1950 North Indian Ocean cyclone season explained

Basin:NIO
Year:1950
Track:1950 North Indian Ocean cyclone season summary.png
First Storm Formed:April 8, 1950
Last Storm Dissipated:December 6, 1950
Average Wind Speed:3
Total Disturbances:16
Total Depressions:9
Total Storms:4
Five Seasons:1948, 1949, 1950, 1951, 1952
Atlantic Season:1950 Atlantic hurricane season
East Pacific Season:1950 Pacific hurricane season
West Pacific Season:1950 Pacific typhoon season

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.[1] Cyclones occurring between the meridians 45°E and 100°E are included in the season by the IMD.[2]

Sixteen depressions developed during the 1950 season, with four of them becoming cyclonic storms while three of them formed over the land. Most tropical cyclones formed in this season are weak, as there is no severe cyclonic storms formed during this season.[3]

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Season summary

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TextData = pos:(670,25) text:"(From the " pos:(717,25) text:"IMD tropical cyclone intensity scale)"

Systems

Deep Depression One

Basin:NIO
Track:01B 1950 track.png
Formed:April 8
Dissipated:April 13
Type:deepdepression

A ship reported thunderstorm rains in the southeast of Sri Lanka in April 4 while a shallow low was formed in the southeast Bay of Bengal on the next day, when Car Nicobar experienced overcast conditions and northeasterly winds. The low moved west and a well-marked trough formed southeast of Sri Lanka in the morning of April 7. By April 8, the trough developed into depression as winds of 15 to 20 knots are reported by number of vessels, and a vessel reported southerly winds The depression tracked north and then tracking northeast by April 10. By April 11, the system intensified and begins to accelerate towards Burma on evening of the same day.[4] In April 13, the system moved ashore across southern Rakhine State coasts and quickly dissipated over land.[5]

The system dropped heavy rains on the east coast of Sri Lanka on April 8 and April 9. As the depression moved northeastwards, widespread rains occurred over Napier Bay Islands on April 11 and April 13, killing two people in Port Blair. As system made landfall near Burmese coast, heavy rains caused some damage to the property and five people.[5]

Deep Depression Two

Basin:NIO
Track:02B 1950 track.png
Formed:May 23
Dissipated:May 30
Pressure:998
Type:deepdepression

Cyclonic Storm Three

Basin:NIO
Formed:June 8
Dissipated:June 12
Track:03B 1950 track.png
3-Min Winds:45

Depression Four

Basin:NIO
Formed:June 23
Dissipated:June 28
Track:04B 1950 track.png
Type:niodepression

Depression Five

Basin:NIO
Formed:July 10
Dissipated:July 12
Track:06B 1950 track.png
Type:niodepression

Land Depression Six

Basin:NIO
Formed:July 11
Dissipated:July 15
Track:05B 1950 track.png
Type:niodepression

Depression Seven

Basin:NIO
Formed:July 25
Dissipated:July 30
Track:07B 1950 track.png
Type:niodepression

Land Depression Eight

Basin:NIO
Formed:August 3
Dissipated:August 7
Track:08B 1950 track.png
Type:niodepression

Depression Nine

Basin:NIO
Formed:August 9
Dissipated:August 15
Track:09B 1950 track.png
Type:niodepression

Land Depression Ten

Basin:NIO
Formed:September 1
Dissipated:September 5
Track:12B 1950 track.png
Type:niodepression

Depression Eleven

Basin:NIO
Formed:September 9
Dissipated:September 11
Track:10B 1950 track.png
Type:niodepression

Cyclonic Storm Twelve

Basin:NIO
Formed:September 12
Dissipated:September 19
Track:13B 1950 track.png
3-Min Winds:40

Depression Thirteen

Basin:NIO
Formed:September 22
Dissipated:September 24
Track:11B 1950 track.png
Type:niodepression

Depression Fourteen

Basin:NIO
Formed:October 17
Dissipated:October 22
Track:14B 1950 track.png
Type:niodepression

Cyclonic Storm Fifteen

Basin:NIO
Formed:November 16
Dissipated:November 20
Track:15B 1950 track.png
3-Min Winds:45

Cyclonic Storm Sixteen

Basin:NIO
Formed:December 2
Dissipated:December 6
Track:16B 1950 track.png
3-Min Winds:50
Pressure:1000

See also

External links

Notes and References

  1. Web site: India Meteorological Department . 2012 . June 8, 2012 . Frequently Asked Questions: What is the annual frequency of Cyclones over the Indian Seas? What is its intra-annual variation? . dead . https://web.archive.org/web/20150521044203/http://www.imd.gov.in/section/nhac/dynamic/faq/FAQP.htm . May 21, 2015 .
  2. Web site: India Meteorological Department. May 25, 2009. July 16, 2012. Bulletins Issued by Regional Specialized Meteorological Centre (RSMC) – Tropical Cyclones, New Delhi. https://web.archive.org/web/20120412152516/http://www.imd.gov.in/section/nhac/dynamic/bulletins.pdf. 2012-04-12. dead.
  3. Web site: Annual frequency of cyclonic disturbances (Maximum sustained windspeeds of 17 knots or more), Cyclones (34 knots or more) and Severe Cyclones (48 knots or more) over the Bay of Bengal (BOB), Arabian Sea (AS) and land surface of India. India Meteorological Department. Unattributed. 2010-08-31. 2011-08-20. https://web.archive.org/web/20110805212718/http://www.imd.gov.in/section/nhac/dynamic/ANNUAL_FREQ_CYCLONIC_DISTURBANCES.pdf. 2011-08-05. dead.
  4. Web site: 1950 Depression NOT_NAMED (1950098N05083) . IBTrACS . 2 August 2020.
  5. [ftp://ftp.library.noaa.gov/docs.lib/htdocs/rescue/cd020_pdf/00471F10.pdf India Weather Review Annual Summary Part C Storms and Depressions 1950]. India Meteorological Department. 1951. June 24, 2020. 1–12.