1963 North Indian Ocean cyclone season

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1963 North Indian Ocean cyclone season
1963 North Indian Ocean cyclone season summary map.png
Season summary map
Seasonal boundaries
First system formedJanuary 3, 1963
(record earliest)
Last system dissipatedDecember 7, 1963
Strongest storm
NameThree
  Maximum winds240 km/h (150 mph)
  Lowest pressure920 hPa (mbar)
Seasonal statistics
Depressions17
Deep depressions11
Cyclonic storms6
Very severe cyclonic storms4
Total fatalitiesAt least 11,735
Total damageUnknown
Related articles
North Indian Ocean tropical cyclone seasons
1961, 1962, 1963, 1964, 1965

The 1963 North Indian Ocean cyclone season had no bounds, but cyclones tend to form between April and December, with peaks in May and November. 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. [1] Cyclones occurring between the meridians 45°E and 100°E are included in the season by the IMD. [2]

Contents

Season Summary

1963 North Indian Ocean cyclone season

Systems

Deep Depression One

Deep depression (IMD)
Tropical depression (SSHWS)
Temporary cyclone north.svg   DeepDepression01-1963.png
DurationJanuary 3 – January 5
Peak intensity45 km/h (30 mph) (3-min);

This tropical depression stalled for three days. [3]

Extremely Severe Cyclonic Storm Two

Extremely severe cyclonic storm (IMD)
Category 1 tropical cyclone (SSHWS)
Cropped Tiros VI mosaic of Extremely Severe Cyclonic Storm (1963-05-24).png   ESCSTwo-1963.png
DurationMay 18 – May 29
Peak intensity195 km/h (120 mph) (3-min);
947  hPa  (mbar)

On May 19, a tropical disturbance formed over the Laccadive Islands, before tracking northwest towards the Arabian peninsula. The system achieved cyclone intensity on May 22. On May 24, a United States Weather Bureau reconnaissance aircraft flew into the 19 km (12 mi) eye of the storm, encountering winds of 193 km/h (120 mph). [4] A ship 111 kilometres (69 mi) west of the system reported winds of 68 knots (126 km/h). At Salalah, a strong northerly wind set in during the morning of May 25. Later in the day, winds increased to gale force and a sandstorm reduced visibility to 400 metres (1,300 ft). Later in the day of May 26 winds again increased to gale force and another sandstorm reduced visibility to 500 metres (1,600 ft). As winds increased to 60 knots (110 km/h) the sandstorm became more severe, with visibility restricted to 50 metres (160 ft). Late on the night of the 26th, winds shifted to northeast and heavy rains fell across the region through the morning hours. Skies remained cloudy with periods of rain into May 28. A total of 230 millimetres (9.1 in) was recorded at Salalah. [5] [6] An estimated 22,000 people were reported to have died, while a further 500,000 were left homeless. [7]

Super Cyclonic Storm Three

Super cyclonic storm (IMD)
Category 1 tropical cyclone (SSHWS)
Temporary cyclone north.svg   SCSThree-1963.png
DurationMay 25 – May 29
Peak intensity240 km/h (150 mph) (3-min);
920  hPa  (mbar)

One of the strongest cyclones ever recorded in the Northern Indian Ocean. Had the lowest known pressure in the basin until it was surpassed by the 1991 Bangladesh cyclone. [8] Killed 11,520 people in Bangladesh. [9]

Deep Depression Four

Deep depression (IMD)
Tropical depression (SSHWS)
Temporary cyclone north.svg   DeepDepressionFour-1963.png
DurationJune 6 – June 8
Peak intensity55 km/h (35 mph) (3-min);
991  hPa  (mbar)

Produced torrential rains over parts of eastern India, peaking at 910 mm (36 in) in Cherrapunji. [10]

Depression Five

Depression (IMD)
Tropical depression (SSHWS)
Temporary cyclone north.svg   Depression05-1963.png
DurationJune 24 – June 26
Peak intensity45 km/h (30 mph) (3-min);
999  hPa  (mbar)

This tropical depression moved from east to west. [11]

Depression Six

Depression (IMD)
Tropical depression (SSHWS)
Temporary cyclone north.svg   Depression06-1963.png
DurationJuly 4 – July 6
Peak intensity45 km/h (30 mph) (1-min);

This tropical depression moved from east to west. [12]

Depression Seven

Depression (IMD)
Tropical depression (SSHWS)
Temporary cyclone north.svg   Depression07-1963.png
DurationAugust 9 – August 14
Peak intensity45 km/h (30 mph) (3-min);
991  hPa  (mbar)

This tropical depression moved from east to west. [13]

Deep Depression Eight

Deep depression (IMD)
Tropical depression (SSHWS)
Temporary cyclone north.svg   Depression08-1963.png
DurationSeptember 7 – September 16
Peak intensity45 km/h (30 mph) (3-min);
990  hPa  (mbar)

Heavy rains from the storm triggered severe flooding that killed at least 200 people. [14] The storm moved from east to west.

Deep Depression Nine

Deep depression (IMD)
Tropical depression (SSHWS)
Temporary cyclone north.svg   DeepDepression09-1963.png
DurationSeptember 25 – September 28
Peak intensity55 km/h (35 mph) (3-min);
996  hPa  (mbar)

At least 15 people were killed by flooding triggered by the depression in Orissa. [15] The storm was formerly in the Western Pacific as an unnamed CMA tropical depression.

Depression Ten

Depression (IMD)
Tropical depression (SSHWS)
Temporary cyclone north.svg   Depression10-1963.png
DurationOctober 5 – October 7
Peak intensity55 km/h (35 mph) (3-min);
995  hPa  (mbar)

Some loss of life was reported in East Pakistan. [16]

Cyclonic Storm Eleven

Cyclonic storm (IMD)
Tropical storm (SSHWS)
Temporary cyclone north.svg   CS11-1963.png
DurationOctober 13 – October 17
Peak intensity75 km/h (45 mph) (3-min);
999  hPa  (mbar)

[17]

Very Severe Cyclonic Storm Twelve-Fourteen

Very severe cyclonic storm (IMD)
Category 1 tropical cyclone (SSHWS)
Temporary cyclone north.svg   VSCS12-14 1963.png
DurationOctober 19 – October 28
Peak intensity150 km/h (90 mph) (3-min);
984  hPa  (mbar)

Significant damage and flooding took place in India, with some loss of life reported. [18] The storm was classified under two different designations, but was reanalyzed to be one system. [19]

Depression Thirteen

Depression (IMD)
Tropical depression (SSHWS)
Temporary cyclone north.svg   Depression13-1963.png
DurationOctober 24 – October 26
Peak intensity55 km/h (35 mph) (3-min);

The storm moved from south to north. [20]

Depression Fifteen

Depression (IMD)
Temporary cyclone north.svg   Depression15-1963.png
DurationNovember 24 – November 25
Peak intensity45 km/h (30 mph) (3-min);

This tropical depression moved from south to north. [21]

Cyclonic Storm Sixteen

Cyclonic storm (IMD)
Tropical storm (SSHWS)
Temporary cyclone north.svg   CS16-1963.png
DurationNovember 29 – December 7
Peak intensity65 km/h (40 mph) (3-min);
1002  hPa  (mbar)

This cyclonic storm moved from east to west. [22]

Deep Depression Seventeen

Deep depression (IMD)
Tropical storm (SSHWS)
Temporary cyclone north.svg   DeepDepression17-1963.png
DurationNovember 30 – December 6
Peak intensity55 km/h (35 mph) (3-min);
1004  hPa  (mbar)

This storm moved from east to west. [23]

See also

Related Research Articles

<span class="mw-page-title-main">North Indian Ocean tropical cyclone</span>

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<span class="mw-page-title-main">1992 North Indian Ocean cyclone season</span>

The 1992 North Indian Ocean cyclone season was unofficially the most active year on record for the basin, with 10 tropical storms developing, according to the Joint Typhoon Warning Center (JTWC). 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 JTWC 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.

<span class="mw-page-title-main">2006 North Indian Ocean cyclone season</span> North Indian Ocean tropical cyclone season

The 2006 North Indian Ocean cyclone season had no bounds, but cyclones tend to form between April and December, with peaks in May and November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean.

<span class="mw-page-title-main">Cyclone Phyan</span>

Cyclonic Storm Phyan developed as a tropical disturbance to the southwest of Colombo in Sri Lanka on November 4, 2009. Over the next couple of days, the disturbance gradually developed before weakening as it made landfall on Southern India on November 7. After the disturbance emerged into the Arabian Sea, it rapidly became more of a concern to the India Meteorological Department (IMD) reporting early on November 9 that the disturbance had intensified into a Depression, and designated it as Depression ARB 03 whilst the Joint Typhoon Warning Center (JTWC) issued a Tropical Cyclone Formation Alert. Later that day, the JTWC designated the system as Cyclone 04A. During the next day, the Depression turned towards the northeast the IMD reported that it had intensified into a Cyclonic Storm and named it as Phyan.

<span class="mw-page-title-main">1960 North Indian Ocean cyclone season</span> Cyclone season in the North Indian ocean

The 1960 North Indian Ocean cyclone season featured two deadly tropical cyclones that killed approximately 20,000 people collectively in East Pakistan. The Indian subcontinent divides the North Indian Ocean into two areas: the Bay of Bengal to the east and the Arabian Sea to the west. The official Regional Specialized Meteorological Centre in this basin is the India Meteorological Department (IMD), while the Joint Typhoon Warning Center releases unofficial advisories. On average, five storms form in the North Indian Ocean every season with dual peaks in activity during May and November. Cyclones that occurred between 45°E and 100°E were included in seasonal records by the IMD.

<span class="mw-page-title-main">1961 North Indian Ocean cyclone season</span>

The 1961 North Indian Ocean cyclone season had no bounds, but cyclones tend to form between April and December, with peaks in May and November. 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.

<span class="mw-page-title-main">1962 North Indian Ocean cyclone season</span>

The 1962 North Indian Ocean cyclone season had 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. The IMD includes cyclones occurring between the meridians 45°E and 100°E in the season.

<span class="mw-page-title-main">1964 North Indian Ocean cyclone season</span>

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.

<span class="mw-page-title-main">2014 North Indian Ocean cyclone season</span> North Indian Ocean tropical cyclone season

The 2014 North Indian Ocean cyclone season was an event in the annual cycle of tropical cyclone formation. The season included two very severe cyclonic storms, both in October, and one other named cyclonic storm, classified according to the tropical cyclone intensity scale of the India Meteorological Department. Cyclone Hudhud is estimated to have caused US$3.58 billion in damage across eastern India, and more than 120 deaths.

<span class="mw-page-title-main">2016 North Indian Ocean cyclone season</span> North Indian Ocean tropical cyclone season

The 2016 North Indian Ocean cyclone season was an event in the annual cycle of tropical cyclone formation. It was the deadliest season since 2010, killing more than 400 people. The season was an average one, seeing four named storms, with one further intensifying into a very severe cyclonic storm. The first named storm, Roanu, developed on 19 May while the season's last named storm, Vardah, dissipated on 18 December. The North Indian Ocean cyclone season has no official bounds, but cyclones tend to form between April and December, with the two peaks in May and November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean.

<span class="mw-page-title-main">2019 North Indian Ocean cyclone season</span> North Indian Ocean tropical cyclone season

The 2019 North Indian Ocean cyclone season was the most active North Indian Ocean cyclone season on record, in terms of cyclonic storms, however the 1992 season was more active according to the Joint Typhoon Warning Center. The season featured 12 depressions, 11 deep depressions, 8 cyclonic storms, 6 severe cyclonic storms, 6 very severe cyclonic storms, 3 extremely severe cyclonic storms, and 1 super cyclonic storm, Kyarr, the first since Cyclone Gonu in 2007. Additionally, it was also the third-costliest season recorded in the North Indian Ocean, only behind the 2020 and 2008 seasons.

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<span class="mw-page-title-main">2023 North Indian Ocean cyclone season</span> North Indian Ocean tropical cyclone season

The 2023 North Indian Ocean cyclone season was a very active season, featuring the second-highest accumulated cyclone energy (ACE) on record for the basin, only behind 2019. The North Indian Ocean cyclone season has no official bounds, but cyclones tend to form between April and December, with the peak from May to November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. However, a cyclone can form at any time during the year shown by an unnamed depression that affected Sri Lanka in January-February.

<span class="mw-page-title-main">Cyclone Asani</span> North Indian Ocean cyclone in 2022

Severe Cyclonic Storm Asani was a strong tropical cyclone that made landfall in India in May 2022. It was the strongest storm of 2022 North Indian Ocean cyclone season. The third depression and deep depression, and the first named storm of the 2022 North Indian Ocean cyclone season, Asani originated from a depression that the Indian Meteorological Department first monitored on May 7. Conditions rapidly favored development as the system became a deep depression by that day before intensifying to a Cyclonic Storm Asani. On the next day it further intensified and peak to a severe cyclonic storm, before making landfall as a deep depression system over Andhra Pradesh. It degenerated into a well marked low-pressure on May 12.

References

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  4. David Membery (July 2002). "Monsoon tropical cyclones: Part 2". Weather. 57 (7): 246–255. Bibcode:2002Wthr...57..246M. doi: 10.1256/004316502760195911 .
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  9. Neil L. Frank; S. A. Husain; National Hurricane Center, Pakistan Meteorological Department (June 1971). "The Deadliest Tropical Cyclone in History?". Bulletin of the American Meteorological Society. 52 (6): 438–444. Bibcode:1971BAMS...52..438F. doi: 10.1175/1520-0477(1971)052<0438:TDTCIH>2.0.CO;2 .
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  17. India Meteorological Department (1963). "Annual Summary — Storms & Depressions: Cyclonic storm in the Arabian Sea" (PDF). India Weather Review: 16–18. Retrieved May 13, 2013.
  18. India Meteorological Department (1963). "Annual Summary — Storms & Depressions: Severe cyclonic storm in the Bay of Bengal" (PDF). India Weather Review: 18–19. Retrieved May 13, 2013.
  19. India Meteorological Department (1963). "Annual Summary — Storms & Depressions: Severe cyclonic storm in the Bay of Bengal" (PDF). India Weather Review: 20–22. Retrieved May 13, 2013.
  20. India Meteorological Department (1963). "Annual Summary — Storms & Depressions: Depression in the Bay of Bengal" (PDF). India Weather Review: 20. Retrieved May 13, 2013.
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  22. India Meteorological Department (1963). "Annual Summary — Storms & Depressions: Cyclonic storm in the Arabian Sea" (PDF). India Weather Review: 22–24. Retrieved May 13, 2013.
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