In 1902, there were 24 tropical cyclones across the northwestern Pacific Ocean, north of the equator and west of the International Date Line. There were at least 11 typhoons, which are tropical cyclones with sustained winds of at least 119 kilometres per hour (74 mph). The most effective storm of the year was an unnamed storm that spawned on October 1. The storm caused 600 fatalities and damages to Japan. Another unnamed storm, which formed on July 16, killed 20 people in Hong Kong.
No storms were recorded between January and April. The first storm of the year was a tropical storm that formed on May 19 and dissipated on May 24. Multiple typhoons formed across the Philippine archipelago in the following months. Another powerful storm formed on July 23, which caused damage to a camp and lead to three indirect fatalities. The last storm formed on November 7 and dissipated on November 11.
No activity was recorded within the months of January and April. [1]
On May 19, a tropical storm spawned to the east of Samar Island. The storm moved north, curving along Luzon and Taiwan. Then the storm started moving northeast, dissipating a few days later on May 24, just south of Japan. [2]
On June 1, a storm spawned east of Cagayan, drifting northwest. The storm made landfall over the Spratly Islands the next day. Over the following days, the storm drifted northwest on the South China Sea before making landfall on China on June 5, dissipating soon after. [3] On June 30, a storm spawned. The storm drifted northeast and ended up in the southern portion of Japan. The storm dissipated shortly after, on July 3. [4]
On July 7, a typhoon spawned east of Samar Island. The storm moved west, impacting the northern portion of Samar. The next day, the typhoon made landfall over Masbate. The next day, the storm made landfall over Mindoro and went outside the Philippines. Over the next few days, the storm progressed northeast over the East China Sea. The storm then impacted Hainan and later mainland China, dissipating thereafter on July 13. [5] The same day, a storm spawned east of Northern Samar. The storm drifted east, making landfall on the Philippines. On July 16, the storm turned north and continued over the following days. The storm dissipated on July 18. [6] The storm caused damages to Hong Kong and had a total of 20 fatalities. [7] On July 23, another storm spawned east of Samar Island. The storm moved northwest, making landfall on Luzon. The storm drifted north and dissipated on July 29, after making landfall over China. [8] The typhoon caused damage to a hospital and destroyed Camp Vicars in Mindanao. There were no casualties, but the storm caused three indirect fatalities after an attack just after the typhoon. [9] On July 31, a storm spawned in the South China Sea. The storm traversed northwest, where it made landfall over mainland China. The storm dissipated on August 3. [10]
On August 4, a storm spawned east of Taiwan. The storm traversed west over the following days until August 7, where the storm curved west. The storm drifted north over the following days, dissipating on August 9. [11] On August 19, a storm formed east of Hainan. The storm drifted west, where it made landfall on Hainan, and dissipated shortly after on August 21. [12] On August 29, a storm formed east of Taiwan. The storm drifted north, where it dissipated on September 1. [13]
On September 1, a storm formed south of the Spratly Islands. The storm drifted northwest, where it dissipated on September 3. [14] On September 5, a storm spawned east of Taiwan, then progressed northward. The it dissipated the next day east of the Amami Islands. [15] On September 20, a storm spawned east of Luzon. It traversed east, making landfall on Luzon. The storm dissipated in Vietnam on September 25. [16] On September 26, a typhoon spawned east of Okinawa Island. The storm progressed northwest, then dissipated. [17] The same day, a storm spawned south of Taiwan. Over the following hours, the storm progressed northeast, then dissipated the following day. [18]
On October 1, a typhoon hit Japan, causing damage to some parts of Japan. In the Odawara region, eight people were killed, while 50 houses were completely destroyed. The Yumoto-Kodzu-Odawara line was completely damaged. [19] The typhoon killed 600 people in the village of Koyawata, while a similar amount was killed in Kohachimara. The typhoon affected the battleship Shikishima, where the ship was unanchored and dragged ashore. Another ship (the Aoi Maru) towed four other vessels, with the captain and the chief engineer drowning. [20] The typhoon affected Yokohama, with shipping disruptions noted. [21] On October 5, a storm spawned near the east of Okinawa Island, progressing northward over the following days. It dissipated thereafter. [22]
On November 7, a storm formed east of the Philippines. The storm traversed east before directly making landfall on the Philippines. The storm followed the South China Sea before dissipating on November 11. [23] The same day, it hit a vessel where United States Army General Adna Chaffee was present in. [24]
The 1959 Pacific typhoon season was regarded as one of the most devastating years for Pacific typhoons on record, with China, Japan and South Korea sustaining catastrophic losses. It was an event in the annual cycle of tropical cyclone formation. The season had no official bounds, but tropical cyclones in the Western Pacific Ocean normally develop between May and October.
The 1966 Pacific typhoon season was an active season, with many tropical cyclones having severe impacts in China, Japan, and the Philippines. Overall, there were 49 tropical depressions declared officially or unofficially, of which 30 officially became named storms; of those, 20 reached typhoon status, while 3 further became super typhoons by having winds of at least 240 km/h (150 mph). Throughout the year, storms were responsible for at least 997 fatalities and $377.6 million in damage; however, a complete record of their effects is unavailable.
The 1953 Pacific typhoon season has no official bounds; it ran year-round in 1953, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean.
The 1990–91 South-West Indian Ocean cyclone season was fairly quiet, although activity began early and the final named storm formed at a record late date. There were seven named storms classified by the Météo-France office (MFR) on Réunion, as well as three depressions; an additional depression was classified by the Joint Typhoon Warning Center (JTWC), an unofficial warning agency. The JTWC tracked storms in both September and October, although neither affected land. In late November, another short-lived depression formed in the northeastern portion of the basin. Activity remained minimal until January, when Tropical Storm Alison formed in the eastern portion of the basin. Later in the month, Cyclone Bella became the strongest storm of the season, reaching 10‑minute maximum sustained winds of 155 km/h (96 mph). It passed near the island of Rodrigues, becoming the worst cyclone there in 20 years and killing half of the population of one endangered species. Bella also likely caused a cargo ship to go missing with 36 people on board. Three storms developed in short succession in the second half of February. Cyclone Cynthia developed rapidly in the Mozambique Channel on February 16 and struck western Madagascar, killing 36 people and ruining local rice harvests. A residual trough after Cynthia dissipated spawned Tropical Storm Debra, which looped in the Mozambique Channel. Toward the end of the month, Tropical Storm Elma exited the basin into the adjacent Australian region, only to re-enter the south-west Indian Ocean and dissipate. Long-lived Cyclone Fatima originated in the Australian basin in late March and changed directions before becoming extratropical. On April 2, a tropical depression struck eastern Madagascar, killing 18 people. The final storm, Gritelle, was named on June 10, the latest on record.
The 1991–92 South-West Indian Ocean cyclone season was an average cyclone season in which most storms remained over open waters. At the time, the season's official bounds lasted from November 15, 1991, to April 30, 1992, although this season began early when three tropical depressions formed before the official start. The second, designated Tropical Depression A2 by the Météo-France office (MFR) on Réunion, passed north of Madagascar on October 16 before weakening.
The 1992–93 South-West Indian Ocean cyclone season lasted longer than normal, with the first storm Aviona forming on September 27 and the final storm Konita not dissipating until May 7. It was an above-average season, with four tropical cyclones – the equivalent of a minimal hurricane – along with six tropical storms, one subtropical depression, and several depressions including one that was named. The basin is defined as the area west of 90°E and south of the Equator in the Indian Ocean, which includes the waters around Madagascar westward to the east coast of Africa. Tropical cyclones in this basin are monitored by the Regional Specialised Meteorological Centre in Réunion (MFR), as well as by the Joint Typhoon Warning Center (JTWC).
The 1993–94 South-West Indian Ocean cyclone season was the most active season in the basin since the start of reliable satellite coverage in 1967, until the record was surpassed 25 years later in the 2018–19 South-West Indian Ocean cyclone season. Activity lasted from mid-November, when Moderate Tropical Storm Alexina formed, until mid-April, when Tropical Cyclone Odille became extratropical. Four tropical cyclones – Daisy, Geralda, Litanne, and Nadia – struck eastern Madagascar, of which Geralda was the costliest and deadliest. With gusts as strong as 350 km/h (215 mph) accompanied by heavy rainfall, Geralda destroyed more than 40,000 homes and left 356,000 people homeless. Geralda killed 231 people and caused more than $10 million in damage. Cyclone Nadia was the second deadliest cyclone, having killed 12 people in northern Madagascar and later severely damaging portions of northeastern Mozambique, killing about 240 people and leaving $20 million in damage in the latter country. In February, Cyclone Hollanda struck Mauritius near peak intensity, causing $135 million in damage and two deaths.
The 1994–95 South-West Indian Ocean cyclone season was fairly active, with storms forming regularly from October through April. It was much less damaging than its predecessor, and most of the storms in the season remained over water or only brushed land. The first system was Tropical Depression A1, which formed in October and passed north of Madagascar. The first named storm was Albertine, which formed on November 23 in the northeastern portion of the basin and became one of three intense tropical cyclones. The last storm was Marlene, which was also an intense tropical cyclone and dissipated on April 11.
The 1940 Pacific typhoon season marked an interruption in meteorological records in both the Philippines and Hong Kong due to the start of World War II. There were 43 reported tropical cyclones, including 27 that attained typhoon status. The first storm was observed in February, and the first typhoon formed two months later, killing three people along Mindanao. Several storms formed in June and July, including reports of a typhoon in the newspapers that killed 52 in South Korea, and another typhoon reported in newspapers that killed one person on Samar after dropping heavy rainfall. The strongest typhoon of the season originated in July and attained a minimum pressure of 927 mbar (27.4 inHg), as reported by a ship northeast of the Philippines.
In 1900, 23 tropical cyclones were observed in the western Pacific Ocean, north of the equator and west of the International Date Line. In that region of the world, cyclones that attain maximum sustained winds of at least 118 km/h (73 mph) are known as typhoons. Of the 23 storms, 13 were tracked by the Hong Kong Observatory. Activity occurred from January to December, although the majority of the storms formed from June to November.
In 1901, 21 tropical cyclones were observed in the western Pacific Ocean, north of the equator. In that region of the world, cyclones that attain maximum sustained winds of at least 118 km/h (73 mph) are known as typhoons. Out of the 21 storms, the Hong Kong Observatory tracked nine of them. The strongest storm, known as the De Witte typhoon, reached a minimum barometric pressure of 920 mbar (27 inHg), before striking eastern China.
In 1927, there were 27 tropical cyclones observed in the western Pacific Ocean, north of the equator and west of the 180th meridian. Many of these storms affected the Philippines, China, and Japan, collectively leaving 15,952 fatalities. The strongest storm of the year also had the lowest barometric pressure recorded in a tropical cyclone worldwide at the time. On August 18, the Dutch steamship Sapoeroea recorded a barometric pressure of 886.7 millibar about 740 kilometres (460 miles) east of Luzon. This typhoon later struck near Hong Kong, where it halted transportation, wrecked buildings, and killed 15 people.
The 1943 Pacific typhoon season has no official bounds; it ran year-round in 1943, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. The scope of this article is limited to the Pacific Ocean, north of the equator and west of the International Date Line. Storms that form east of the date line and north of the equator are called hurricanes; see 1943 Pacific hurricane season.
The 1944 Pacific typhoon season has no official bounds; it ran year-round in 1944, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. The scope of this article is limited to the Pacific Ocean, north of the equator and west of the International Date Line. Storms that form east of the date line and north of the equator are called hurricanes; see 1944 Pacific hurricane season.
There were 30 tropical cyclones in the western Pacific Ocean in 1931, including 19 typhoons, as well as one that developed in December of the previous year. The most significant typhoon was one that struck eastern China near Shanghai in the midst of the country's worst floods on record; heavy rainfall caused levees to collapse along the Grand Canal, killing an estimated 300,000 people, including about 2,000 people overnight in the city of Gaoyou.
The following is a list of Pacific typhoon seasons from 1920 to 1935. Data from these years was extremely unreliable, so there were many more typhoons that did not hit land and were not detected by ships. The average from these times was 23 tropical storms, which now would be considered a well-below-average season.
This article encompasses the 1890s Pacific typhoon seasons.
In 1935, there were 24 tropical cyclones across the western part of the Pacific Ocean.