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Typhoon Fran (1955)
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. Storms that form east of the date line and north of the equator are called hurricanes; see 1955 Pacific hurricane season. Tropical Storms formed in the entire west Pacific basin were assigned a name by the Fleet Weather Center on Guam. Systems ImageSize = width:1002 height ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 coast of the peninsula runs the Kuril–Kamchatka Trench. The Kamchatka Peninsula, the Commander Islands, and Karaginsky Island constitute Kamchatka Krai of the Russian Federation. The majority of the 322,079 inhabitants are ethnic Russians, with about 13,000 being Koryaks (2014). More than half of the population lives in Petropavlovsk-Kamchatsky (179,526 in 2010) and nearby Yelizovo (38,980). The Kamchatka Peninsula contains the volcanoes of Kamchatka, a UNESCO World Heritage Site, that form part of the Ring of Fire. Geography Politically, the peninsula forms part of Kamchatka Krai. The southern tip is called Cape Lopatka. (Lopatka is Russian for spade.) The circular bay to the north of this on the Pacific side is Ava ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
1954–55 South-West Indian Ocean Cyclone Season
The following is a list of South-West Indian Ocean tropical cyclones in the 1950s decade, before the 1959–60 season. Storms February 1950 Mozambique Channel cyclone A cyclone was first observed northeast of Madagascar on February 9. The storm moved west-southwestwards, crossing northern Madagascar on February 13. The storm moved across the Mozambique Channel and struck eastern Mozambique on February 15. The circulation moved inland across much of Africa, eventually reaching northern Namibia (then known as South-West Africa). April 1952 Tanzania cyclone On April 13, 1952, a tropical cyclone was first observed north of the Comoros. The cyclone moved west-southwestwards towards the coast of Africa at a low latitude. On April 15, the ship ''M.V. Tayari'' encountered the eye of the cyclone and observed a minimum pressure of . Later that day, the cyclone moved ashore in southeastern Tanzania near Lindi, where maximum sustained winds were estimated at ; this ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
1955–56 South Pacific Cyclone Season
The following is a list of all reported tropical cyclones within the South Pacific Ocean to the east of 160°E during the 1950s decade. __TOC__ Systems 1949–50 *January 22 – 27, 1950 – A possible tropical cyclone existed to the north of New Caledonia. *January 29 – February 6, 1950 – A tropical cyclone developed in between the Northern and Southern Cook Islands and passed to the south of the Samoan Islands. Moving westwards the system passed within of Niuatoputapu during January 31, before it passed near Niuafoou during February 1. The system then moved south-westwards through the Lau Islands during February 2, where it caused gale-force winds but no significant damage. *February 20 – March 1, 1950 – During February 25, a tropical cyclone moved westwards through the Lau Islands and between Fiji's main islands of Viti Levu and Vanua Levu. The system subsequently turned south-southeastwards during the following day, while its movement sl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
1954–55 Australian Region Cyclone Season
The following is a list of all reported tropical cyclones within the Australian region between 90°E and 160°E in the 1950s. 1950–51 *December 10–11, 1950 – A tropical cyclone passed overland to the west of Groote Eylandt, where hurricane-force winds generated a storm surge. *January 10–24, 1951 – During January 10, a tropical cyclone moved into the Gulf of Carpentria near Karumba. The system subsequently moved around the Gulf of Carpertaria, before it made landfall on Queensland near Karumba during January 22. *January 25, 1951 – A tropical cyclone became slow moving near Fraser Island. *February 20–28, 1951 – A tropical cyclone impacted the Solomon Islands, Vanuatu and New Caledonia. *March 15, 1951 – A tropical cyclone made landfall on Queensland near Maryborough. *March 24 – April 2, 1951 – A tropical cyclone impacted the Solomon Islands. 1951–52 *January 19–20, 1952 – A tropical cyclone made landfall ne ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 form between April and December, peaks in May and November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. Below are the most significant cyclones in the time period. Because much of the North Indian coastline is near sea level and prone to flooding, these cyclones can easily kill many with storm surge and flooding. These cyclones are among the deadliest on earth in terms of numbers killed. At the time, only one RSMC, the India Meteorological Department (IMD), monitored the basin. However, in 1959, the Joint Typhoon Warning Center (JTWC) was founded, resulting in it releasing unofficial advisories for the basin. 1950 season *April 8–13, 1950 – A deep depress ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 active season in terms of accumulated cyclone energy (ACE), but only slightly above average in terms of storm formation, with 13 recorded tropical cyclones. The first reported system of the year, January's Hurricane Alice, was later found to have formed on December 30, during the 1954 season. Alice caused relatively minor impact as it tracked through the Lesser Antilles and eastern Caribbean Sea. The first tropical cyclone to form in 1955, Tropical Storm Brenda, caused two deaths and minor damage along the Gulf Coast of the United States in early August. The quick succession of Hurricanes Connie and Diane caused significant flooding in the Northeastern United States, with nearly $1 billion (1955 USD, $11.05 billion in 20 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Typhoon Louise (1955)
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. Storms that form east of the date line and north of the equator are called hurricanes; see 1955 Pacific hurricane season. Tropical Storms formed in the entire west Pacific basin were assigned a name by the Fleet Weather Center on Guam. Systems ImageSize = width:1002 heigh ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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–Simpson scale, Saffir–Simpson category 3 to 5. In such storms, some of the outer rainbands may strengthen and organize into a ring of thunderstorms—a new, outer Eye (cyclone), eyewall—that slowly moves inward and robs the original, inner eyewall of its needed moisture and angular momentum. Since the strongest winds are in a tropical cyclone's Eye (cyclone), eyewall, the storm usually weakens during this phase, as the inner wall is "choked" by the outer wall. Eventually the outer eyewall replaces the inner one completely, and the storm may re-intensify. The discovery of this process was partially responsible for the end of the U.S. government's hurricane modification experiment Project Stormfury. This project set out to cloud seeding, seed ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 surface. Sea surface temperatures greatly modify air masses in the Atmosphere of Earth, Earth's atmosphere within a short distance of the shore. The thermohaline circulation has a major impact on average sea surface temperature throughout most of the world's oceans. Warm sea surface temperatures can develop and Tropical cyclogenesis, strengthen cyclones over the ocean. Tropical cyclones can also cause a cool wake. This is due to turbulent mixing of the upper of the ocean. Sea surface temperature changes during the day. This is like the air above it, but to a lesser degree. There is less variation in sea surface temperature on breezy days than on calm days. Coastal sea surface temperatures can cause offshore winds to generate upwelling ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
