The list of unnamed tropical cyclones since naming began includes all tropical cyclones that met the criteria for naming in a basin, but that for whatever reason, did not receive a name. These systems have occurred in all basins and for various reasons.
Naming has been used since the 1950 season. In order to ease communications and advisories, [1] tropical cyclones are named when, according to the appropriate Regional Specialized Meteorological Center or Tropical Cyclone Warning Center, it has reached tropical storm status. A tropical cyclone with winds of tropical storm intensity or higher goes unnamed when operationally, it is not considered to have met the criteria for naming. Reasons for this include:
Only unnamed subtropical cyclones that could have been named are included. This excludes several that existed, but that were unnamed because subtropical cyclones were not named when they existed.
Storm | Year | Peak classification |
---|---|---|
Twelve | 1950 | Tropical storm |
Fifteen | 1950 | Tropical storm |
Sixteen | 1950 | Tropical storm |
One | 1951 | Tropical storm |
Twelve | 1951 | Category 1 hurricane |
"Groundhog Day" | 1952 | Tropical storm |
Three | 1952 | Tropical storm |
Five | 1952 | Tropical storm |
Eight | 1952 | Tropical storm |
Eleven | 1952 | Tropical storm |
Two | 1953 | Tropical storm |
Five | 1953 | Tropical storm |
Eight | 1953 | Tropical storm |
Eleven | 1953 | Tropical storm |
Thirteen | 1953 | Tropical storm |
One | 1954 | Tropical storm |
Two | 1954 | Tropical storm |
Four | 1954 | Tropical storm |
Nine | 1954 | Tropical storm |
Eleven | 1954 | Tropical storm |
Thirteen | 1954 | Category 2 hurricane |
Fifteen | 1954 | Tropical storm |
Five | 1955 | Tropical storm |
Eleven | 1955 | Tropical storm |
Twelve | 1955 | Tropical storm |
One | 1956 | Tropical storm |
Two | 1956 | Tropical storm |
Nine | 1956 | Tropical storm |
Ten | 1956 | Tropical storm |
Twelve | 1956 | Tropical storm |
One | 1957 | Tropical storm |
Eight | 1957 | Tropical storm |
One | 1958 | Tropical storm |
Twelve | 1958 | Tropical storm |
Storm | Year | Peak classification |
---|---|---|
"Escuminac" | 1959 | Category 1 hurricane |
Six | 1959 | Tropical storm |
Eight | 1959 | Tropical storm |
Nine | 1959 | Tropical storm |
"Texas" | 1960 | Tropical storm |
Six | 1960 | Tropical storm |
Six | 1961 | Tropical storm |
Twelve | 1961 | Tropical storm |
One | 1962 | Tropical storm |
Ten | 1962 | Category 1 hurricane |
One | 1963 | Tropical storm |
Four | 1963 | Category 1 hurricane |
One | 1964 | Tropical storm |
Two | 1964 | Tropical storm |
Three | 1964 | Category 1 hurricane |
Thirteen | 1964 | Tropical storm |
One | 1965 | Tropical storm |
Four | 1965 | Tropical storm |
Seven | 1965 | Tropical storm |
Nine | 1965 | Tropical storm |
Ten | 1965 | Tropical storm |
Two | 1966 | Tropical storm |
Fourteen | 1966 | Tropical storm |
Fifteen | 1966 | Tropical storm |
One | 1967 | Tropical storm |
Two | 1967 | Tropical storm |
Four | 1967 | Tropical storm |
Eight | 1967 | Tropical storm |
Twelve | 1967 | Tropical storm |
Five | 1968 | Tropical storm |
Ten | 1969 | Category 1 hurricane |
Eleven | 1969 | Tropical storm |
Sixteen | 1969 | Tropical storm |
Seventeen | 1969 | Category 1 hurricane |
Storm | Year | Peak classification |
---|---|---|
Eight | 1970 | Category 1 hurricane |
Ten | 1970 | Tropical storm |
Twenty-One | 1970 | Tropical storm |
"Caribbean–Azores" | 1970 | Category 1 hurricane |
"Canada" | 1970 | Category 2 hurricane |
Nineteen | 1970 | Category 2 hurricane |
Twenty-Three | 1970 | Tropical storm |
Two | 1971 | Category 1 hurricane |
"Gulf Coast" | 1987 | Tropical storm |
Unnamed | 1988 | Tropical storm |
"Perfect Storm" [nb 1] | 1991 | Category 1 hurricane |
Unnamed [nb 2] | 1997 | Subtropical storm |
Unnamed [nb 2] | 2000 | Subtropical storm |
"Azores" | 2005 | Subtropical storm |
Unnamed | 2006 | Tropical storm |
Unnamed [nb 3] | 2011 | Tropical storm |
Unnamed | 2013 | Subtropical storm |
Unnamed | 2023 | Subtropical storm |
The South Atlantic is not officially classified as a tropical cyclone basin by the World Meteorological Organization and does not have a designated regional specialized meteorological center (RSMC) that gives official names to tropical cyclones. Despite this, in 2011, the Hydrographic Center of the Brazilian Navy began giving unofficial names to tropical and subtropical cyclones in the south Atlantic. Prior to that, a few systems in the south Atlantic were given names.
There has been one system, Tropical Storm 01Q in 2021, that was monitored and designated 01Q by the National Oceanic and Atmospheric Administration (NOAA). However, the Brazilian Navy did not recognize the system as a tropical cyclone and it remains unnamed.
Naming began in 1960. Before 1960, a few systems in the central Pacific basin were given names, generally in an ad hoc manner.
Storm | Year | Peak classification |
---|---|---|
Four [nb 4] | 1962 | Tropical storm |
Hurricane "C" | 1962 | Unknown |
Tropical Storm "R" | 1962 | Tropical storm |
Tropical Storm "T" | 1962 | Tropical storm |
Tropical Storm "X" | 1962 | Tropical storm |
Tropical Storm "Z" | 1962 | Tropical storm |
Tropical Storm "A" | 1962 | Tropical storm |
Seven [nb 5] | 1962 | Tropical storm |
Four [nb 6] | 1963 | Tropical storm |
"Pacific Northwest" | 1975 | Category 1 hurricane |
Unnamed [nb 7] | 1996 | Tropical storm |
Unnamed [nb 8] | 2020 | Tropical storm |
The official practice of tropical cyclone naming started in 1945 within the western north Pacific. [14] [15] Due to differences in wind speed criteria between the Japan Meteorological Agency and the Joint Typhoon Warning Center, a system will sometimes be considered a tropical storm by the JTWC but only a depression by the JMA, or vice versa. This results in several apparent unnamed systems. Prior to 2000, the JTWC was responsible for tropical cyclone naming, with the JMA assuming responsibility for naming from 2000 and beyond. Due to this, unnamed cyclones that met the JMA's tropical storm criteria but not those of the JTWC prior to 2000 are excluded. Likewise, systems that met the JTWC's tropical storm criteria but not those of the JMA from 2000 to present are also excluded.
Storm | Year | Peak classification |
---|---|---|
Tropical Storm 24W | 1948 | Tropical storm |
Tropical Storm 26W | 1948 | Tropical storm |
Tropical Storm 02W | 1950 | Tropical storm |
Tropical Storm 12W | 1952 | Tropical storm |
Tropical Storm 14W | 1952 | Tropical storm |
Tropical Storm 04W | 1953 | Tropical storm |
Tropical Storm 09W | 1953 | Tropical storm |
Tropical Storm 13W | 1953 | Tropical storm |
Tropical Storm 16W | 1953 | Tropical storm |
Tropical Storm 22W | 1953 | Tropical storm |
Tropical Storm 23W | 1953 | Tropical storm |
Tropical Storm 01W | 1954 | Tropical storm |
Tropical Storm 07W | 1954 | Tropical storm |
Tropical Storm 08W | 1954 | Tropical storm |
Tropical Storm 15W | 1954 | Tropical storm |
Storm | Year | Peak classification |
---|---|---|
Tropical Storm 09W | 1955 | Tropical storm |
Tropical Storm 17W | 1955 | Tropical storm |
Tropical Storm 20W | 1955 | Tropical storm |
Tropical Storm 02W | 1956 | Tropical storm |
Tropical Storm 04W | 1956 | Tropical storm |
Tropical Storm 08W | 1956 | Tropical storm |
Tropical Storm 18W | 1956 | Tropical storm |
Tropical Storm 01W | 1957 | Tropical storm |
Tropical Storm 08W | 1957 | Tropical storm |
Tropical Storm 17W | 1957 | Tropical storm |
Tropical Storm 06W | 1995 | Tropical storm |
Tropical Storm 24W [nb 9] | 1996 | Tropical storm |
Tropical Storm 35W | 1996 | Tropical storm |
Tropical Storm 38W | 1996 | Tropical storm |
Tropical Storm 03W | 1998 | Tropical storm |
Due to differences in wind speed criteria between the India Meteorological Department and the Joint Typhoon Warning Center, a system will sometimes be considered a tropical storm by the JTWC but only a depression by the IMD. This results in several apparent unnamed systems. Because the IMD is responsible for naming, unnamed cyclones that met the JTWC's tropical storm criteria but not those of the IMD are excluded.
Naming has taken place since mid-2003.
There have been no unnamed tropical cyclones using the India Meteorological Department's criteria. One system, 2007's Yemyin, was upgraded after the fact and retroactively named. [16]
Tropical cyclones have been named within this basin since 1960, with any tropical or subtropical depressions that RSMC La Réunion analyze as having 10-minute sustained windspeeds of at least 65 km/h, 40 mph being named. However, unlike other basins RSMC La Réunion does not name tropical depressions, as they delegate the rights to name tropical cyclones to the subregional tropical cyclone warning centers in Mauritius or Madagascar depending on whether the system is located east or west of the 55th meridian east.
Storm | Year | Peak classification |
---|---|---|
Moderate Tropical Storm F1 | 1998–99 | Moderate tropical storm |
Subtropical Depression 13 | 1999–2000 | Subtropical depression |
Moderate Tropical Storm 10 | 2000–01 | Moderate tropical storm |
Subtropical Depression 11 | 2000–01 | Subtropical depression |
Subtropical Depression 15 | 2006–07 | Subtropical depression |
Tropical Cyclone 01U | 2007–08 | Category 1 tropical cyclone |
Subtropical Depression 10 | 2009–10 | Subtropical depression |
Subtropical Depression 09 | 2010–11 | Subtropical depression |
Subtropical Depression 13 | 2013–14 | Subtropical depression |
Moderate Tropical Storm 01 | 2018–19 | Moderate tropical storm |
Moderate Tropical Storm 08 | 2021–22 | Moderate tropical storm |
Moderate Tropical Storm 09 | 2022–23 | Moderate tropical storm |
Storm | Year | Peak classification |
---|---|---|
Five | 1964–65 | Unknown |
Six | 1964–65 | Unknown |
Six | 1965–66 | Unknown |
Nine | 1965–66 | Unknown |
Two | 1967–68 | Unknown |
Three | 1967–68 | Unknown |
Eleven | 1967–68 | Unknown |
Thirteen | 1967–68 | Unknown |
Seventeen | 1967–68 | Unknown |
Fifteen | 1968–69 | Unknown |
Sixteen | 1968–69 | Unknown |
One | 1969–70 | Unknown |
Seven | 1969–70 | Unknown |
Storm | Year | Peak classification |
---|---|---|
"Flores" [17] | 1972–73 | Category 3 severe tropical cyclone |
Tropical Cyclone 04U | 1981–82 | Category 1 tropical cyclone |
Tropical Cyclone 06U | 1983–84 | Category 1 tropical cyclone |
Tropical Cyclone 01U | 2002–03 | Category 2 tropical cyclone |
Tropical Cyclone 01U [18] | 2007–08 | Category 1 tropical cyclone |
Tropical Cyclone 25U [19] | 2010–11 | Category 1 tropical cyclone |
Tropical Cyclone 22U [20] | 2016–17 | Category 2 tropical cyclone |
Tropical Cyclone 01U | 2022–23 | Category 1 tropical cyclone |
Storm | Year | Peak classification |
---|---|---|
One | 1971–72 | Category 1 tropical cyclone |
Six | 1971–72 | Category 1 tropical cyclone |
One | 1973–74 | Category 1 tropical cyclone |
Five | 1976–77 | Category 1 tropical cyclone |
Six | 1976–77 | Category 1 tropical cyclone |
Five | 1980–81 | Category 2 tropical cyclone |
Seven | 1980–81 | Category 1 tropical cyclone |
Four | 1983–84 | Category 1 tropical cyclone |
Six | 1983–84 | Category 1 tropical cyclone |
One | 1984–85 | Category 1 tropical cyclone |
Tropical Cyclone 19P | 1986–87 | Category 2 tropical cyclone |
Two | 1990–91 | Category 1 tropical cyclone |
Tropical Cyclone 29P [nb 10] | 1996–97 | Category 2 tropical cyclone |
Tropical cyclones are ranked on one of five tropical cyclone intensity scales, according to their maximum sustained winds and which tropical cyclone basins they are located in. Only a few scales of classifications are used officially by the meteorological agencies monitoring the tropical cyclones, but other scales also exist, such as accumulated cyclone energy, the Power Dissipation Index, the Integrated Kinetic Energy Index, and the Hurricane Severity Index.
The 2008 Pacific typhoon season was a below average season which featured 22 named storms, eleven typhoons, and two super typhoons. The season had no official bounds; it ran year-round in 2008, but most tropical cyclones tend to form in the northwestern Pacific Ocean between May and November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean.
Hurricane Ekeka was the most intense off-season tropical cyclone on record in the northeastern Pacific basin. The first storm of the 1992 Pacific hurricane season, Ekeka developed on January 28 well to the south of Hawaii. It gradually intensified to reach major hurricane status on February 2, although it subsequently began to weaken due to unfavorable high wind shear. It crossed the International Date Line as a weakened tropical storm, and shortly thereafter degraded to tropical depression status. Ekeka continued westward, passing through the Marshall Islands and later over Chuuk State, before dissipating on February 9 about 310 miles (500 km) off the north coast of Papua New Guinea. The storm did not cause any significant damage or deaths.
The 2012 Pacific typhoon season was a slightly above average season that produced 25 named storms, fourteen typhoons, and four intense typhoons. It was a destructive and the second consecutive year to be the deadliest season. It was an event in the annual cycle of tropical cyclone formation, in which tropical cyclones form in the western Pacific Ocean. The season ran throughout 2012, though most tropical cyclones typically develop between May and October. The season's first named storm, Pakhar, developed on March 28, while the season's last named storm, Wukong, dissipated on December 29. The season's first typhoon, Guchol, reached typhoon status on June 15, and became the first super typhoon of the year on June 17.
The 2010 Pacific typhoon season, with 14 named storms, was the least active Pacific typhoon season on record. Seven of them strengthened into typhoons while one reached super typhoon intensity. The Pacific typhoon season during 2010 was in fact less active than the 2010 Atlantic hurricane season, with only three other occurrences of that happening, 2005, 2020, and 2023. In the same year, the Pacific hurricane season broke the same record being the least active season on record. During the season, no storms made landfall in mainland Japan, only the second such occurrence since 1988. Also, all of the 14 named storms developed west of 150°E.
This timeline documents all of the events of the 2009 Pacific typhoon season which was the period that tropical cyclones formed in the Western Pacific Ocean during 2009, with most of the tropical cyclones forming between May and November. The scope of this article is limited to the Pacific Ocean, north of the equator between 100°E and the International Date Line. Tropical storms that form in the entire Western Pacific basin are assigned a name by the Japan Meteorological Agency. Tropical depressions that form in this basin are given a number with a "W" suffix by the United States' Joint Typhoon Warning Center. In addition, the Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) assigns names to tropical cyclones that enter or form in the Philippine area of responsibility. These names, however, are not in common use outside of the Philippines.
The 2011 Pacific typhoon season was a below average season that produced a total of 21 named storms, 8 typhoons, and four super typhoons. This season was much more active than the previous season, although both seasons were below the Pacific typhoon average of 26. The season ran throughout 2011, though most tropical cyclone tend to develop between May and October. The season's first named storm, Aere, developed on May 7 while the season's last named storm, Washi dissipated on December 19.
The 2013 Pacific typhoon season was the most active Pacific typhoon season since 2004, and the deadliest since 1975. It featured Typhoon Haiyan, one of the most powerful storms and one of the strongest landfalling tropical cyclones in history. It was an above-average season with 31 named storms, 13 typhoons, and five super typhoons. The season's first named storm, Sonamu, developed on January 4 while the season's last named storm, Podul, dissipated on November 15. Despite the activity, most of the first seventeen named storms before mid-September were relatively weak, as only two of them reached typhoon intensity. Total damage amounted to at least $26.41 billion (USD), making it at the time the costliest Pacific typhoon season on record; it is currently the third costliest, behind the 2018 and 2019 seasons.
The 2015 Pacific typhoon season was a slightly above average season that produced twenty-seven tropical storms, eighteen typhoons, and nine super typhoons. The season ran throughout 2015, though most tropical cyclones typically develop between May and November. The season's first named storm, Mekkhala, developed on January 15, while the season's last named storm, Melor, dissipated on December 17. The season saw at least one named tropical system forming in each of every month, the first time since 1965. Similar to the previous season, this season saw a high number of super typhoons. Accumulated cyclone energy (ACE) during 2015 was extremely high, the third highest since 1970, and the 2015 ACE has been attributed in part to anthropogenic warming.
Typhoon Ma-on, known in the Philippines as Typhoon Ineng, was a large and powerful typhoon that affected southern Japan in July 2011. It was the sixth named storm and second typhoon of the 2011 Pacific typhoon season. Originating from an area of low pressure near Wake Island on July 9, the precursor to Ma-on gradually developed as it moved westward. By July 11, it had become sufficiently organized to be declared a tropical depression, although the cyclone's circulation remained broad. Over the following days, Ma-on gradually intensified and attained typhoon status on July 14. Favorable environmental conditions allowed for additional strengthening, and the storm ultimately attained peak ten-minute sustained winds of 175 km/h (109 mph) on July 16. After turning northward in response to a weakening subtropical ridge, the typhoon underwent a series of eyewall replacement cycles that caused it to weaken. On July 19, Ma-on struck Shikoku before turning southeastward and moving back over water. Slow weakening continued as Ma-on succumbed to the effects of high wind shear. The system ultimately became extratropical on July 24, and was last noted by the Japan Meteorological Agency a week later near the Kamchatka Peninsula.
The 2020 Pacific typhoon season was the first with below-average tropical cyclone activity since 2017, with 23 named storms, 10 of which became typhoons and only 2 became super typhoons. This low activity was a consequence of La Niña that persisted from the summer of the year. It had the fifth-latest start in the basin on record, slightly behind 1973, and was the first to start that late since 2016. The first half of the season was unusually inactive, with only four systems, two named storms and one typhoon at the end of July. Additionally, the JTWC recorded no tropical cyclone development in the month of July, the first such occurrence since reliable records began. The season's first named tropical cyclone, Vongfong, developed on May 8, while the season's last named tropical cyclone, Krovanh, dissipated on December 24. However, the season's last system was an unnamed tropical depression which dissipated on December 29.
Severe Tropical Storm Rumbia, known in the Philippines as Tropical Storm Gorio, was a tropical cyclone that brought widespread flooding in areas of the Philippines and China late June and early July 2013. The sixth internationally named storm of the season, Rumbia formed from a broad area of low pressure situated in the southern Philippine Sea on June 27. Steadily organizing, the initial tropical depression moved towards the northwest as the result of a nearby subtropical ridge. On June 28, the disturbance strengthened to tropical storm strength, and subsequently made its first landfall on Eastern Samar in the Philippines early the following day. Rumbia spent roughly a day moving across the archipelago before emerging into the South China Sea. Over open waters, Rumbia resumed strengthening, and reached its peak intensity with winds of 95 km/h (50 mph) on July 1, ranking it as a severe tropical storm. The tropical cyclone weakened slightly before moving ashore the Leizhou Peninsula late that day. Due to land interaction, Rumbia quickly weakened into a low pressure area on July 2 and eventually dissipated soon afterwards.
Most of the tropical cyclones of the 2013 Pacific typhoon season formed between May and November of that year. The scope of this article is the Pacific Ocean north of the equator, between 100°E and the International Date Line. Tropical storms which form in the Western Pacific basin are assigned a name by the Japan Meteorological Agency (JMA). Tropical depressions forming in this basin are given a number with a "W" suffix by the United States' Joint Typhoon Warning Center (JTWC). The Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) assigns names to tropical cyclones that enter or form in the Philippine area of responsibility, but these names are not in common use outside the Philippines.
This timeline documents all of the events of the 2014 Pacific typhoon season. Most of the tropical cyclones forming between May and November. The scope of this article is limited to the Pacific Ocean, north of the equator between 100°E and the International Date Line. Tropical storms that form in the entire Western Pacific basin are assigned a name by the Japan Meteorological Agency. Tropical depressions that form in this basin are given a number with a "W" suffix by the United States' Joint Typhoon Warning Center. In addition, the Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) assigns names to tropical cyclones that enter or form in the Philippine area of responsibility. These names, however, are not in common use outside of the Philippines.
Tropical Storm Lingling, known in the Philippines as Tropical Depression Agaton, was a weak but deadly tropical cyclone that affected the Philippines in January 2014. The first named storm of the annual typhoon season, this early-season cyclone remained very disorganized throughout its lifespan. Lingling was the first major natural disaster in the Philippines after Typhoon Haiyan just two months earlier, as it caused widespread landslide incidents and floods in Mindanao, resulting in 70 deaths and damage amounting to over 566 million pesos on the island.
Hurricane Genevieve, also referred to as Typhoon Genevieve, was the first tropical cyclone to track across all three northern Pacific basins since Hurricane Dora in 1999. Genevieve developed from a tropical wave into the eighth tropical storm of the 2014 Pacific hurricane season well east-southeast of Hawaii on July 25. However, increased vertical wind shear caused it to weaken into a tropical depression by the following day and degenerate into a remnant low on July 28. Late on July 29, the system regenerated into a tropical depression, but it weakened into a remnant low again on July 31, owing to vertical wind shear and dry air.
Typhoon Kim, known in the Philippines as Typhoon Osang, was the second typhoon in a week to directly affect the Philippines during July 1980. Like Typhoon Joe, Kim formed from the near equatorial monsoon trough in the northwestern Pacific Ocean on July 19. The disturbance tracked quickly westward-northwest underneath a subtropical ridge, reaching tropical storm strength on the July 21 and typhoon strength on July 23. After developing an eye, Kim began to rapidly intensify, and during the afternoon of July 24, peaked in intensity as a super typhoon. Several hours later, Kim made landfall over the Philippines, but the storm had weakened considerably by this time. Throughout the Philippines, 40 people were killed, 2 via drownings, and 19,000 others were directly affected. A total of 12,000 homes were destroyed and 5,000 villages were flooded. Less than a week earlier, the same areas were affected by Joe; however, Kim was considered the more damaging of the two typhoons. Land interaction took its toll on Kim, and upon entering the South China Sea, the storm was down below typhoon intensity. Kim continued northwestward but its disrupted circulation prevented re-intensification, and it remained a tropical storm until hitting southern China July 27 to the northeast of Hong Kong, where only slight damage was reported. Later that day, Kim dissipated.
This timeline documents all of the events of the 2015 Pacific typhoon season. Most of the tropical cyclones formed between May and November. The scope of this article is limited to the Pacific Ocean, north of the equator between 100°E and the International Date Line. This area, called the Western Pacific basin, is the responsibility of the Japanese Meteorological Agency (JMA). They host and operate the Regional Specialized Meteorological Center (RSMC), located in Tokyo. The Japanese Meteorological Agency (JMA) is also responsible for assigning names to all tropical storms that are formed within the basin. However, any storm that enters or forms in the Philippine Area of Responsibility (PAR) will be named by the Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) using a local name. Also of note - the Western Pacific basin is monitored by the United States' Joint Typhoon Warning Center (JTWC), which gives all Tropical depressions a number with a "W" suffix.
The 2021 Pacific typhoon season was the second consecutive to have below-average tropical cyclone activity, with twenty-two named storms, and was the least active since 2011. Nine became typhoons, and five of those intensified into super typhoons. This low activity was caused by a strong La Niña that had persisted from the previous year. The season's first named storm, Dujuan, developed on February 16, while the last named storm, Rai, dissipated on December 21. The season's first typhoon, Surigae, reached typhoon status on April 16. It became the first super typhoon of the year on the next day, also becoming the strongest tropical cyclone in 2021. Surigae was also the most powerful tropical cyclone on record in the Northern Hemisphere for the month of April. Typhoons In-fa and Rai are responsible for more than half of the total damage this season, adding up to a combined total of $2.02 billion.
During 2023, tropical cyclones formed in seven major bodies of water, commonly known as tropical cyclone basins. They were named by various weather agencies when they attained maximum sustained winds of 35 knots. Throughout the year, a total of 115 systems formed, 79 of them being named. The most intense storms of the year were Typhoons Mawar and Bolaven, which both had a minimum pressure of 900 hPa (26.58 inHg). The deadliest and costliest tropical cyclone of the year was Cyclone Daniel, which killed at least 10,028 people in Libya, Greece, Turkey, and Bulgaria, and caused at least US$21.14 billion worth of damage. Among this year's systems, thirty became major tropical cyclones, of which nine intensified into Category 5 tropical cyclones on the Saffir–Simpson scale (SSHWS). This year, for the first time on record, at least one such Category 5 system formed in each tropical cyclone basin: Mawar and Bolaven in the western Pacific Ocean, Jova and Otis in the eastern Pacific, Lee in the Atlantic, Mocha in the North Indian Ocean, Freddy in the southwest Indian Ocean, Ilsa in the Australian region, and Kevin in the South Pacific. The accumulated cyclone energy (ACE) index for the 2023, as calculated by Colorado State University (CSU) was 897.9 units overall.
Unless otherwise indicated, all storms come from the following datasets from the Regional Specialized Meteorological Center: