1960 North Indian Ocean cyclone season#Very Severe Cyclonic Storm Ten

{{Infobox tropical cyclone small

|Basin=NIO

|Image=Severe Cyclonic Storm One analysis 16 May 1960.png

|Track=02-A 1960 track.png

|Formed=May 10

|Dissipated=May 19

|3-min winds=65

|Pressure=974

}}

On May 10, an area of low pressure was identified over the Arabian Sea roughly 400 km (250 mi) to the northwest of the Maldives. Moving northwestward, it gradually organized,{{cite web|publisher=International Best Track Archive|year=2013|access-date=May 9, 2013|title=1960 02A (1960132N09070)|url={{IBTRACS url|id=1960132N09070}}}} becoming a depression during by the evening of May 12.{{cite journal |author=India Meteorological Department |year=1960 |title=Annual Summary — Storms & Depressions: Severe cyclonic storm in the Arabian Sea |url=https://docs.lib.noaa.gov/rescue/cd024_pdf/005ED26A.pdf |journal=India Weather Review |publisher=National Oceanic and Atmospheric Administration |pages=1–4 |access-date=May 9, 2013 |archive-date=March 1, 2017 |archive-url=https://web.archive.org/web/20170301175136/https://docs.lib.noaa.gov/rescue/cd024_pdf/005ED26A.pdf |url-status=bot: unknown }} After turning more toward the west, the system continued to slowly deepen. On May 14, the S.S. Kampala sailed into the system, encountering {{convert|55|km/h|mph|abbr=on|round=5}} winds and rough seas. Over the following two days, the depression intensified into a cyclonic storm, with gale-force winds extending 150 km (90 mi) from the center. During the overnight hours of May 16 through 17, the SS Mohammedi sailed almost directly into the center of the cyclone, reporting a barometric pressure of 974 mbar (hPa; {{convert|974|mbar|inHg|lk=on|abbr=on|sigfig=4|disp=out}}) and {{convert|9.1|m|ft|abbr=on|0}} waves. Several other vessels, such as the S.S. Saudi and S.S. Exchequer, encountered the storm. Both ships reported hurricane-force winds, and the latter endured seas as high as {{convert|15.2|m|ft|abbr=on|0}} early on May 18. Later that day, the storm weakened so rapidly the crew of the S.S. Exchequer were able to watch the pressure on their barometer actively rise. The storm continued westward, moving ashore Al Mahrah Governorate in eastern South Yemen as a severe cyclonic storm on May 18, before dissipating. The next Yemeni landfall would not occur again until 2015 with Cyclone Chapala.{{cite report|publisher=India Meteorological Department|title=Extremely Severe Cyclonic Storm, Chapala over the Arabian Sea (28 October - 04 November 2015): A Report |date=December 2015|access-date=27 January 2016|url=http://www.rsmcnewdelhi.imd.gov.in/images/pdf/publications/preliminary-report/chap.pdf}}

As a developing cyclone, the system brought monsoon-like moisture to much of the Maldives, Ceylon (present-day Sri Lanka), and southern India between May 14 and 17. The heaviest rains fell on May 17, with {{convert|190|mm|in|abbr=on}} recorded at Cochin, India, that day.

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{{Infobox tropical cyclone small

|Basin=NIO

|Image=Deep Depression Two analysis 27 May 1960.png

|Track=01-B 1960 track.png

|Formed=May 26

|Dissipated=May 29

|Type1=deepdepression

|3-min winds=40

|Pressure=988

}}

On May 25, an upper-level low-pressure system developed over the northern Bay of Bengal. The following day, a surface low formed in association with this feature. By May 27, the low further consolidated into a depression while situated 285 km (175 mi) south of Calcutta, India.{{cite journal |author=India Meteorological Department |year=1960 |title=Annual Summary — Storms & Depressions: Deep depression in the Bay of Bengal |url=https://docs.lib.noaa.gov/rescue/cd024_pdf/005ED26A.pdf |journal=India Weather Review |publisher=National Oceanic and Atmospheric Administration |pages=4–5 |access-date=May 9, 2013 |archive-date=March 1, 2017 |archive-url=https://web.archive.org/web/20170301175136/https://docs.lib.noaa.gov/rescue/cd024_pdf/005ED26A.pdf |url-status=bot: unknown }} Tracking northward,{{cite web|publisher=International Best Track Archive|year=2013|access-date=May 9, 2013|title=1960 01B (1960148N20089)|url={{IBTRACS url|id=1960148N20089}}}} it intensified into a deep depression before making landfall on the Sundarbans region of West Bengal—near the border of East Pakistan—early on May 28. Though it was classified a deep depression, stronger winds of up to {{convert|75|km/h|mph|abbr=on|round=5}} were reported from Sagar Island. Based on measurements from nearby stations, it is estimated that the system attained a minimum pressure of 988 mb (hPa; 29.18 inHg) just as it moved ashore. Once inland, the system quickly weakened and accelerated northeastward. It later dissipated over Assam on May 30.

The system produced torrential rains across eastern India and East Pakistan. In Cherrapunji, {{convert|540|mm|in|abbr=on}} of rain fell during a two-day span, while many other areas recorded over {{convert|100|mm|in|abbr=on}}. No rainfall data were available from West Bengal and Assam. Strong winds from the storm destroyed numerous homes in West Bengal, and at least seven people were killed.{{cite news|agency =Associated Press|newspaper=Lewiston Morning Tribune|date=May 30, 1960|access-date=May 9, 2013|title=Indian Gale Kills Seven|page=6|location=Calcutta, India|url=https://news.google.com/newspapers?id=171eAAAAIBAJ&sjid=EDEMAAAAIBAJ&pg=5032,4738647&dq=bengal&hl=en}}

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{{Infobox tropical cyclone small

|Basin=NIO

|Image=Deep Depression Three analysis 2 July 1960.png

|Track=03-B 1960 track.png

|Formed=June 29

|Dissipated=July 4

|Type1=deepdepression

|3-min winds=

|Pressure=

}}

On June 29, a trough, associated with an upper-level low, extended over the northwestern Bay of Bengal. Following a drop in sea-level pressure over the next day, a depression formed in this area.{{cite journal|journal=India Weather Review|author =India Meteorological Department|publisher=National Oceanic and Atmospheric Administration|year=1960|access-date=May 9, 2013|title=Annual Summary — Storms & Depressions: Depression in the Bay of Bengal|url=http://docs.lib.noaa.gov/rescue/cd024_pdf/005ED26A.pdf|pages=5}} Moving slowly westward,{{cite web|publisher=International Best Track Archive|year=2013|access-date=May 9, 2013|title=1960 03B (1960182N20089)|url={{IBTRACS url|id=1960182N20089}}}} the storm intensified into a deep depression early on July 2. Shortly thereafter, the system made landfall near Angul, India, and accelerated toward the northwest. The system later dissipated on July 4 over Madhya Pradesh after being absorbed back into the trough that it developed from.

Widespread heavy rains accompanied the depression along portions of the coast from Orissa to West Bengal and as far inland as Madhya. Sagar Island recorded at least {{convert|360|mm|in|abbr=on}} of rain over the span of two days, while Vishakhapatnam received {{convert|300|mm|in|abbr=on}} in just one. As much as {{convert|100|mm|in|abbr=on}} of precipitation fell across Madhya Pradesh.

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{{Infobox tropical cyclone small

|Basin=NIO

|Image=Depression Four analysis 3 July 1960.png

|Track=04-A 1960 track.png

|Formed=July 2

|Dissipated=July 5

|Type1=niodepression

|3-min winds=40

|Pressure=991

}}

On June 26, a slow-moving trough developed over Gujarat. By July 2, the system developed into a shallow land depression while situated {{convert|80|km|mi|abbr=on}} north of Veraval. Winds in the area were measured up to {{convert|45|km/h|mph|abbr=on|round=5}}; however, as the system moved offshore, winds quickly increased to {{convert|65|km/h|mph|abbr=on|round=5}}. Low pressures were recorded across the area, with a minimum of 990.8 mbar (hPa; {{convert|990.8|mbar|inHg|abbr=on|sigfig=4|disp=out}}) measured in Dwarka. Becoming nearly stationary off the coast of Gujarat, the depression began to interact with an approaching monsoon. This interaction caused winds to increase, with two vessels reporting {{convert|75|km/h|mph|abbr=on|round=5}} winds during the late morning hours of July 4. Later that day, the system began moving to the northwest and quickly weakened. It was last noted the following day as a dissipating low over the northeastern Arabian Sea.{{cite journal|journal=India Weather Review|author =India Meteorological Department|publisher=National Oceanic and Atmospheric Administration|year=1960|access-date=May 9, 2013|title=Annual Summary — Storms & Depressions: Depression in the Arabian Sea|url=http://docs.lib.noaa.gov/rescue/cd024_pdf/005ED26A.pdf|pages=5–6}}

Between July 2 and 4, heavy rains amounting to more than {{convert|300|mm|in|abbr=on}} fell across much of the Saurashtra region of Gujarat. These rains triggered severe flooding that killed at least 35 people and left 6,000 others homeless. At least 500 homes were destroyed in the region.{{cite news|agency=Associated Press|newspaper=The Morning Herald|date=July 5, 1960|page=2|title=30 Die In Floods|location=Bombay, India}} {{subscription required|via=Newspapers.com}}

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{{Infobox tropical cyclone small

|Basin=NIO

|Image=Depression Five analysis 8 August 1960.png

|Track=05-B 1960 track.png

|Formed=August 8

|Dissipated=August 10

|Type1=niodepression

|3-min winds=15

|Pressure=996

}}

On August 6, a westward moving area of low pressure was identified over Burma. Initially an upper-level system, it gradually propagated to the surface, becoming a depression on August 9. Tracking west-northwestward, the system crossed the Indian coastline later that day near Balasore, where a pressure of 996.1 mbar (hPa; {{convert|996.1|mbar|inHg|abbr=on|sigfig=4|disp=out}}) was measured. Sustained winds reached just {{convert|30|km/h|mph|abbr=on|round=5}}. Once onshore, the depression degenerated into a remnant low on August 10. The remnants continued northwestward, ultimately merging with a trough over Uttar Pradesh on August 12.{{cite journal |author=India Meteorological Department |year=1960 |title=Annual Summary — Storms & Depressions: Depression in the Bay of Bengal |url=https://docs.lib.noaa.gov/rescue/cd024_pdf/005ED26A.pdf |journal=India Weather Review |publisher=National Oceanic and Atmospheric Administration |pages=6–7 |access-date=May 9, 2013 |archive-date=March 1, 2017 |archive-url=https://web.archive.org/web/20170301175136/https://docs.lib.noaa.gov/rescue/cd024_pdf/005ED26A.pdf |url-status=bot: unknown }}

The depression dropped heavy rains over parts of India between August 8 and August 14. The highest totals were recorded on August 14 when {{convert|240|mm|in|abbr=on}} of rain fell in Jhansi. Significant flooding took place along the Ganges River as a result of the rains. Forty villages along the river near Fatehgarh were inundated.

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{{Infobox tropical cyclone small

|Basin=NIO

|Image=Depression Six analysis 14 August 1960.png

|Track=07-B 1960 track.png

|Formed=August 12

|Dissipated=August 20

|Type1=deepdepression

|3-min winds=25

|Pressure=

}}

As the previous depression dissipated over India, a new circulation developed over the Bay of Bengal on August 12. This system quickly became a depression.{{cite journal |author=India Meteorological Department |year=1960 |title=Annual Summary — Storms & Depressions: Deep depression in the Bay of Bengal |url=https://docs.lib.noaa.gov/rescue/cd024_pdf/005ED26A.pdf |journal=India Weather Review |publisher=National Oceanic and Atmospheric Administration |pages=7–8 |access-date=May 9, 2013 |archive-date=March 1, 2017 |archive-url=https://web.archive.org/web/20170301175136/https://docs.lib.noaa.gov/rescue/cd024_pdf/005ED26A.pdf |url-status=bot: unknown }} Moving slowly northwestward,{{cite web|publisher=International Best Track Archive|access-date=May 9, 2013|title=1960 07B (1960226N19090)|url={{IBTRACS url|id=1960226N19090}}}} it became a deep depression on August 14 before making landfall in the Sundarbans region. Winds up to {{convert|45|km/h|mph|abbr=on|round=5}} were reported in Sandheads. Once onshore, it turned westward and slowed while maintaining its intensity. The system finally weakened on August 18 as it resumed moving northwestward again, and two days later it dissipated over southeastern Rajasthan.

Large portions of India were affected by rains from the depression, with Orissa and Madhya receiving the heaviest rains. According to Prime Minister Jawaharlal Nehru, up to {{convert|40|in|mm|abbr=on|disp=flip}} of rain fell across portions of Orissa. The tremendous precipitation triggered disastrous floods that killed at least 65 people. Continued rains over the next two weeks exacerbated the situation and by August 30, an estimated 2.5 million people were homeless.{{cite news|agency=United Press International|newspaper=Wisconsin State Journal|date=August 30, 1960|title=2,500,000 Homeless in India Floods|location=Calcutta, India|page=5}} {{subscription required|via=Newspapers.com}} Most affected were areas around the Mahanadi River and its tributaries where flood waters reached {{convert|12|ft|m|abbr=on|disp=flip}} in depth. At least 85 villages were reportedly destroyed. Orissa government officials described the disaster as "the worst in living memory."{{cite news|agency=New York Times Service|newspaper=The Salt Lake Tribune|date=August 26, 1960|title=Flood Disaster Hits India Area|location=New Delhi, India|page=6}} {{subscription required|via=Newspapers.com}} Rail lines and roads were severely damaged across the state, hampering initial relief efforts. A total of 1.87 million acres of crops were flooded and overall damage amounted to {{ntsp|111700000||{{Indian Rupee|link=Indian Rupee}}}}.{{cite web|work=Department of Water Resources|publisher=Government of Orissa|year=2009|access-date=April 23, 2015|title=List of Past Flood and Area Damaged by Flood in Orissa|url=http://www.dowrorissa.gov.in/HistoryofFLOOD/HistoryofFLOOD.pdf|archive-url=https://web.archive.org/web/20150225020947/http://dowrorissa.gov.in/HistoryofFLOOD/HistoryofFLOOD.pdf|archive-date=February 25, 2015|url-status=dead}}

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{{Infobox tropical cyclone small

|Basin=NIO

|Image=Depression Seven analysis 24 August 1960.png

|Track=06-B 1960 track.png

|Formed=August 24

|Dissipated=August 28

|Type1=niodepression

|3-min winds=

|Pressure=

}}

On August 20, a wave of low pressure formed over Burma. Moving westwards, this upper-level system triggered the development of a surface low two days later over the Bay of Bengal. Turning northwestward, the low consolidated into a depression by August 24 before making landfall in the Sundarbans region later that day. Once onshore, the depression degenerated into a remnant low; the remnants persisted until August 28 when they were absorbed into a trough over Rajasthan Pradesh.{{cite journal |author=India Meteorological Department |year=1960 |title=Annual Summary — Storms & Depressions: Depression in the Bay of Bengal |url=https://docs.lib.noaa.gov/rescue/cd024_pdf/005ED26A.pdf |journal=India Weather Review |publisher=National Oceanic and Atmospheric Administration |pages=8 |access-date=May 9, 2013 |archive-date=March 1, 2017 |archive-url=https://web.archive.org/web/20170301175136/https://docs.lib.noaa.gov/rescue/cd024_pdf/005ED26A.pdf |url-status=bot: unknown }}

Heavy rains affected much of Bihar, Madhya Pradesh, Punjab, and Uttar Pradesh. The highest daily precipitation total was measured in Ghatsila at {{convert|190|mm|in|abbr=on}}. These rains triggered severe flooding along the Beas, Ganges, Jamuna, and Sutlej rivers. Large areas of Uttar Pradesh were left submerged, and significant crop and property damage took place in Punjab. At least 55 people were killed in Punjab alone, and losses overall amounted to $9.24 million (1960 USD).{{cite news|newspaper=New York Times|date=September 4, 1960|title=Punjab Flood Toll 55; Loss From High Water Is Put at $9,240,000}}

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{{Infobox tropical cyclone small

|Basin=NIO

|Image=Deep Depression Eight analysis 24 September 1960.png

|Track=08-B 1960 track.png

|Formed=September 24

|Dissipated=September 28

|Type1=

|3-min winds=30

|Pressure=

}}

On September 22, an area of low pressure was identified over the Andaman Sea. Tracking northwestward, the system consolidated into a depression two days later over the Bay of Bengal. During the evening of September 24, it further strengthened to a deep depression, with winds of {{convert|55|km/h|mph|abbr=on|round=5}}. Early the next day it made landfall in Orissa between Balasore and Chandabali.{{cite journal|journal=India Weather Review|author =India Meteorological Department|publisher=National Oceanic and Atmospheric Administration|year=1960|access-date=May 9, 2013|title=Annual Summary — Storms & Depressions: Deep depression in the Bay of Bengal|url=http://docs.lib.noaa.gov/rescue/cd024_pdf/005ED26A.pdf|pages=9–10}} Once onshore, the system slowed and turned northeastward.{{cite web|publisher=International Best Track Archive|year=2013|access-date=May 9, 2013|title=1960 08B (1960270N21087)|url={{IBTRACS url|id=1960270N21087}} }} It later dissipated over Nepal on September 28 as it interacted with the Himalayas.

Heavy rains accompanying the depression affected much of Bihar, Orissa, and West Bengal. Many areas recorded more than {{convert|200|mm|in|abbr=on}} during a four-day span; the highest single-day total was {{convert|270|mm|in|abbr=on}} in Bahadurganj.

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{{Infobox tropical cyclone small

|Basin=NIO

|Image=Severe Cyclonic Storm Nine analysis 10 October 1960.png

|Track=10-B 1960 track.png

|Formed=October 5 (Entered basin)

|Dissipated=October 12

|Type1=

|3-min winds=60

|1-min winds=85

|Pressure=986

}}

In late September, a tropical storm developed over the South China Sea. Striking South Vietnam, the storm slowly moved over Indochina, ultimately crossing 100°E and entering the basin on October 5 while over Thailand. After crossing southern Burma,{{cite web|publisher=International Best Track Archive|year=2013|access-date=May 9, 2013|title=1960 10B (1960273N13117)|url={{IBTRACS url|id=1960273N13117}}}} the low moved northwestward over the Bay of Bengal and reorganized. Following a report of {{convert|45|km/h|mph|abbr=on|round=5}} winds from the S.S. Glenpark on October 8, the system was classified as a depression.{{cite journal|journal=India Weather Review|author =India Meteorological Department|publisher=National Oceanic and Atmospheric Administration|year=1960|access-date=May 9, 2013|title=Annual Summary — Storms & Depressions: Severe cyclonic storm in the Bay of Bengal|url=http://docs.lib.noaa.gov/rescue/cd024_pdf/005ED26A.pdf|pages=10–11}} Moving slowly northwestwards, the system further deepened into a cyclonic storm on October 9. Several ships in the path of the storm recorded gale-force winds, depicting its strengthening. Early on October 10, it became a severe cyclonic storm and soon reached its peak intensity with winds of {{convert|110|km/h|mph|abbr=on|round=5}}. Its central pressure at this time was estimated to be 986 mbar (hPa; {{convert|986|mbar|inHg|abbr=on|sigfig=4|disp=out}}). The National Oceanic and Atmospheric Administration (NOAA) estimated that the storm attained one-minute sustained winds of {{convert|155|km/h|mph|abbr=on|round=5}}. Turning northeastward, the system made landfall between Barisal and Noakhali in East Pakistan, with the eye passing directly over the islands of Bhola, Hatia, and Ramgati. Once onshore, the system quickly weakened and ultimately dissipated over Assam early on October 12.

Across coastal areas of East Pakistan, the storm wrought catastrophic damage. A {{convert|5.8|m|ft|abbr=on}} tidal surge washed over the islands of Hatia, Sandwip, Kutubdia. Communications across the region were crippled, and it took six days for word of the scale of damage to reach officials. Entire villages were reportedly wiped out by the storm.{{cite news|agency =Associated Press|newspaper=St. Petersburg Times|date=October 17, 1960|access-date=May 9, 2013|title=Tidal Wave Kills 3,000 In Pakistan|page=1|location=Dacca, East Pakistan|url=https://news.google.com/newspapers?id=tz5SAAAAIBAJ&sjid=HHkDAAAAIBAJ&dq=bengal&pg=3665%2C3502118}} Approximately 35,000 homes were destroyed, most of which were thatched huts made of bamboo and mud. About 300 schools were also damaged.{{cite news|newspaper=The Age|date=October 18, 1960|access-date=May 9, 2013|title=Pakistan Troops Aid Rescue Teams|location=Dacca, East Pakistan|page=4|url=https://news.google.com/newspapers?id=6q4UAAAAIBAJ&sjid=e7oDAAAAIBAJ&dq=pakistan&pg=5665%2C3128446}} The worst damage took place on Ramgati Island where 3,500 people were killed.{{cite news|newspaper=The Glasgow-Herald|date=October 18, 1960|access-date=May 9, 2013|title=Relief Work In Pakistan: Cyclone Aftermath|page=1|location=Dacca, East Pakistan|url=https://news.google.com/newspapers?id=AHdAAAAAIBAJ&sjid=b6MMAAAAIBAJ&dq=pakistan&pg=5896%2C7138164}} Roughly 95 percent of the island's structure were destroyed, forcing residents to cling to trees for survival. Only two police officers survived and were able to inform government officials of the disaster.{{cite news|agency =Associated Press|newspaper=The Sunday News Press|date=October 22, 1960|access-date=May 9, 2013|title=Pakistan Storm Toll on Island Rises to 3,500|location=Dacca, East Pakistan|page=5|url=https://news.google.com/newspapers?id=yypUAAAAIBAJ&sjid=IjoNAAAAIBAJ&dq=pakistan&pg=2243%2C3614997}} An estimated 6,000 people perished while another 100,000 were left homeless. Heavy rain accompanied the storm, with Cox's Bazar reporting {{convert|180|mm|in|abbr=on}}. Relief efforts in the wake of the storm were hampered by the nation's poor infrastructure and debris left behind.{{cite news|agency =Associated Press|newspaper=The Milwaukee Journal|date=October 17, 1960|access-date=May 9, 2013|title=3,000 East Pakistanis Are Killed by Storm|location=Dacca, East Pakistan|page=1|url=https://news.google.com/newspapers?id=Ot8jAAAAIBAJ&sjid=_iUEAAAAIBAJ&dq=bengal&pg=1952%2C4626892}} On October 18, members of the East Pakistani military were deployed to the hardest hit areas to provide stable communication and clean drinking water.

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{{Infobox tropical cyclone small

|Basin=NIO

|Image=Severe Cyclonic Storm Ten analysis 31 October 1960.png

|Track=09-B 1960 track.png

|Formed=October 27

|Dissipated=November 1

|Type1=

|3-min winds=80

|1-min winds=105

|Pressure=967

}}

On October 26, a trough formed over the south Andaman Sea and extended into the southern Bay of Bengal. By October 28, the system consolidated into a depression as it moved northwestward. Steadily intensifying, several ships encountered the storms increasing winds as it moved northward in the Bay. On October 30, it attained gale-force winds and further became a severe cyclonic storm early the next morning. During the evening of October 31, the IST Barisal recorded winds of {{convert|130|km/h|mph|abbr=on|round=5}}, indicating that the system had acquired a core of hurricane-force winds. The maximum winds of this system is unknown, though reports indicated that winds peaked between 150 and 215 km/h (90 and 135 mph). NOAA estimated that the storm peaked with one-minute sustained winds of {{convert|195|km/h|mph|abbr=on|round=5}} and a pressure of 966.7 mbar (hPa; {{convert|966.7|mbar|inHg|abbr=on|sigfig=4|disp=out}}).{{cite journal|journal=Monthly Weather Review|author =Gordon E. Dunn, United States Weather Bureau|publisher=National Oceanic and Atmospheric Administration|issue=3|volume=90|date=March 1962|access-date=May 10, 2013|title=The Tropical Cyclone Problem In East Pakistan|url=http://docs.lib.noaa.gov/rescue/mwr/090/mwr-090-03-0083.pdf|doi=10.1175/1520-0493(1962)090<0083:TTCPIE>2.0.CO;2|pages=83–86|bibcode = 1962MWRv...90...83D |doi-access=free}} The storm soon made landfall with great intensity near Noakhali, East Pakistan, just three weeks after the previous storm devastated the country.{{cite journal|journal=India Weather Review|author =India Meteorological Department|publisher=National Oceanic and Atmospheric Administration|year=1960|access-date=May 9, 2013|title=Annual Summary — Storms & Depressions: Severe cyclonic storm in the Bay of Bengal|url=http://docs.lib.noaa.gov/rescue/cd024_pdf/005ED26A.pdf|pages=11–13}} Once onshore, cold, dry air quickly wrapped around the backside of the cyclone. Within four hours of landfall, little rainfall was reported near the storm's eye. The cyclone rapidly weakened and dissipated the following day over the Lushai Hills.

Striking East Pakistan as a powerful storm, the system produced a storm tide of {{convert|6.1|m|ft|abbr=on}} that moved 16 km (10 mi) inland, devastating many communities. A storm surge of {{convert|6.7|m|ft|abbr=on}} was measured in Halishahar. In addition to the surge, there was a series of tidal waves that followed the storm, causing additional damage. Offshore, these waves were estimated at {{convert|12.2|m|ft|abbr=on}}; though they significantly decreased before impacting land. Chittagong and surrounding communities were regarded as the hardest hit, with most being submerged in {{convert|3|m|ft|abbr=on|0}} of water. The city's port was largely destroyed, with almost every vessel washed ashore. Some were found 16 km (10 mi) away and one even at another port. The storm's intense winds, estimated as high as {{convert|240|km/h|mph|abbr=on|round=5}} on Sandwip Island, leveled buildings and scattered debris over large distances. Crops were flattened by the storm and in some instances had been "burnt" by the sheer force of the wind. A total of 14,174 people perished in the storm while another 200,000 were left homeless.{{cite news|agency =Reuters|newspaper=The Sydney Morning Herald|date=May 10, 1961|access-date=May 10, 2013|title=Ships Sink In Cyclone|location=Karachi, India|page=1|url=https://news.google.com/newspapers?id=5XxWAAAAIBAJ&sjid=HeYDAAAAIBAJ&dq=cyclone&pg=2196%2C1993784}} Following the mass casualties from the two storms, the Government of Pakistan requested the assistance of former National Hurricane Center director, Gordon E. Dunn, to improve the warning system.{{cite journal|journal=Bulletin of the American Meteorological Society|publisher=American Meteorological Society|author =Neil L. Frank|author2=S. A. Husain|author3=National Hurricane Center, Pakistan Meteorological Department|title=The Deadliest Tropical Cyclone in History?|date=June 1971|pages=438–444|volume=52|issue=6|doi=10.1175/1520-0477(1971)052<0438:TDTCIH>2.0.CO;2|bibcode=1971BAMS...52..438F|doi-access=free}}

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{{Infobox tropical cyclone small

|Basin=NIO

|Image=Depression Eleven analysis 7 November 1960.png

|Track=14-A 1960 track.png

|Formed=November 7

|Dissipated=November 10

|Type1=

|3-min winds=25

|Pressure=

}}

On November 5, an area of low pressure was identified over Lakshadweep.{{cite journal|journal=India Weather Review|author =India Meteorological Department|publisher=National Oceanic and Atmospheric Administration|year=1960|access-date=May 9, 2013|title=Annual Summary — Storms & Depressions: Depression in the Arabian Sea|url=http://docs.lib.noaa.gov/rescue/cd024_pdf/005ED26A.pdf|pages=13–14}} Tracking generally northwestward,{{cite web|publisher=International Best Track Archive|year=2013|access-date=May 9, 2013|title=1960 14A (1960312N11069)|url={{IBTRACS url|id=1960312N11069}}}} it gradually organized into a depression by November 7. No further development took place over the following days and the system eventually degraded into a remnant low on November 10. Though the storm itself did not impact land, associated moisture combined with a low over the Bay of Bengal to produce heavy rains across Madras State and nearby islands from November 5 to 10.

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{{Infobox tropical cyclone small

|Basin=NIO

|Image=Shallow Depression Twelve analysis 10 November 1960.png

|Track=11-B 1960 track.png

|Formed=November 10

|Dissipated=November 12

|Type1=niodepression

|3-min winds=

|Pressure=

}}

On November 7, an area of low pressure over the Bay of Bengal formed and gradually moved towards India. By November 9, it was located just of the Coromandel Coast. The following day, it deepened into a depression while situated off the northern edge of Ceylon. Becoming nearly stationary, the system failed to develop and soon weakened into a remnant low. The low dissipated early on November 12. Heavy rains fell across much of Madras State in association with the system; a 24‑hour total of {{convert|240|mm|in|abbr=on}} was reported in Nagapattinam. These rains triggered significant flooding that disrupted travel and communications. Severe damage took place in Madurai where 10,000 people were left homeless. Overall, five people were killed and 150,000 were left homeless.{{cite journal|journal=India Weather Review|author =India Meteorological Department|publisher=National Oceanic and Atmospheric Administration|year=1960|access-date=May 9, 2013|title=Annual Summary — Storms & Depressions: Depression in the Arabian Sea|url=http://docs.lib.noaa.gov/rescue/cd024_pdf/005ED26A.pdf|pages=13}}

{{clear}}

{{Infobox tropical cyclone small

|Basin=NIO

|Image=Cyclonic Storm Thirteen analysis 20 November 1960.png

|Track=15-A 1960 track.png

|Formed=November 17

|Dissipated=November 23

|3-min winds=40

|Pressure=994

}}

On November 14, an area of low pressure formed to the west of Lakshadweep. Tracking generally westward, it eventually developed into a depression three days later. Gradual intensification took place over the following two days, with the system becoming a cyclonic storm on November 19. On November 20, the system attained its peak intensity with winds of {{convert|75|km/h|mph|abbr=on|round=5}} and a minimum pressure of 994 mbar (hPa; {{convert|994|mbar|inHg|abbr=on|sigfig=4|disp=out}}). Continuing westward, the cyclone entered the Gulf of Aden on November 22 before becoming nearly stationary. During this time, it weakened to a depression before dissipating the following day.{{cite journal|journal=India Weather Review|author =India Meteorological Department|publisher=National Oceanic and Atmospheric Administration|year=1960|access-date=May 9, 2013|title=Annual Summary — Storms & Depressions: Cyclonic storm in the Arabian Sea|url=http://docs.lib.noaa.gov/rescue/cd024_pdf/005ED26A.pdf|pages=14–15}}

{{clear}}

{{Infobox tropical cyclone small

|Basin=NIO

|Image=Cyclonic Storm Fourteen analysis 19 November 1960.png

|Track=13-B 1960 track.png

|Formed=November 18

|Dissipated=November 21

|Type1=cyclstorm

|3-min winds=

|Pressure=996

}}

A well-defined area of low pressure was identified over the southwestern Bay of Bengal on November 17. The following day, the system developed into a depression as it moved slowly northwestward. On November 20, as it neared the coast of Tamil Nadu, it intensified into a cyclonic storm, with gusts estimated as high as {{convert|135|km/h|mph|abbr=on}}. Shortly thereafter, it made landfall near Chennai. In nearby Tambaram, a pressure of 995.7 mbar (hPa; {{convert|995.7|mbar|inHg|abbr=on|sigfig=4|disp=out}}) was recorded, the lowest in relation to the cyclone. A small storm, it quickly weakened once onshore and was last noted early on November 21 as a dissipating low.{{cite journal|journal=India Weather Review|author =India Meteorological Department|publisher=National Oceanic and Atmospheric Administration|year=1960|access-date=May 9, 2013|title=Annual Summary — Storms & Depressions: Cyclonic storm in the Bay of Bengal|url=http://docs.lib.noaa.gov/rescue/cd024_pdf/005ED26A.pdf|pages=14}}

Heavy rains impacted most of southern Madras State, with a maximum daily total of {{convert|110|mm|in|abbr=on}} in Punalur. The most significant damage took place in Madras City where gale-force winds uprooted trees and disrupted transport and communications. Many poorly constructed homes were damaged or destroyed by the storm, leaving numerous low-income families homeless.

{{clear}}

{{Infobox tropical cyclone small

|Basin=NIO

|Image=Depression Fifteen analysis 1 December 1960.png

|Track=12-B 1960 track.png

|Formed=November 26

|Dissipated=December 3

|3-min winds=30

|Type1=niodepression

|Pressure=

}}

On November 24, the SS Rajula sailed under a well-defined trough over the southwest Bay of Bengal and reported {{convert|55|km/h|mph|abbr=on|round=5}} winds. Two days later, a tropical wave interacted with the system and resulted in the development of a depression. Over the following several days, the system drifted northwestward without change in intensity. By December 3, it degenerated into a remnant low, ultimately tracking over southern India, near Circars, on December 4 before dissipating. The system brought locally heavy rains to parts of the Andaman Islands and Andhra Pradesh.{{cite journal|journal=India Weather Review|author =India Meteorological Department|publisher=National Oceanic and Atmospheric Administration|year=1960|access-date=May 9, 2013|title=Annual Summary — Storms & Depressions: Depression in the Bay of Bengal|url=http://docs.lib.noaa.gov/rescue/cd024_pdf/005ED26A.pdf|pages=15–17}}

{{clear}}

This is a table of all storms in the 1960 North Indian Ocean cyclone season. It mentions all of the season's storms and their names, durations, peak intensities (according to the IMD storm scale), areas affected, damages, and death totals. Damage and death totals include the damage and deaths caused when that storm was a precursor wave or extratropical low, and all of the damage figures are in 1960 USD.

{{North Indian Ocean areas affected (Top)}}

|-

| One || {{Sort|01|May 10–19}} || bgcolor=#{{storm colour|VSCS}}|{{Sort|5|Very severe cyclonic storm}} || bgcolor=#{{storm colour|VSCS}}|{{Sort|120|{{convert|120|km/h|mph|abbr=on|round=5}}}} || bgcolor=#{{storm colour|VSCS}}|{{sort|0974|{{convert|974|hPa|inHg|sigfig=4|abbr=on}}}} || Maldives, Ceylon, South India ||align=right| {{ntsh|0}} Minimal ||align=right| {{nts|0}} ||

|-

| Two || {{Sort|02|May 26–29}} || bgcolor=#{{storm colour|DD}}|{{Sort|2|Deep depression}} || bgcolor=#{{storm colour|DD}}|{{Sort|075|{{convert|75|km/h|mph|abbr=on|round=5}}}} || bgcolor=#{{storm colour|DD}}|{{sort|0988|{{convert|988|hPa|inHg|sigfig=4|abbr=on}}}} || East India, Northeast India, East Pakistan ||align=right| {{ntsh|1}} Unknown ||align=right| {{nts|7}} ||

|-

| Three || {{Sort|03|June 29 – July 4}} || bgcolor=#{{storm colour|DD}}|{{Sort|2|Deep depression}} || bgcolor=#{{storm colour|DD}}|{{Sort|0|N/A}} || bgcolor=#{{storm colour|DD}}|{{sort|0|N/A}} || East India, North India ||align=right| {{ntsh|1}} Unknown ||align=right| {{nts|0}} ||

|-

| Four || {{Sort|04|July 2–5}} || bgcolor=#{{storm colour|D}}|{{Sort|1|Depression}} || bgcolor=#{{storm colour|D}}|{{Sort|075|{{convert|75|km/h|mph|abbr=on|round=5}}}} || bgcolor=#{{storm colour|D}}|{{sort|0991|{{convert|991|hPa|inHg|sigfig=4|abbr=on}}}} || Gujarat ||align=right| {{ntsh|1}} Unknown ||align=right| {{nts|35}} ||

|-

| Five || {{Sort|05|August 8–10}} || bgcolor=#{{storm colour|D}}|{{Sort|1|Depression}} || bgcolor=#{{storm colour|D}}|{{Sort|030|{{convert|30|km/h|mph|abbr=on|round=5}}}} || bgcolor=#{{storm colour|D}}|{{sort|0996|{{convert|996|hPa|inHg|sigfig=4|abbr=on}}}} || East India, North India ||align=right| {{ntsh|1}} Unknown ||align=right| {{nts|0}} ||

|-

| Six || {{Sort|06|August 12–20}} || bgcolor=#{{storm colour|DD}}|{{Sort|2|Deep depression}} || bgcolor=#{{storm colour|DD}}|{{Sort|045|{{convert|45|km/h|mph|abbr=on|round=5}}}} || bgcolor=#{{storm colour|DD}}|{{sort|0|N/A}} || East India, Northeast India, North India ||align=right| {{ntsh|2}} Millions ||align=right| {{nts|65}} ||

|-

| Seven || {{Sort|07|August 24–28}} || bgcolor=#{{storm colour|D}}|{{Sort|1|Depression}} || bgcolor=#{{storm colour|D}}|{{Sort|0|N/A}} || bgcolor=#{{storm colour|D}}|{{sort|0|N/A}} || East India, Northeast India, North India ||align=right| {{ntsp|9240000}} ||align=right| {{ntsh|55}} >55 ||

|-

| Eight || {{Sort|08|September 24–28}} || bgcolor=#{{storm colour|DD}}|{{Sort|2|Deep depression}} || bgcolor=#{{storm colour|DD}}|{{Sort|055|{{convert|55|km/h|mph|abbr=on|round=5}}}} || bgcolor=#{{storm colour|DD}}|{{sort|0|N/A}} || East India, Northeast India ||align=right| {{ntsh|0}} Minimal ||align=right| {{nts|0}} ||

|-

| Nine || {{Sort|09|October 5–12}} || bgcolor=#{{storm colour|SCS}}|{{Sort|4|Severe cyclonic storm}} || bgcolor=#{{storm colour|SCS}}|{{Sort|110|{{convert|110|km/h|mph|abbr=on|round=5}}}} || bgcolor=#{{storm colour|SCS}}|{{sort|0986|{{convert|986|hPa|inHg|sigfig=4|abbr=on}}}} || Thailand, Burma, East Pakistan, Northeast India ||align=right| {{ntsh|1}} Unknown ||align=right| {{ntsh|6000}} ~6,000 ||

|-

| Ten || {{Sort|10|October 27 – November 1}} || bgcolor=#{{storm colour|VSCS}}|{{Sort|5|Very severe cyclonic storm}} || bgcolor=#{{storm colour|VSCS}}|{{Sort|150|{{convert|150|km/h|mph|abbr=on|round=5}}}} || bgcolor=#{{storm colour|VSCS}}|{{sort|0967|{{convert|967|hPa|inHg|sigfig=4|abbr=on}}}} || East Pakistan, Northeast India, Burma ||align=right| {{ntsh|1}} Unknown ||align=right| {{nts|14,174}} ||

|-

| Eleven || {{Sort|11|November 7–10}} || bgcolor=#{{storm colour|D}}|{{Sort|1|Depression}} || bgcolor=#{{storm colour|D}}|{{Sort|045|{{convert|45|km/h|mph|abbr=on|round=5}}}} || bgcolor=#{{storm colour|D}}|{{sort|0|N/A}} || Madras State ||align=right| {{ntsh|0}} None ||align=right| {{nts|0}} ||

|-

| Twelve || {{Sort|12|November 10–12}} || bgcolor=#{{storm colour|D}}|{{Sort|0|Shallow depression}} || bgcolor=#{{storm colour|D}}|{{Sort|0|N/A}} || bgcolor=#{{storm colour|D}}|{{sort|0|N/A}} || Ceylon, Madras State ||align=right| {{ntsh|1}} Unknown ||align=right| {{nts|5}} ||

|-

| Thirteen || {{Sort|13|November 17–23}} || bgcolor=#{{storm colour|CS}}|{{Sort|3|Cyclonic storm}} || bgcolor=#{{storm colour|CS}}|{{Sort|075|{{convert|75|km/h|mph|abbr=on|round=5}}}} || bgcolor=#{{storm colour|CS}}|{{sort|0994|{{convert|994|hPa|inHg|sigfig=4|abbr=on}}}} || None ||align=right| {{ntsh|0}} None ||align=right| {{nts|0}} ||

|-

| Fourteen || {{Sort|14|November 18–21}} || bgcolor=#{{storm colour|CS}}|{{Sort|3|Cyclonic storm}} || bgcolor=#{{storm colour|CS}}|{{Sort|1|N/A}} || bgcolor=#{{storm colour|CS}}|{{sort|0996|{{convert|996|hPa|inHg|sigfig=4|abbr=on}}}} || South India ||align=right| {{ntsh|1}} Unknown ||align=right| {{nts|0}} ||

|-

| Fifteen || {{Sort|15|November 26 – December 3}} || bgcolor=#{{storm colour|D}}|{{Sort|1|Depression}} || bgcolor=#{{storm colour|D}}|{{Sort|055|{{convert|55|km/h|mph|abbr=on|round=5}}}} || bgcolor=#{{storm colour|D}}|{{sort|0|N/A}} || Andaman Islands, Andhra Pradesh ||align=right| {{ntsh|0}} None ||align=right| {{nts|0}} ||

|-

{{TC Areas affected (Bottom)|TC's=15 systems|dates=May 10 – December 3|winds={{convert|150|km/h|mph|abbr=on|round=5}}|pres={{convert|967|hPa|inHg|sigfig=4|abbr=on}}|damage=>{{ntsp|9240000}}|deaths=20,341|Refs=}}

{{Portal|Tropical cyclones}}

• North Indian Ocean tropical cyclone
• List of tropical cyclone records
• 1960 Atlantic hurricane season
• 1960 Pacific hurricane season
• 1960 Pacific typhoon season
• Australian region cyclone seasons: 1959–60 1960–61
• South Pacific cyclone seasons: 1959–60 1960–61
• South-West Indian Ocean cyclone seasons: 1959–60 1960–61

{{reflist|30em}}

• [https://web.archive.org/web/20150517005046/http://www.imd.gov.in/section/nhac/dynamic/cyclone.htm India Meteorological Department]
• [http://www.usno.navy.mil/JTWC/ Joint Typhoon Warning Center] {{Webarchive|url=https://web.archive.org/web/20150809201922/http://www.usno.navy.mil/JTWC/ |date=2015-08-09 }}

{{TC Decades|Year=1960|basin=North Indian Ocean|type=cyclone}}

{{Tropical cyclone season|1960}}

{{DEFAULTSORT:1960 North Indian Ocean Cyclone Season}}

Category:Tropical cyclones in India

Category:1960 in India

Category:1960 in East Pakistan

Category:Articles which contain graphical timelines

Category:1960 disasters in India

Category:1960 disasters in Pakistan