Subtropical Storm One On April 21, a
low-pressure area separated from the prevailing
westerlies about southeast of
Bermuda, and developed into a
subtropical depression at 1200
UTC. The system maintained a large comma-shaped cloud pattern around the low-level circulation. Operationally, it was not classified until 27 hours later. Isolated from strong steering currents, the depression tracked northwestward at , and intensified into a subtropical storm early on April 22. The
National Hurricane Center remarked the potential for the system transitioning into a
tropical cyclone. On April 23, the cyclone weakened to depression status due to strong
wind shear. Early on April 24, the subtropical depression turned eastward, maintaining limited convection. At the time, forecasters anticipated the depression would continue east-northeastward and become an
extratropical cyclone. By late on April 24, the system was too weak to classify using the
Dvorak technique, and the NHC ceased issuing advisories. Within 24 hours, the circulation dissipated as the system continued eastward through the westerlies. Operationally, the National Hurricane Center designated this system as Tropical Depression Two, which led to confusion because of Subtropical Storm One in April, and then another Tropical Depression Two in July. Outflow from
Hurricane Celia in the Pacific Ocean and a trough in the Gulf of Mexico generated wind shear on the depression, which prevented it from intensifying into a tropical storm. The depression dropped heavy rainfall in
Cuba, peaking at . Large amounts of precipitation resulted in flooding, which damaged or destroyed hundreds of homes and caused two fatalities in
provinces of
Pinar del Río and
La Habana. As the system was only a tropical depression, light winds were reported; however, a peak gust of was reported at
MacDill Air Force Base. Heavy rainfall fell on the west coast of Florida, with local amounts exceeded . Precipitation throughout the state peaked at in Arcadia Tower. Heavy rainfall caused flooding in portions of Florida, which in turn, destroyed 70 houses. In addition, five homes destroyed and twelve were damaged by a tornado spawned in
Nokomis. The depression caused two fatalities in Florida and damage totaled to $2.6 million (1992 USD).
Tropical Depression Two A squall line which moved offshore New York and southern
New England formed a
mesoscale convective vortex, which fired new thunderstorm activity each day as it moved within the
westerlies across the northern Atlantic. Once it reached mid-ocean, an increasingly northerly steering flow dropped the system down into the subtropics to the east of
Bermuda, and it maintained decent organization. By 2100 UTC on July 24, the National Hurricane Center began classifying the system as Tropical Depression Two. In the first advisory on the depression, it was noted that the previous tropical depression was erroneously classified as Tropical Depression Two. Due to northeasterly wind shear, the depression failed to intensified or organize further, as predicted. Instead, the depression weakened by late on July 25, with satellite imagery indicating that much of the deep convection was removed from the surface circulation. By July 26, the National Hurricane Center issued its final advisory, noting that it was "too weak to classify and is rapidly losing its identity". The depression dissipated about three hours later. and on August 23 the hurricane peaked with winds of . It crossed the
Bahamas at that intensity, weakened slightly, and re-intensified to a
Category 5 hurricane before making landfall near
Homestead, Florida. It weakened slightly over the state to a hurricane, but restrengthened to a hurricane over the Gulf of Mexico. A strong mid-latitude trough turned Andrew northward, where it greatly weakened before hitting west of
Morgan City, Louisiana on August 26 as a Category 3 hurricane. It turned northeastward, and lost its tropical identity over
Tennessee on August 28, before merging with the remnants of
Hurricane Lester and another
frontal system over
Pennsylvania on August 29. In the Bahamas, Andrew brought high tides, hurricane-force winds, and tornadoes, which caused significant damage in the archipelago, especially on
Cat Cays. At least 800 houses were destroyed and left damage to the transport, communications, water, sanitation, agriculture, and fishing sectors. Overall, Andrew caused four fatalities and $250 million in damage in the Bahamas. Throughout the southern portions of Florida, Andrew brought very high winds; a wind gust of was reported at a house in
Perrine, Florida. In the
Everglades, 70,000 acres (280 km2) of trees were knocked down and about 182 million fish were killed. Rainfall in Florida was moderate, peaking at in western Miami-Dade County. Significant damage to
oil platforms was reported, with one company losing 13 platforms, had 104 structures damaged, and five drilling wells blown off course. In Louisiana, Andrew produced hurricane-force winds along its path, An F3 tornado in
St. John the Baptist Parish damaged or destroyed 163 structures. 17 fatalities were reported in Louisiana, six of which were drowning victims offshore. Overall, Andrew caused 65 fatalities and $27.3 billion (1992 USD) in damage, making it the ninth-costliest hurricane in U.S. history, behind
Hurricane Katrina in 2005,
Hurricane Ike in 2008,
Hurricane Sandy in 2012, hurricanes
Harvey,
Irma,
Maria in 2017,
Hurricane Florence in 2018,
Hurricane Ida in 2021, and
Hurricane Ian in 2022
Hurricane Bonnie On September 11, a
cold front moved off the
U.S. East Coast and cloud cover began to slowly detach itself from the front and form into a tropical low. On September 17, the system organized into a tropical depression. On September 18, it was upgraded to Tropical Storm Bonnie and began to move slowly northeast. Low wind shear allowed Bonnie to quickly strengthen into a Category 2 hurricane before weakening slightly. On September 21, Bonnie restrengthened slightly and reached its peak intensity of 110 mph (175 km/h) sustained winds and a central pressure of 965 mbar. The next day, Bonnie began gradually weakening while turning eastward before reaching a ridge of
high pressure, stalling its motion. Convection began to diminish, and on September 24, Bonnie was downgraded to a tropical storm. On September 25, Bonnie was downgraded to a tropical depression. Bonnie then turned southeast while strengthening. Bonnie was operationally declared
extratropical on September 27 as it turned northeast until September 28. The storm then entered an environment with greater wind shear while accelerating northeast. The storm crossed over the Azores on September 30 with 65 mph (100 km/h) winds. Bonnie was then declared extratropical. The extratropical low drifted southwest in a clockwise loop, approaching the Azores again and dissipated October 2. In the
Azores, the
Lajes Air Base reported sustained winds of 40 mph (64 km/h) with gusts to 59 mph (94 km/h). In
São Miguel, a man was killed by a rock fall.
Hurricane Charley On September 20, METEOSAT imagery indicated an area of convection becoming concentrated while well south of the Azores. It is possible that a mid to upper-level cyclonic circulation interacted with the northern portion of a tropical wave. By the following day, satellite imagery noted a well-defined low-level circulation and thus, Tropical Depression Five while centered about south of the Azores. The depression tracked northwestward and satellite imagery began to indicate banding features. As a result, the depression was upgraded to Tropical Storm Charley on September 22. An eye developed as Charley tracked north-northwestward, and it became a hurricane on September 23. Further strengthening occurred, and by late on September 24, Charley peaked as a Category 2 hurricane. Thereafter, Charley turned eastward and then east-northeastward while tracking over decreasing
sea surface temperatures (SST). Early on September 27, Charley was downgraded to a tropical storm. Later that day, Charley crossed over
Terceira Island in the Azores with winds of . Charley gradually lost tropical characteristics, and by 1800 UTC on September 27, it had transitioned into an extratropical storm.
Tropical Storm Danielle Tropical Depression Six developed offshore of the Southeastern United States on September 22 from the merger of a surface trough, a tropical wave, and a cold front. The depression quickly intensified and was upgraded to Tropical Storm Danielle six hours later. An approaching trough caused a northeastward movement, but later a high pressure system forced the storm to northwestward, which caused Danielle to execute a small anti-cyclonic loop on September 23–24. While offshore of
North Carolina on September 25, Danielle reached its peak intensity as a moderately strong tropical storm with maximum sustained winds of . It was initially predicted that Danielle would make landfall in North Carolina; however, the storm curved north-northwestward and made landfall in
Maryland on the eastern shore of the
Delmarva Peninsula at the same intensity. Danielle continued inland and weakened and dissipated over eastern
Pennsylvania on September 26. Virginia, and Maryland, which resulted in overwash, which in turn, damaged or destroyed several businesses and houses in the coastal portions of the three states. In addition, street flooding also closed several roads in the region, most notably,
North Carolina Highway 12. In addition high seas offshore of
New Jersey capsized a sailboat, causing two people to drown. Overall, damage from the storm was minimal, with the exception of the damaged or destroyed businesses and houses in North Carolina, Virginia, and Maryland. Because the depression was tracking over warm SST, it was predicted to intensify into a tropical storm. However, wind shear exposed the center Early on September 27, the center of the depression became difficult to locate on satellite imagery. By September 28, the organization of the depression deteriorated further due to strong vertical wind shear. The center of the depression again became difficult to location by infrared images early on September 29. Later that day, a few computer models indicated a decrease in wind shear over the depression within two days, thus, it was predicted to strengthen into a tropical storm. However, wind shear exposed the center of the depression again by early on September 30, though it was still forecast to intensify to tropical storm status. By late on October 1, satellite imagery noted that the depression dissipated, and the National Hurricane Center issued its final advisory on the system.
Tropical Storm Earl On September 26, a tropical wave developed into Tropical Depression Eight while centered about north of
Hispaniola. The depression tracked west-northwestward toward the Bahamas. Initially, the depression remained weak, but after reaching the
Gulf Stream it strengthened into Tropical Storm Earl at 1200 UTC on September 29. Around that time, Earl began to veer east, lessening the threat to Florida. Early on October 1, Earl reached maximum sustained winds of and a minimum barometric pressure of . It gradually weakened thereafter, and Earl was downgraded to a tropical depression on October 3. Later that day, Earl became extratropical about south of
Bermuda. Because Earl remained offshore, impact was generally minor. and brought moderately heavy rainfall, peaking at near
Canal Point, Florida. In addition, light amounts of precipitation were also reported in
Georgia and North Carolina. Above normal tides washed away of beaches, and lifeguards on
St. Augustine Beach made eight rescues.
Hurricane Frances A low pressure area developed along the end of a quasi-stationary frontal trough. Initially, vertical wind shear prevented deep convection from forming on the western portion of the system. After wind shear decreased, the system became a gale center late on October 22. By early on the following day, the gale center had transitioned into a tropical storm, and it is estimated that Tropical Storm Frances developed at 0600 UTC on October 23. Frances quickly strengthened after becoming a tropical storm, and was upgraded to a hurricane by 1800 UTC on that same day. After becoming a hurricane, Frances curved northeastward, and remained well east of Bermuda. By midday on October 24, Frances peaked as an 85 mph (140 km/h) Category 1 hurricane. On land, Frances caused minimal impact, limited to light rainfall across Newfoundland. == Storm names ==