An Atlantic–Pacific crossover hurricane is a
tropical cyclone that develops in the
Atlantic Ocean and moves into the
Pacific Ocean, or vice versa. Since reliable records began in 1851, a total of twenty-one crossover tropical cyclones have been recorded. As tropical cyclones must travel over land to pass between the Atlantic and Pacific basins, usually their
low-level circulation center dissipates and degenerate into
remnant lows before completing the crossing. In such instances, they are not considered the same system.[1]
Note: Information is mostly provided by the Atlantic best track.[1]
Other storms
There have also been numerous tropical cyclones that formed in one basin, dissipated, and re-developed in the other, which are not considered an Atlantic-Pacific crossover hurricane by the NHC. In
chronological order from earliest to most recent, they are:
The remnants of
Hurricane Janet in 1955 later led to the formation of an
unnamed tropical storm in the East Pacific on October 1;[3] the newly generated tropical cyclone later brought rains to the southwestern United States.[4]
In 1960,
Hurricane Abby made landfall over
Belize, then known as
British Honduras, and dissipated a day later while situated over the Mexican state of
Tabasco. Its remnants crossed over Mexico into the Pacific Ocean and regenerated into
Hurricane Celeste on July 20.[5]
In 1969,
Hurricane Francelia hit southern Belize, then known as British Honduras, weakening quickly over land and dissipating over Guatemala. The system continued slowly across Central America, crossing into the eastern Pacific Ocean three days after it moved ashore. Its remnants eventually redeveloped into
Tropical Storm Glenda off the coast of Mexico.[6][7]
Tropical Storm Chloe in 1971 made landfall in the
YucatĂĄn Peninsula and dissipated soon after. Its remnants continued into the Eastern Pacific and developed into
Hurricane Lily, which made landfall in southwest Mexico.[8]
In 1978,
Tropical Storm Bess went southward, affecting Mexico. Its remnants crossed into the Pacific Ocean, where it regenerated into
Hurricane Iva.[10]
Later in 1978,
Hurricane Cora's remnants crossed over Central America into the Pacific Ocean, where it reintensified, becoming
Hurricane Kristy.[10]
In 1988,
Tropical Depression Six degenerated into a tropical wave near the island of
Jamaica on August 23.[11] A day later it moved over Central America with minimal convection and redeveloped into
Hurricane Kristy once it reached the eastern Pacific.[12]
Hurricane Cosme in 1989 crossed from the Pacific, and its low-level circulation dissipated over northern Mexico. Its remnants merged with another tropical wave and contributed to the development of
Tropical Storm Allison in the Atlantic.[15]
Operationally, it was considered that
Tropical Storm Bret, from 1993, retained its circulation and was designated Tropical Depression Eight-E upon reaching the Pacific, later becoming
Hurricane Greg, but post-storm analysis determined that Bret actually dissipated over western
Nicaragua, with Greg forming from its remnants several days later.[16]
Tropical Depression Nine in 2001 made landfall in Nicaragua and degenerated into a tropical wave. The wave later regenerated into a tropical depression that became
Hurricane Juliette.[17]
Tropical Storm Alma of 2008 formed off of the West Coast of
Costa Rica, and made landfall in Nicaragua with sustained wind speeds up to 100 kilometres per hour (62 mph). The low-level circulation center of the storm soon dissipated. A day later, the storm's remnants regenerated on Nicaragua's east coast into
Tropical Storm Arthur, after encountering a pair of two
tropical waves, with sustained winds of 75 km/h (47 mph), and again made landfall in Nicaragua. It is not considered as crossover storm, as the original low-level circulation center had dissipated, and since the system also merged with another tropical wave prior to regeneration.[20][21]
Hurricane Barbara of 2013 made landfall in southwest Mexico and dissipated before reaching the
Gulf of Mexico. The remnants of Barbara and a cyclonic gyre led to the formation of a broad area of low pressure, which later became
Tropical Storm Andrea over the central Gulf of Mexico.[24]
The remnant moisture from
Hurricane Earl of 2016 interacted with a disturbance on the Pacific coast of Mexico, which contributed to the formation of
Tropical Storm Javier in the eastern Pacific.[26]
The remnants of
Tropical Storm Bret of 2017 traversed over Central America and emerged into the eastern Pacific, which led to the formation of
Hurricane Dora.[27]
Also in 2017,
Hurricane Franklin made landfall in the Mexican state of
Veracruz; its remnants moved across Mexico during the following day and emerged into the eastern Pacific, later developing into
Tropical Storm Jova.[28]
Later that year,
Hurricane Katia made landfall in Mexico and was then downgraded to a remnant low; its remnants crossed into the Pacific Ocean, where it regenerated into
Hurricane Otis.[29]
Tropical Storm Amanda of 2020 made landfall in southeastern Guatemala, rapidly weakened, and the storm's low-level circulation center dissipated. However, its remnant low-pressure area continued northward and eventually regenerated into
Tropical Storm Cristobal in the Bay of
Campeche.[30][31]
Hurricane Nana of 2020 made landfall in
Belize, weakened, and the storm's low-level circulation center dissipated over
Guatemala. After its mid-level circulation emerged into the Pacific, contrary to expectations, it developed a new surface low and regenerated into
Tropical Storm Julio.[32][33]
Hurricane Grace in 2021 made landfall in Mexico as a strong Category 3 hurricane, and the system's low-level circulation center soon dissipated. Its mid-level remnants emerged into the Eastern Pacific and redeveloped into
Tropical Storm Marty.[34][35]
Hurricane Agatha of 2022 made landfall in
Oaxaca then degenerated into a remnant low which dissipated inland, near the northern coast of the
Isthmus of Tehuantepec. The remnant low was absorbed into the disorganized disturbance complex that eventually became
Tropical Storm Alex.[36]
Hurricane Julia of 2022, itself a crossover system, made landfall in El Salvador and degraded to a remnant low over Guatemala. Its broad low-level circulation partially contributed to the formation of
Tropical Storm Karl over the Gulf of Mexico.[37]
Prior to 2000, storms were renamed after crossing from the Atlantic into the Eastern Pacific. At the 22nd hurricane committee in 2000 it was decided that tropical cyclones that moved from the Atlantic to the Eastern Pacific basin and vice versa would no longer be renamed.[39]Hurricane Otto in 2016 was the first storm to cross from one basin to another to apply under this rule.
^National Hurricane Center; Hurricane Research Division; Central Pacific Hurricane Center (2013-04-05).
"The Northeast and North Central Pacific hurricane database 1949-2012"(TXT). United States National Oceanic and Atmospheric Administration's National Weather Service. Retrieved 2013-12-23.
An Atlantic–Pacific crossover hurricane is a
tropical cyclone that develops in the
Atlantic Ocean and moves into the
Pacific Ocean, or vice versa. Since reliable records began in 1851, a total of twenty-one crossover tropical cyclones have been recorded. As tropical cyclones must travel over land to pass between the Atlantic and Pacific basins, usually their
low-level circulation center dissipates and degenerate into
remnant lows before completing the crossing. In such instances, they are not considered the same system.[1]
Note: Information is mostly provided by the Atlantic best track.[1]
Other storms
There have also been numerous tropical cyclones that formed in one basin, dissipated, and re-developed in the other, which are not considered an Atlantic-Pacific crossover hurricane by the NHC. In
chronological order from earliest to most recent, they are:
The remnants of
Hurricane Janet in 1955 later led to the formation of an
unnamed tropical storm in the East Pacific on October 1;[3] the newly generated tropical cyclone later brought rains to the southwestern United States.[4]
In 1960,
Hurricane Abby made landfall over
Belize, then known as
British Honduras, and dissipated a day later while situated over the Mexican state of
Tabasco. Its remnants crossed over Mexico into the Pacific Ocean and regenerated into
Hurricane Celeste on July 20.[5]
In 1969,
Hurricane Francelia hit southern Belize, then known as British Honduras, weakening quickly over land and dissipating over Guatemala. The system continued slowly across Central America, crossing into the eastern Pacific Ocean three days after it moved ashore. Its remnants eventually redeveloped into
Tropical Storm Glenda off the coast of Mexico.[6][7]
Tropical Storm Chloe in 1971 made landfall in the
YucatĂĄn Peninsula and dissipated soon after. Its remnants continued into the Eastern Pacific and developed into
Hurricane Lily, which made landfall in southwest Mexico.[8]
In 1978,
Tropical Storm Bess went southward, affecting Mexico. Its remnants crossed into the Pacific Ocean, where it regenerated into
Hurricane Iva.[10]
Later in 1978,
Hurricane Cora's remnants crossed over Central America into the Pacific Ocean, where it reintensified, becoming
Hurricane Kristy.[10]
In 1988,
Tropical Depression Six degenerated into a tropical wave near the island of
Jamaica on August 23.[11] A day later it moved over Central America with minimal convection and redeveloped into
Hurricane Kristy once it reached the eastern Pacific.[12]
Hurricane Cosme in 1989 crossed from the Pacific, and its low-level circulation dissipated over northern Mexico. Its remnants merged with another tropical wave and contributed to the development of
Tropical Storm Allison in the Atlantic.[15]
Operationally, it was considered that
Tropical Storm Bret, from 1993, retained its circulation and was designated Tropical Depression Eight-E upon reaching the Pacific, later becoming
Hurricane Greg, but post-storm analysis determined that Bret actually dissipated over western
Nicaragua, with Greg forming from its remnants several days later.[16]
Tropical Depression Nine in 2001 made landfall in Nicaragua and degenerated into a tropical wave. The wave later regenerated into a tropical depression that became
Hurricane Juliette.[17]
Tropical Storm Alma of 2008 formed off of the West Coast of
Costa Rica, and made landfall in Nicaragua with sustained wind speeds up to 100 kilometres per hour (62 mph). The low-level circulation center of the storm soon dissipated. A day later, the storm's remnants regenerated on Nicaragua's east coast into
Tropical Storm Arthur, after encountering a pair of two
tropical waves, with sustained winds of 75 km/h (47 mph), and again made landfall in Nicaragua. It is not considered as crossover storm, as the original low-level circulation center had dissipated, and since the system also merged with another tropical wave prior to regeneration.[20][21]
Hurricane Barbara of 2013 made landfall in southwest Mexico and dissipated before reaching the
Gulf of Mexico. The remnants of Barbara and a cyclonic gyre led to the formation of a broad area of low pressure, which later became
Tropical Storm Andrea over the central Gulf of Mexico.[24]
The remnant moisture from
Hurricane Earl of 2016 interacted with a disturbance on the Pacific coast of Mexico, which contributed to the formation of
Tropical Storm Javier in the eastern Pacific.[26]
The remnants of
Tropical Storm Bret of 2017 traversed over Central America and emerged into the eastern Pacific, which led to the formation of
Hurricane Dora.[27]
Also in 2017,
Hurricane Franklin made landfall in the Mexican state of
Veracruz; its remnants moved across Mexico during the following day and emerged into the eastern Pacific, later developing into
Tropical Storm Jova.[28]
Later that year,
Hurricane Katia made landfall in Mexico and was then downgraded to a remnant low; its remnants crossed into the Pacific Ocean, where it regenerated into
Hurricane Otis.[29]
Tropical Storm Amanda of 2020 made landfall in southeastern Guatemala, rapidly weakened, and the storm's low-level circulation center dissipated. However, its remnant low-pressure area continued northward and eventually regenerated into
Tropical Storm Cristobal in the Bay of
Campeche.[30][31]
Hurricane Nana of 2020 made landfall in
Belize, weakened, and the storm's low-level circulation center dissipated over
Guatemala. After its mid-level circulation emerged into the Pacific, contrary to expectations, it developed a new surface low and regenerated into
Tropical Storm Julio.[32][33]
Hurricane Grace in 2021 made landfall in Mexico as a strong Category 3 hurricane, and the system's low-level circulation center soon dissipated. Its mid-level remnants emerged into the Eastern Pacific and redeveloped into
Tropical Storm Marty.[34][35]
Hurricane Agatha of 2022 made landfall in
Oaxaca then degenerated into a remnant low which dissipated inland, near the northern coast of the
Isthmus of Tehuantepec. The remnant low was absorbed into the disorganized disturbance complex that eventually became
Tropical Storm Alex.[36]
Hurricane Julia of 2022, itself a crossover system, made landfall in El Salvador and degraded to a remnant low over Guatemala. Its broad low-level circulation partially contributed to the formation of
Tropical Storm Karl over the Gulf of Mexico.[37]
Prior to 2000, storms were renamed after crossing from the Atlantic into the Eastern Pacific. At the 22nd hurricane committee in 2000 it was decided that tropical cyclones that moved from the Atlantic to the Eastern Pacific basin and vice versa would no longer be renamed.[39]Hurricane Otto in 2016 was the first storm to cross from one basin to another to apply under this rule.
^National Hurricane Center; Hurricane Research Division; Central Pacific Hurricane Center (2013-04-05).
"The Northeast and North Central Pacific hurricane database 1949-2012"(TXT). United States National Oceanic and Atmospheric Administration's National Weather Service. Retrieved 2013-12-23.