Typhoon Clara (1955)
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The 1955 Pacific typhoon season has no official bounds; it ran year-round in 1955, 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 season produced a large number of tropical storms but most of them were weak, and sources from American typhoon warning agencies often grossly overestimated the maximum wind speed of many systems which could not properly match with their respective central pressure observations. The scope of this article is limited to the Pacific Ocean, north of the equator and west of the
International Date Line The International Date Line (IDL) is the line extending between the South and North Poles that is the boundary between one calendar day and the next. It passes through the Pacific Ocean, roughly following the 180.0° line of longitude and de ...
. Storms that form east of the date line and north of the equator are called hurricanes; see
1955 Pacific hurricane season The 1955 Pacific hurricane seasons began on May 15, 1955, in the northeast Pacific Ocean and on June 1, 1955, in the central Pacific. They ended on November 30, 1955. These dates conventionally delimit the time of year when most tropical cyclones ...
. Tropical Storms formed in the entire west Pacific basin were assigned a name by the Fleet Weather Center on
Guam Guam ( ; ) is an island that is an Territories of the United States, organized, unincorporated territory of the United States in the Micronesia subregion of the western Pacific Ocean. Guam's capital is Hagåtña, Guam, Hagåtña, and the most ...
.


Systems

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The rest of the storms, such as unnumbered and unnamed tropical depressions and storms, are only classified by the CMA while the JMA is sometimes rare before the 1960s - 1970s.


Typhoon Violet

Typhoon Violet formed on January 1 and dissipated on January 6. It peaked as a Category 1 typhoon by the JTWC before making landfall in Mindinao in the Philippines.


JMA Tropical Storm Two


Typhoon Wilda

Forming in an area full of islands, Wilda moved up into the open ocean where it reached typhoon strength. Shortly after, Wilda peaked in intensity as a lower-end category 2 cyclone. Wilda soon made a turn and began to weaken. Soon enough, Wilda had weakened under typhoon strength and dissipated on March 29.


Typhoon Anita

Anita formed as a tropical depression on April 17. Anita entered a phase of warm waters, and it rapidly intensified to a category 1 typhoon and even a category 2 typhoon later. Anita encountered on a phase of cool waters, and as a result, it gradually weakened. Anita but re-intensified into a category 1 typhoon on April 20. However, it weakened again on April 22 but again re-intensified to a category 1 and even a category 2 typhoon later. Anita reached its peak intensity as a category 3 typhoon. Anita encountered a strong wind shear and because of this, Anita rapidly weakened to a tropical storm. Anita weakened to a tropical depression on April 25. Later, Anita loses its identity and dissipated.


Typhoon Billie

Billie hit China as a weak typhoon.


JMA Tropical Storm Six


Typhoon Clara

a tropical disturbance formed near Guam and turn tropical storm Clara. It slowly intensify to a category 4 and it made landfall on the Japanese islands as a category 4. It continue going to northeast China and dissipated in mainland China.


Tropical Storm Dot


Typhoon Ellen


Tropical Storm 09W


Typhoon Fran

On July 18, a tropical depression formed southeast of Japan. It entered a phase of favorable environments and was soon upgraded into a tropical storm and named Fran. Fran then moved into a favorable environment and Fran was upgraded into a category 1 typhoon. Intensification occurred and Fran intensified from a category 1 to 4 typhoon and reached its peak intensity. After peaking in intensity, unfavorable environments made Fran to start a weakening trend. On July 20, Fran weakened to a category 2 typhoon and later weakened to a category 1 typhoon and even as a strong tropical storm. On July 21 of noon, Fran weakened to a tropical depression, and soon encountered with strong wind shear and dissipated. Fran became extratropical on July 21, before moving further to the east and dissipated on July 23.


JMA Tropical Storm Twelve


Typhoon Georgia


JMA Tropical Storm Fifteen


Typhoon Hope

A tropical depression formed east of
Philippines The Philippines, officially the Republic of the Philippines, is an Archipelagic state, archipelagic country in Southeast Asia. Located in the western Pacific Ocean, it consists of List of islands of the Philippines, 7,641 islands, with a tot ...
on August 2. It intensified to a tropical storm in the next day and named Hope. Hope intensified into a category 1 hurricane while at the south of
Japan Japan is an island country in East Asia. Located in the Pacific Ocean off the northeast coast of the Asia, Asian mainland, it is bordered on the west by the Sea of Japan and extends from the Sea of Okhotsk in the north to the East China Sea ...
. It weakened to a tropical storm and the storm turned to the north and intensified into a category 1 again. It was downgraded to a tropical storm and turned northeast before it slowed down. Hope became
extratropical Extratropical cyclones, sometimes called mid-latitude cyclones or wave cyclones, are low-pressure areas which, along with the anticyclones of high-pressure areas, drive the weather over much of the Earth. Extratropical cyclones are capable of p ...
on August 17. Shortly after, the remnants hit the south of
Kamchatka Peninsula The Kamchatka Peninsula (, ) is a peninsula in the Russian Far East, with an area of about . The Pacific Ocean and the Sea of Okhotsk make up the peninsula's eastern and western coastlines, respectively. Immediately offshore along the Pacific ...
and dissipated.


JMA Tropical Storm Sixteen


JMA Tropical Storm Seventeen

Seventeen was a short tropical storm that never affected land.


JMA Tropical Storm Eighteen

This storm never affected land, it remained in open waters.


Typhoon Iris


Typhoon Joan


Typhoon Kate


Typhoon Louise

Louise formed on September 20 as a weak tropical depression. It intensified into a tropical storm and even a typhoon later. Wind shear quickly decreased and
sea surface temperature Sea surface temperature (or ocean surface temperature) is the ocean temperature, temperature of ocean water close to the surface. The exact meaning of ''surface'' varies in the literature and in practice. It is usually between and below the sea ...
s began to rise and Louise rapidly intensified into a category 5 super typhoon. However, the process of eyewall replacement cycle caused Louise to weaken. Louise weakened to a category 2 typhoon and it started to affect the Kyūshū island of
Japan Japan is an island country in East Asia. Located in the Pacific Ocean off the northeast coast of the Asia, Asian mainland, it is bordered on the west by the Sea of Japan and extends from the Sea of Okhotsk in the north to the East China Sea ...
and even weakened to a category 1 typhoon and affected
Japan Japan is an island country in East Asia. Located in the Pacific Ocean off the northeast coast of the Asia, Asian mainland, it is bordered on the west by the Sea of Japan and extends from the Sea of Okhotsk in the north to the East China Sea ...
. Louise dissipated on September 30. On Kyūshū island, 54 people were killed and 14 went missing.


Typhoon Marge


JMA Tropical Storm Twenty-four


Tropical Storm 17W


Typhoon Nora


Typhoon Opal


Tropical Storm 20W


Typhoon Patsy

Patsy started on its life as a tropical depression on November 25. It hit Philippines as a tropical storm. It moved out of area before intensifying into Typhoon Patsy. Patsy reached its peak intensity before undergoing an
eyewall replacement cycle In meteorology, eyewall replacement cycles, also called concentric eyewall cycles, naturally occur in intense tropical cyclones with maximum sustained winds greater than , or hurricane-force, and particularly in major hurricanes of Saffir–Simps ...
and started to weaken.


Typhoon Ruth

Typhoon Ruth was among one of the strongest storms on record reaching 180 kts (205 mph) sustained winds measured by a reconnaissance aircraft. However, it was later determined that measurements and estimates from the 1940s to 1960s were erroneous. Thus, Ruth's measurement may likely be lower than the official best-track values.


Storm names

The following names listed here are names of the 1955 Pacific Typhoon Season.


See also

*
1955 Pacific hurricane season The 1955 Pacific hurricane seasons began on May 15, 1955, in the northeast Pacific Ocean and on June 1, 1955, in the central Pacific. They ended on November 30, 1955. These dates conventionally delimit the time of year when most tropical cyclones ...
*
1955 Atlantic hurricane season The 1955 Atlantic hurricane season was, at the time, the costliest season ever recorded, just ahead of the previous year. The hurricane season officially began on June 15, 1955, and ended on November 15, 1955. It was an extremely activ ...
*
1955 North Indian Ocean cyclone season The years between 1950 and 1959 featured the 1950s North Indian Ocean cyclone seasons. Each season was an ongoing event in the annual cycle of tropical cyclone formation. The North Indian tropical cyclone season has no bounds, but they tend to for ...
* Australian region cyclone seasons: 1954–55 1955–56 * South Pacific cyclone seasons: 1954–55 1955–56 * South-West Indian Ocean cyclone seasons: 1954–55 1955–56 {{Tropical cyclone season, 1955