensing technologies, the storm's path and intensity beyond this point may have went undocumented.
It would seem that the cyclone in question followed a track opposite in every particular to the track usually followed by cyclones originating within the tropics in the hurricane season.
While passing through the Leeward Islands, damaging winds, heavy rainfall, and widespread destruction was reported on several islands.
On March 6, Saint Croix experienced a partly blue sky, rough seas, and a strong wind from the north. By the 7th, the seas and wind began to worsen and shifted toward the northeast. The weather continued to deteriorate into the morning. By 8 am local, the wind shifted ENE, to then SE at 11 am, and east at 4 pm. It remained gusty, but gradually decreased throughout the day. Rainfall amounted to less than 1 inch (2.5 cm) and a few trees were knocked down.[5][7] On that same day, Saint Tomas also experienced a heavy gale from the northwest and a drop in pressure. However, no damage was reported.[8][9]
In Saint Martin, damaging winds toppled tents and did considerable damage to crops.[3] In Saint Barthélemy, many buildings either damaged or completely blown down.[4] Vessels were also blown out to sea along the leeside of Saint Eustatiu. A ship call "Sea Hawk" was taken off her anchorage and discovered in Arroyo, Puerto Rico weeks later.[8] These islands were said to have been "devastated" by the hurricane.[5]
Extreme winds, rain, and damage was experienced in Saint Kitts. Crops were reportedly "severely damaged", with much of it being leveled into the ground.[10] At least 24 vessels and boats were driven ashore and were either badly damaged or entirely destroyed.[8] Trees and property were also blown down, while telephone lines stood damaged. In Nevis, extensive damage was caused by the storm. Ships were reportedly smashed into the pieces in the wharf, while large parts of the ports were either carried away or destroyed.[4]
Upon sunrise, the havoc and destruction was much more apparent. At least 1 man drowned when his ship sunk, while other reports on fatalities remain unknown.[4] Rainfall totals reached over 8 inches (20.3 cm) near Cayon, 4 inches (10.2 cm) in Basseterre, and 3 inches (7.6 cm) in Nevis.[8][10]
Records
Atlantic tropical storm and hurricane frequency, by month (1851-2017).
The 1908 hurricane formed opposite to that of the climatological peak of its season. Despite this, it still managed to be the first tropical cyclone to achieve Category 2 status during the off-season. 1-minute sustained winds peaked at 100 mph (160 km/h), which also makes it the strongest tropical cyclone before June.[1]
The storm was described as unusual, and a first of its kind by locals. Most notably was its unusual southwest trajectory & appearance so odd in the calendar year.[4][5] Despite its intensity, no other Atlantic tropical cyclone has been documented in March.[note 2][1] It's also the only storm to have reached hurricane status during the winter months of February-March-April (FMA).
Its landfall in Saint Kitts is the second earliest for a hurricane, only surpassed by Hurricane Alice on January 2nd.[note 3] The storm is also one of two hurricanes to strike the Lesser Antilles with non-tropical origins.[1]
1 2 3 4 5 6 Jose Fernandez Partagas & Henry F. Diaz (1997). Year 1908(PDF). Atlantic Oceanographic and Meteorological Laboratory (Report). Miami, Florida: National Oceanic and Atmospheric Administration. Retrieved June 9, 2016.
↑ Yes, There Was Once a March Atlantic Hurricane |March 08, 2020
↑ "Hurricanes Frequently Asked Questions". AOML.NOAA.gov. Atlantic Oceanographic and Meteorological Laboratory / National Oceanic and Atmospheric Administration. 1 June 2023. Archived from the original on 4 July 2024. (click on "What is the Total Number of Hurricanes and Average Number of Hurricanes in Each Month?")
↑ Hurricane Impacts on Land in the Central and Eastern Caribbean Since 1494 CE From Written Records (July 07, 2023) | by Michael Chenoweth & Ian Howard
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