1950s North Indian Ocean cyclone seasons

1950s North Indian Ocean cyclone seasons
1950s North Indian Ocean cyclone seasons
Seasonal boundaries
First system formed	April 8, 1950
Last system dissipated	1960
Seasonal statistics
Depressions	71
Total fatalities	12,500+
Total damage	Unknown
	North Indian Ocean tropical cyclone seasons ; 1930s, 1940s, 1950s, 1960, 1961

Last updated January 22, 2024

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 depression existed over the Bay of Bengal.^[1]
May 23–30, 1950 – A deep depression existed over the Bay of Bengal.^[1]
June 8–12, 1950 – A cyclonic storm existed over the Bay of Bengal.^[1]
June 23–28, 1950 – A depression existed over the Bay of Bengal.^[1]
July 10–12, 1950 – A depression existed over the Bay of Bengal.^[1]
July 11–15, 1950 – A depression existed over land.^[1]
July 25–30, 1950 – A depression existed over the Bay of Bengal.^[1]
August 3–7, 1950 – A depression existed over land.^[1]
August 9–15, 1950 – A depression existed over the Bay of Bengal.^[1]
September 1–5, 1950 – A depression existed over land.^[1]
September 9–11, 1950 – A depression existed over the Bay of Bengal.^[1]
September 12–19, 1950 – A cyclonic storm existed over the Bay of Bengal.^[1]
September 22–24, 1950 – A depression existed over the Bay of Bengal.^[1]
October 17–22, 1950 – A depression existed over the Bay of Bengal.^[1]
November 16–20, 1950 – A cyclonic storm existed over the Bay of Bengal.^[1]
December 2–6, 1950 – A cyclonic storm existed over the Bay of Bengal.^[1]

1951 season

April 15–24, 1951 – A cyclonic storm existed over the Arabian Sea.^[2]
June 4–7, 1951 – A depression existed over the Bay of Bengal.^[2]
June 11–13, 1951 – A depression existed over the Arabian Sea.^[2]
June 26 – July 7, 1951 – A depression existed over the Bay of Bengal.^[2]
July 19–22, 1951 – A depression existed over the Bay of Bengal.^[2]
July 24–29, 1951 – A cyclonic storm existed over the Bay of Bengal.^[2]
July 30 – August 1, 1951 – A depression existed over the Bay of Bengal.^[2]
August 4–5, 1951 – A depression existed over the Bay of Bengal.^[2]
August 16–19, 1951 – A depression existed over the Bay of Bengal.^[2]
August 30 – September 1, 1951 – A depression existed over the Bay of Bengal.^[2]
September 9–13, 1951 – A depression existed over Land.^[2]
October 9–11, 1951 – A depression existed over the Bay of Bengal.^[2]
November 12–19, 1951 – A severe cyclonic storm existed over the Arabian Sea.^[2]
November 23–26, 1951 – A depression existed over the Bay of Bengal.^[2]
December 5–14, 1951 – A severe cyclonic storm existed over the Bay of Bengal.^[2]

1952 season

Typhoon Vae crossed over into the Indian Ocean in 1952.

1953 season

1954 season

1955 season

1956 season

June 1956 India cyclone

This cyclone brought torrential rainfall to Midnapore district in West Bengal. About 20,000 people were left homeless, while another 20,000 people were left stranded near the Assam border after the Haora River topped its banks. There was an estimated 480 fatalities, most caused by landslides.^[3]

1957 season

December 1957 cyclone

A cyclone developed over the Arabian Sea near the Gulf of Oman on December 27. Moving westward, the storm lashed Bahrain with winds of 110 mph (180 km/h). An offshore oil rig collapsed, killing 20 Royal Dutch Shell employees.^[3]

1958 season

A cyclonic storm lasted from October 21–24 and struck Bangladesh (then East Pakistan), causing 12,000 deaths.^[4]

1959 season

February 1959 Bahrain cyclone

A tropical cyclone impacted Bahrain and caused 500 deaths.^[3]

May 1959 Salalah cyclone

This system first became a low-pressure area near the Laccadive Islands on May 19, tracking northwest towards the Arabian peninsula. The system made landfall at Raysut on May 24. At Salalah, skies clouded over on May 23 as the pressure fell significantly. Winds turned northerly before midnight that night. At 1 a.m. on May 24 the peak of the storm's winds arrived. Maximum sustained winds were estimated at 70 knots (130 km/h) and the pressure at Salalaha fell to 968 millibars (28.6 inHg). Many vessels offshore, including two large passenger ships, went to pieces. Five buildings collapsed and several roofs were blown away by the cyclone. Salalah recorded 82 millimetres (3.2 in) of rain at their airport. A total of 141 lives from the ship Samha were taken during this tempest.^[5]

Related Research Articles

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The 1964 North Indian Ocean cyclone season had no bounds, but cyclones tend to form between April and December, with peaks in May and November. The season has no official bounds but cyclones tend to form between April and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. There are two main seas in the North Indian Ocean—the Bay of Bengal to the east of the Indian subcontinent and the Arabian Sea to the west of India. The official Regional Specialized Meteorological Centre in this basin is the India Meteorological Department (IMD), while the Joint Typhoon Warning Center releases unofficial advisories. An average of four to six storms form in the North Indian Ocean every season with peaks in May and November. Cyclones occurring between the meridians 45°E and 100°E are included in the season by the IMD.

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The 1950 North Indian Ocean cyclone season was part of the annual cycle of tropical cyclone formation. The season has no official bounds but cyclones tend to form between April and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. There are two main seas in the North Indian Ocean—the Bay of Bengal to the east of the Indian subcontinent and the Arabian Sea to the west of India. The official Regional Specialized Meteorological Centre in this basin is the India Meteorological Department (IMD), while the Joint Typhoon Warning Center (JTWC) releases unofficial advisories. An average of five tropical cyclones form in the North Indian Ocean every season with peaks in May and November. Cyclones occurring between the meridians 45°E and 100°E are included in the season by the IMD.

The 1951 North Indian Ocean cyclone season was part of the annual cycle of tropical cyclone formation. The season has no official bounds but cyclones tend to form between April and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. There are two main seas in the North Indian Ocean—the Bay of Bengal to the east of the Indian subcontinent and the Arabian Sea to the west of India. The official Regional Specialized Meteorological Centre in this basin is the India Meteorological Department (IMD), while the Joint Typhoon Warning Center (JTWC) releases unofficial advisories. An average of five tropical cyclones form in the North Indian Ocean every season with peaks in May and November. Cyclones occurring between the meridians 45°E and 100°E are included in the season by the IMD.

The years between 1940 and 1949 featured the 1940s 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. On 27 April 1949, India Meteorological Department (IMD) became a member of the World Meteorological Organization after independence.

The following is a list of North Indian Ocean tropical cyclones from 1930 to 1939. Records from before the 1970s were extremely unreliable, and storms that stayed at sea were often only reported by ship reports.

The following is a list of North Indian Ocean tropical cyclones from 1920 to 1929. Records from before the 1970s were extremely unreliable, and storms that stayed at sea were often only reported by ship reports.

References

1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 India Weather Review Annual Summary Part C Storms and Depressions 1950 (PDF) (Report). India Meteorological Department. 1951. pp. 1–12. Retrieved June 24, 2020.
1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 India Weather Review Annual Summary Part C Storms and Depressions 1951 (PDF) (Report). India Meteorological Department. 1952. pp. 1–12. Retrieved June 24, 2020.
1 2 3 David Longshore (May 12, 2010). Encyclopedia of Hurricanes, Typhoons, and Cyclones. Infobase Publishing. pp. 113, 258. ISBN 978-1438118796 . Retrieved February 26, 2016.
↑ Damen, Michiel. "Cyclone Hazard in Bangladesh".
↑ David Membery (July 2002). "Monsoon Tropical Cyclones: Part 2". Weather. Royal Meteorological Society. 57 (7): 247–255. Bibcode:2002Wthr...57..246M. doi: 10.1256/004316502760195911 .

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[1950_AR-1] 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 India Weather Review Annual Summary Part C Storms and Depressions 1950 (PDF) (Report). India Meteorological Department. 1951. pp. 1–12. Retrieved June 24, 2020.

[1951_AR-2] 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 India Weather Review Annual Summary Part C Storms and Depressions 1951 (PDF) (Report). India Meteorological Department. 1952. pp. 1–12. Retrieved June 24, 2020.

[longshore-3] 1 2 3 David Longshore (May 12, 2010). Encyclopedia of Hurricanes, Typhoons, and Cyclones. Infobase Publishing. pp. 113, 258. ISBN 978-1438118796 . Retrieved February 26, 2016.

[4] Damen, Michiel. "Cyclone Hazard in Bangladesh".

[5] David Membery (July 2002). "Monsoon Tropical Cyclones: Part 2". Weather. Royal Meteorological Society. 57 (7): 247–255. Bibcode:2002Wthr...57..246M. doi: 10.1256/004316502760195911 .

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