1936 North Indian Ocean cyclone season

none NIO 1960 April 22, 1936 December 31, 1936 Two 65 979 3 20 (18 official, 2 unofficial) 8 6 3 3 293 total 0.075 > 1934, 1935, 1936, 1937, 1938 1936 Atlantic hurricane season 1936 Pacific hurricane season 1936 Pacific typhoon season The 1936 North Indian Ocean cyclone season was an above-average cyclone season, featuring eighteen depressions, eight of which intensified into deep depressions. Of those eight systems, six intensified into cyclonic storms. Of these six, three intensified further, becoming severe cyclonic storms and very severe cyclonic storms. The North Indian Ocean cyclone season has no official bounds, but cyclones tend to form between April and November, with peaks in late April to May and October to November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. The official Regional Specialized Meteorological Centre in the basin is the India Meteorological Department (IMD), which at the time, was the sole agency issuing warnings on tropical cyclones in the basin. left Season summary The 1936 North Indian Ocean cyclone season took place during the neutral phase of the El Niño–Southern Oscillation,Past Events https://psl.noaa.gov/enso/past_events.html Physics Science Laboratory National Oceanic and Atmospheric Administration 20 September 2024 which is correlated with less activity in the basin.Climate Dynamics 2020 1575 Additionally, ENSO-neutral conditions are also correlated to a higher chance of landfall in the eastern coast of India,Climate Dynamics 2020 1585 hence the fact that a majority of the systems impacted land.India Weather Review 1936 In total, the season had eighteen depressions, eight of which intensified into deep depressions, with six intensifying further into cyclonic storms, and three further developing into severe cyclonic storms and very severe cyclonic storms.India Weather Review 1936 The season began on April 21, when a cyclone developed in the Bay of Bengal. Peaking as an very severe cyclonic storm, it would make landfall in modern-day Myanmar prior to dissipating.India Weather Review 1936 1-4 A month after that system dissipated, another very severe cyclonic storm formed in late May, making landfall in East India prior to dissipating.India Weather Review 1936 5-7 Three depressions would form in June, with two developing into cyclonic storms.India Weather Review 1936 8-11 In July, three depressions would form, with one of them developing into a deep depression prior to dissipating.India Weather Review 1936 11-12 In August, two systems would form, with one of them becoming a deep depression prior to making landfall in Andhra Pradesh.India Weather Review 1936 13-14 September would feature three systems.India Weather Review 1936 14-20 The first and second systems, weak depression, would not be of much importance.India Weather Review 1936 14-16 However, the third system would peak as a very severe cyclonic storm prior to striking Odisha in early October.India Weather Review 1936 16-20 In October, only one system, a deadly cyclonic storm would form.India Weather Review 1936 21-22 However, November and December would be more active, featuring two depressions each.India Weather Review 1936 24-26 The last system, a weak depression offshore Sri Lanka, would form on December 30 and dissipate early the next day.India Weather Review 1936 22 Systems Very Severe Cyclonic Storm One 1936 Burma cyclone NIO 01B 1936 path.png 22 April 26 April 65 993 On April 21, due to a temporary advancement of the southwest monsoon, a low-pressure area was first identified near the Nicobar Islands. Developing over the southeastern Bay of Bengal, later that day, it coalesced into an area of unsettled weather.India Weather Review 1936 1 Further development occurred, and on 00:00 UTC the next day, the disturbance developed into a depression west of the Nicobar Islands.India Weather Review 1936 11936 Severe Cyclonic Storm UNNAMED (1936113N10090) 2024 https://ncics.org/ibtracs/index.php?name=v04r01-1936113N10090 Gahtan J. 2024-09-12 Knapp K. R. National Centers for Environmental Information Schreck C. J. Diamond H. J. Kossin J. P. Kruk M. C. Undergoing rapid intensification,India Weather Review 1936 3 by 12:00 UTC that same day, the cyclone had peaked as a very severe cyclonic storm with sustained winds of 65 kn mph km/h. It later attained a minimum pressure of 993 hPa inHg at 21:00 UTC that day.India Weather Review 1936 4 Soon after, the cyclone recurved, with its intensity remaining the same as it tracked northeastward the next few days.India Weather Review 1936 4 At 03:00 UTC on April 26, the cyclone made its first landfall over Cheduba Island near peak intensity, producing intense winds there.India Weather Review 1936 4 Soon after, it made its second landfall along the coast of Myanmar, somewhere between Thandwe and Kyaukphyu.India Weather Review 1936 3 Rapidly weakening, it dissipated later that day.India Weather Review 1936 4 The most intense storm to strike Myanmar prior to 1970,Masters Jeff Top weather story of 2008: Cyclone Nargis https://www.wunderground.com/blog/JeffMasters/top-weather-story-of-2008-cyclone-nargis.html 12 September 2024 Category 6™ Weather Underground 5 January 2009 immense property damage occurred in Thandwe and Kyaukphyu.India Weather Review 1936 4 Many villages along the coast were destroyed either due to the cyclone's winds or storm surge.India Weather Review 1936 4 Over 150,000 were affected by the resulting flooding that came from it.MYANMAR 2014 National Institute of Disaster Management 6 https://nidm.gov.in/easindia2014/err/pdf/country_profile/Myanmar.pdf 12 September 2024 In some villages, torrential rainfall destroyed all of the grain that was stored while thousands of cattle were lost. Initial reports also stated that more than due to the cyclone, over 1000 people had died or drowned,India Weather Review 1936 5 however, a 2006 report by Jeff Masters of Wunderground stated that only 36 people were killed. Very Severe Cyclonic Storm Two NIO 02B 1936 path.png 22 May 29 May 65 979 On May 22, due to the southwest monsoon strengthening, an area of unsettled weather formed over the Bay of Bengal.India Weather Review 1936 5 Just a few hours later, this disturbance developed into a depression.India Weather Review 1936 5 However, further intensification was slow to occur, as it would not become a cyclonic storm until May 25.India Weather Review 1936 5 Paralleling the eastern coast of India as it recurved northwards prior to resuming its northeastward track a few days later, the next day, the cyclone peaked as a very severe cyclonic storm with sustained winds of 65 kn mph km/h out 5.1936 Severe Cyclonic Storm UNNAMED (1936144N14084) 2024 https://ncics.org/ibtracs/index.php?name=v04r01-1936144N14084 Gahtan J. 2024-09-12 Knapp K. R. National Centers for Environmental Information Schreck C. J. Diamond H. J. Kossin J. P. Kruk M. C. Despite weakening into a severe cyclonic stormIndia Weather Review 1936 5 as it made landfall along the coast of eastern India on May 27, it attained a minimum pressure of 979 hPa inHg at that time.India Weather Review 1936 5 Tracking northeastward after landfall, it weakened rapidly once inland, eventually dissipating over Mymensingh on May 29.India Weather Review 1936 6 Due to the cyclone, the southwest monsoon was able to establish itself in Northern India and Myanmar. As a result, torrential rainfall occurred, peaking with 21 in cm in Cherrapunji and 15 in cm in Shillong on May 29. Many rivers flooded, carrying away cattle and making many families homeless. Nearly every single building in Tura was damaged due to flooding as overflowing rivers caused many boats to be lost.India Weather Review 1936 6-7 Cyclonic Storm Three NIO 03B 1936 path.png 11 June 17 June 35 On June 10, an area of unsettled weather was first over the northern Bay of Bengal. Developing into a cyclonic circulation a few hours later, on June 11, this disturbance developed into a depression.India Weather Review 1936 8-9 As it tracked northwest towards India,https://ncics.org/ibtracs/index.php?name=v04r01-1936163N20089 1936 Cyclonic Storm UNNAMED (1936163N20089) Gahtan J. Knapp K. R. 2024 National Centers for Environmental Information Schreck C. J. Diamond H. J. Kossin J. P. Kruk M. C. 2024-09-12 it intensified into a deep depression a few hours later.India Weather Review 1936 9 As a result, prior to making landfall southeast of Balasore,India Weather Review 1936 9 it peaked as a minimal cyclonic storm early on June 13 with peak winds of 35 kn mph km/h out 5. However, once inland, it rapidly weakened, becoming a depression by June 14.India Weather Review 1936 9 The weakening depression would persist northwestwards, dissipating over Westcentral India on June 17.India Weather Review 1936 9 Due to the cyclone, the southwest monsoon was able to establish itself in North and Central India, causing torrential rainfall.India Weather Review 1936 9 As a result, a country boat travelling in the Gomal River capsized, causing 20 deaths.Boats Capsize In Rivers https://books.google.com/books?id=C8A-AAAAIBAJ 14 September 2024 224 The Indian Express 15 June 1936 8 en Locally heavy rain would also occur in the Central Provinces and Orissa, peaking in Kumhari, which received 11 in cm of rainfall.India Weather Review 1936 9 The cyclone, which at the time was expected to impact Mount Everest, prevented Hugh Ruttledge and his fellow climbers from successfully completing their expedition.Mountain Climbers Are Balked By Storm https://books.google.com/books?id=PLIhAAAAIBAJ Reading Eagle 12 June 1936 Front Cover en Depression Four NIO 04B 1936 path.png 25 June 28 June 25 ≤ On June 21, after temporarily weakening, the monsoon began strengthening over the Bay of Bengal. As a result, three days later, a trough of low pressure was first identified offshore Orissa and Ganjam. This trough would develop in favorable environmental conditions,India Weather Review 1936 10 becoming a depression on June 25.India Weather Review 1936 11 Deepening as it travelled near-stationary for the next few days, the depression finally made landfall near Balasore on June 28. Once inland, the depression rapidly weakened, dissipating just a few hours later.India Weather Review 1936 10 Cyclonic Storm Five NIO 28 June 4 July 45 On June 28, a land depression was first identified over the west Central Provinces.India Weather Review 1936 11 As it tracked northwestwards and then westwards,https://ncics.org/ibtracs/index.php?name=v04r01-1936180N23077 1936 Cyclonic Storm UNNAMED (1936180N23077) Gahtan J. Knapp K. R. 2024 National Centers for Environmental Information Schreck C. J. Diamond H. J. Kossin J. P. Kruk M. C. 2024-09-12 it began deepening over Deesa.India Weather Review 1936 11 As a result, early on July 1, it developed into a cyclonic storm over Badin,India Weather Review 1936 11 peaking with sustained winds of 45 kn mph km/h out 5 later that day. However, weakening soon commenced, and as it crossed into the Arabian Sea on July 2,India Weather Review 1936 11 it weakened into a deep depression. The weakening cyclone would traverse westwards prior to dissipating over Oman on July 4.India Weather Review 1936 11 Heavy rainfall associated with the storm caused three deaths in Ernakulam and uprooted several trees. Additionally, three country boats carrying merchandise were capsized.Storm Havoc In Ernakulam https://books.google.com/books?id=58A-AAAAIBAJ 16 September 2024 239 4 The Indian Express 1 July 1936 3 en Depression Six NIO 2 July 5 July 25 ≤ On June 30, a low-pressure area was first identified over Myanmar. Travelling eastwards, this disturbance would spawn an area of unsettled weather over the north and central Bay of Bengal.India Weather Review 1936 11 As a result of this, on July 2, a depression formed over the bay.India Weather Review 1936 12 Initially tracking north, after it made landfall between Balasore and Sagar Island the next day, it would begin tracking northwestwards instead. As a result, the weakening depression would persist until finally dissipating on July 5.India Weather Review 1936 12 Land Depression Seven NIO 7 July 11 July 25 ≤ On July 7, a land depression was first identified near Lucknow. This depression would slowly track southwestwards, deepening slightly due to the rains intensifying the monsoon over the United Provinces. However, two days later, it began tracking northwestwards, weakening steadily. As a result, it dissipated over Bareilly on July 11.India Weather Review 1936 12 Deep Depression Eight NIO 21 July 29 July 30 On July 20, a cyclonic circulation was first identified offshore Orissa. Developing, it soon became a depression the next day.India Weather Review 1936 12 Developing as it initially moved near-stationary,India Weather Review 1936 12 on 03:00 UTC that same day, it became a deep depression.1936 Depression UNNAMED (1936203N18087) 2024 https://ncics.org/ibtracs/index.php?name=v04r01-1936203N18087 Gahtan J. 2024-09-12 Knapp K. R. National Centers for Environmental Information Schreck C. J. Diamond H. J. Kossin J. P. Kruk M. C. Soon after, it tracked northwestwards, making landfall along the coast of Puri and Gopalpur two days later.India Weather Review 1936 12 Once inland, the depression slowly weakened as it tracked northwestwards,India Weather Review 1936 12 slowly tracking northwards prior to dissipating on July 29.India Weather Review 1936 12 Depression Nine NIO 17 August 18 August 25 ≤ On August 15, due to the strengthening monsoon, an area of unsettled weather formed in the northern Bay of Bengal. Developing offshore Odisha, two days later, the disturbance developed into a depression. Tracking northwards, after it made landfall near Chandabali on the evening of August 18, it rapidly weakened, dissipating soon after.India Weather Review 1936 13 Deep Depression Ten NIO 26 August 1 September 30 On August 25, an area of unsettled weather with a weak low-level circulation formed over the northern Bay of Bengal.India Weather Review 1936 13-14 Developing into a shallow depression early the next day, it initially stalled prior to deepening.India Weather Review 1936 14 As a result, as it tracked southwestwards prior to recurving on August 28,1936 Depression UNNAMED (1936239N19089) 2024 https://ncics.org/ibtracs/index.php?name=v04r01-1936239N19089 Gahtan J. 2024-09-12 Knapp K. R. National Centers for Environmental Information Schreck C. J. Diamond H. J. Kossin J. P. Kruk M. C. it peaked as a deep depression.India Weather Review 1936 14 However, as it neared the coast, the system weakened into a depression,India Weather Review 1936 14 prior to making landfall near Kalingapatnam on 03:00 UTC on August 29.India Weather Review 1936 14 Tracking northwestwards soon after, it persisted inland prior to dissipating on September 1.India Weather Review 1936 14 Depression Eleven NIO 5 September 9 September 25 ≤ On September 4, due to the strengthening monsoon, an area of unsettled weather formed in the northern Bay of Bengal. Developing into a depression a day later, it began tracking northwestwards. Never developing further, after it made landfall in Odisha on September 7, it kept moving northwestwards prior to being absorbed by a trough of low pressure over northern India.India Weather Review 1936 14 Depression Twelve NIO 29 September 1 October 25 ≤ On September 27, an area of unsettled weather was first identified over the Bay of Bengal. The next day, ship reports revealed that two cyclonic circulations had formed from this disturbance. Both developing into depressions on September 29, the former one would intensify further prior to making landfall in Tharrawaddy. Tracking northwestwards soon after, it would degenerate into a weak low-pressure area. Despite that it was able to retain its upper-level circulation.India Weather Review 1936 16 Very Severe Cyclonic Storm Thirteen 1936 Odisha cyclone NIO Very Severe Cyclonic Storm Thirteen 3 October 1936.png 11B 1936 path.png 29 September 7 October 65 986 On September 29, two depressions would form from an area of unsettled weather over the Bay of Bengal. While the former one would make landfall in Tharrawaddy and dissipate,India Weather Review 1936 16 the latter one would track northeastwards due to favorable upper-level conditions.India Weather Review 1936 17 As a result, on October 2, it would deepen into a deep depression, developing into a cyclonic storm a few hours later.India Weather Review 1936 17 Further developing, the next day, the system intensified into a severe cyclonic storm,India Weather Review 1936 20 peaking with sustained winds of 65 kn mph km/h out 5.1936 Severe Cyclonic Storm UNNAMED (1936273N15086) 2024 https://ncics.org/ibtracs/index.php?name=v04r01-1936273N15086 Gahtan J. 2024-09-12 Knapp K. R. National Centers for Environmental Information Schreck C. J. Diamond H. J. Kossin J. P. Kruk M. C. On 21:00 UTC that same day, the cyclone would make landfall alongside the coast of Odisha.India Weather Review 1936 20 Rapidly weakening once inland, by the next day, the cyclone had weakened into a deep depression, further weakening as it recurved northeastwards.India Weather Review 1936 20 It would finally dissipate over Bangladesh on October 7.India Weather Review 1936 20 Widespread rainfall from the cyclone affected Myanmar, Bangladesh, and portions of India, with the most concentrated amounts seeing in Odisha. As a result, extensive damage occurred in the state, with Cuttack alone seeing 300 homes collapsing.India Weather Review 1936 20 In Bangladesh, many areas in Noakhali District were inundated due to the cyclone's storm surge.Severe Cyclone on East Coast https://books.google.com/books?id=FME-AAAAIBAJ 19 September 2024 302 4 The Indian Express 5 October 1936 7 In West Bengal, the cyclone produced a tornado which capsized several country boats carrying jute.Severe Tornado and Cyclone https://books.google.com/books?id=FsE-AAAAIBAJ 19 September 2024 304 4 The Indian Express 7 October 1936 Front Cover en In total, the cyclone caused one death.Cyclone in Orrisa https://books.google.com/books?id=FsE-AAAAIBAJ 19 September 2024 304 4 The Indian Express 7 October 1936 5 en Cyclonic Storm Fourteen 1936 Andhra Pradesh cyclone NIO 25 October 31 October 45 On October 25, due to the northeast monsoon establishing itself, a cyclonic circulation developed in the southern Bay of Bengal.India Weather Review 1936 21 Developing into a depression later that day, the cyclone would develop into a cyclonic storm as it tracked north-northwestwardly.India Weather Review 1936 22 Soon after, it peaked with sustained winds of 45 kn mph km/h out 5 on October 27.Severe Cyclonic Storm UNNAMED (1936299N10088) 2024 https://ncics.org/ibtracs/index.php?name=v04r01-1936299N10088 Gahtan J. 2024-09-12 Knapp K. R. National Centers for Environmental Information Schreck C. J. Diamond H. J. Kossin J. P. Kruk M. C. Tracking northwestwardly for a while, it later made landfall near Machilipatnam on 06:00 UTC the next day.India Weather Review 1936 22 Weakening soon after, it became a deep depression over Hyderabad, finally dissipating over the Central Provinces on October 31.India Weather Review 1936 22 Severe rainfall from the cyclone caused immense damage in Andhra Pradesh. Many villages were either inundated or collapsed due to heavy rainfall, causing thousands to become homeless. In Chirala, the tobacco factory sustained 2 lakh rupees ($75,000) in damage.India Weather Review 1936 22Measures of worth, inflation rates, saving calculator, relative value, worth of a dollar, worth of a pound, purchasing power, gold prices, GDP, history of wages, average wage https://www.measuringworth.com/datasets/exchangeglobal/result.php?year_source=1916&year_result=1948&countryE[]=India Measuring Worth 19 September 2024 In total, the storm killed 233 people in India.ADRC 20th Century Asian Natural Disasters Data Book August 2002 Asian Disaster Reduction Center 8 https://www.adrc.asia/publications/databook/ORG/databook_20th/IND.pdf 15 September 2024 Top 25 Natural Disasters in India according to Number of Killed (1901-2000) In the storm's aftermath, Mahatma Gandhi visited flooded areas to bring help pay for flood relief.Akbar Syed When Mahatma Gandhi toured Andhra Pradesh to raise cyclone relief fund https://timesofindia.indiatimes.com/city/hyderabad/when-gandhi-toured-ap-to-raise-cyclone-relief-fund/articleshow/71412603.cms 15 September 2024 The Times of India 3 October 2019 Deep Depression Fifteen NIO 3 November 15 November 30 1005 On November 1, a low-pressure area formed near the eastern coast of Sri Lanka. Developing further, as it tracked into the Arabian Sea two days later, it became a depression. Tracking westwards and then northwestwards, on November 6, the depression intensified further, becoming a deep depression.India Weather Review 1936 23 Further deepening as it tracked northwards towards the coast of Gujarat, it attained a minimum pressure of 1005 hPa inHg on November 12. However, soon after, it rapidly weakened, dissipating on November 15 over Kutch.India Weather Review 1936 23 Depression Sixteen NIO 13B 1936 path.png 4 November 7 November 25 ≤ On November 3, an area of unsettled weather formed in the southern Bay of Bengal, developing into a depression early the next day. Never intensifying further, the depression would track northwestwardly and then west-northwestwardly prior to weakening four days later. It soon made landfall along the coast of Chennai, dissipating a few hours later.India Weather Review 1936 24-25 Depression Seventeen NIO 14B 1936 path.png 2 December 4 December 25 ≤ From November 28–30, a low-pressure area in the Gulf of Thailand would produce convective activity in the Andaman Sea. As it passed through Thailand and entered the Andaman Sea on December 1, it would produce an area of unsettled weather which developed into a depression early the next day. Never intensifying further, the depression degenerated into a trough of low pressure on December 4. This remnant trough would persist prior to dissipating two days later.India Weather Review 1936 25-26 Depression Eighteen NIO 15B 1936 path.png 30 December 31 December 25 ≤ On December 30, an area of unsettled weather formed offshore Sri Lanka over the southwest Bay of Bengal, developing into a depression a few hours later. Never intensifying further, the depression would track southwesterly into the Arabian Sea prior to degenerating into a low-pressure area early the next day.India Weather Review 1936 26 Other systems According to IBTrACS, on July 2, a tropical cyclone formed in the border of India and Pakistan. Crossing into the Arabian Sea the next day, it dissipated.1936 UNNAMED (1936177N21088) 2024 https://ncics.org/ibtracs/index.php?name=v04r01-1936177N21088 Gahtan J. 2024-09-12 Knapp K. R. National Centers for Environmental Information Schreck C. J. Diamond H. J. Kossin J. P. Kruk M. C. According to IBTrACS, on July 15, a depression with sustained winds of 25 kn mph km/h out 5 formed in modern-day Pakistan. Crossing into the Arabian Sea the next day, it dissipated.1936 Depression UNNAMED (1936197N24069) 2024 https://ncics.org/ibtracs/index.php?name=v04r01-1936197N24069 Gahtan J. 2024-09-12 Knapp K. R. National Centers for Environmental Information Schreck C. J. Diamond H. J. Kossin J. P. Kruk M. C. Bibliographies India Weather Review India Meteorological Department National Oceanic and Atmospheric Administration 1936 September 2, 2024 Annual Summary — Storms & Depressions ftp://ftp.library.noaa.gov/docs.lib/htdocs/rescue/cd019_pdf/00462956.pdf https://web.archive.org/web/20190614094801/ftp://ftp.library.noaa.gov/docs.lib/htdocs/rescue/cd019_pdf/00462956.pdf dead 2019-06-14 India Weather Review 1936 Wahiduzzaman Md Oliver Eric C. J. Wotherspoon Simon J. Luo Jing-Jia Seasonal forecasting of tropical cyclones in the North Indian Ocean region: the role of El Niño-Southern Oscillation Climate Dynamics February 2020 54 3-4 1571–1589 10.1007/s00382-019-05075-7 Climate Dynamics 2020 Season effects This is a table of all storms in the 1936 North Indian Ocean cyclone season. It mentions all of the season's storms and their names, duration, peak intensities according to the IMD storm scale, damage, and death totals. Damage and death totals include the damage and deaths caused when that storm was a precursor wave or extratropical low. All of the damage figures are in 1936 USD. 1936 |- | One || 01 April 22 – 26 || bgcolor=#VSCS|4 Very severe cyclonic storm || bgcolor=#VSCS|65 kn km/h mph 5 out on on || bgcolor=#VSCS| 993 off hPa inHg 4 on|| Myanmar || 0 $ Unknown || 36 || |- | Two || 02 May 22 – 29 || bgcolor=#VSCS|4 Very severe cyclonic storm || bgcolor=#VSCS|65 kn km/h mph 5 out on on || bgcolor=#VSCS| 979 off hPa inHg 4 on|| Myanmar, Bangladesh, North India || 0 $ Unknown || None || |- | Three || 03 June 11 – 17 || bgcolor=#CS|2 Cyclonic storm || bgcolor=#CS|35 kn km/h mph 5 out on on || bgcolor=#CS| Not specified || North India, Central India, Bangladesh || 0 $ Unknown || 20 || |- | Four || 04 June 25 – 28 || bgcolor=#niodepression|0 Depression || bgcolor=#niodepression|≤25 kn km/h mph 5 out on on || bgcolor=#niodepression| Not specified || Myanmar || 0 $ Unknown || None || |- | Five || 05 June 28 – July 4 || bgcolor=#CS|2 Cyclonic storm || bgcolor=#CS|45 kn km/h mph 5 out on on || bgcolor=#CS| Not specified || India (primarily Gujarat and Kerala), Pakistan, Oman || 0 $ Unknown || 3 || |- | Six || 06 July 2 – 5 || bgcolor=#niodepression|0 Depression || bgcolor=#niodepression|≤25 kn km/h mph 5 out on on || bgcolor=#niodepression| Not specified || Myanmar, West Bengal || 0 $ Unknown || None || |- | Seven || 07 July 7 – 11 || bgcolor=#niodepression|0 Depression || bgcolor=#niodepression|≤25 kn km/h mph 5 out on on || bgcolor=#niodepression| Not specified || North India || 0 $ Unknown || None || |- | Eight || 08 July 21 – 29 || bgcolor=#DD|1 Deep depression || bgcolor=#DD|30 kn km/h mph 5 out on on || bgcolor=#DD| Not specified || India || 0 $ Unknown || None || |- | Nine || 09 August 17 – 18 || bgcolor=#niodepression|0 Depression || bgcolor=#niodepression|≤25 kn km/h mph 5 out on on || bgcolor=#niodepression| Not specified || East India (primarily Odisha), Myanmar (primarily Rakhine) || 0 $ Unknown || None || |- | Ten || 10 August 26 – September 1 || bgcolor=#DD|1 Deep depression || bgcolor=#DD|30 kn km/h mph 5 out on on || bgcolor=#DD| Not specified || North India (primarily Odisha and Andhra Pradesh), Myanmar || 0 $ Unknown || None || |- | Eleven || 11 September 5 – 9 || bgcolor=#niodepression|0 Depression || bgcolor=#niodepression|≤25 kn km/h mph 5 out on on || bgcolor=#niodepression| Not specified || East India (primarily Odisha), North India || 0 $ Unknown || None || |- | Twelve || 12 September 29 – October 1 || bgcolor=#niodepression|0 Depression || bgcolor=#niodepression|≤25 kn km/h mph 5 out on on || bgcolor=#niodepression| Not specified || Myanmar || 0 $ Unknown || None || |- | Thirteen || 12 September 29 – October 7 || bgcolor=#VSCS|4 Very severe cyclonic storm || bgcolor=#VSCS|65 kn km/h mph 5 out on on || bgcolor=#VSCS| 986 off hPa inHg 4 on|| Myanmar, Odisha, West Bengal, Bangladesh || 0 $ Unknown || 1 || |- | Fourteen || 13 October 25 – 31 || bgcolor=#CS|2 Cyclonic storm || bgcolor=#CS|45 kn km/h mph 5 out on on || bgcolor=#CS| Not specified || India (primarily Andhra Pradesh) || 1 75000 $ $75,000 || 233 ||India Weather Review 1936 22 |- | Fifteen || 14 November 3 – 15 || bgcolor=#DD|1 Deep depression || bgcolor=#DD|30 kn km/h mph 5 out on on || bgcolor=#DD| 1005 off hPa inHg 4 on|| Sri Lanka, West India (primarily Gujarat) || 0 $ Unknown || None || |- | Sixteen || 15 November 4 – 7 || bgcolor=#niodepression|0 Depression || bgcolor=#niodepression|≤25 kn km/h mph 5 out on on || bgcolor=#niodepression| Not specified || Tamil Nadu || 0 $ Unknown || None || |- | Seventeen || 16 December 2 – 4 || bgcolor=#niodepression|0 Depression || bgcolor=#niodepression|≤25 kn km/h mph 5 out on on || bgcolor=#niodepression| Not specified || Thailand, Andaman Islands || 0 $ Unknown || None || |- | Eighteen || 17 December 30 – 31 || bgcolor=#niodepression|0 Depression || bgcolor=#niodepression|≤25 kn km/h mph 5 out on on || bgcolor=#niodepression| Not specified || Sri Lanka || 0 $ Unknown || None || |- 18 systems April 22 – December 31 65 kn km/h mph 5 out on on 979 off hPa inHg 4 on 1 75000 $ $75,000 293 See also Tropical cyclones in 1936 1936 Atlantic hurricane season 1936 Pacific hurricane season 1936 Pacific typhoon season 1930s Australian region cyclone seasons 1900–1940 South Pacific cyclone seasons 1900–1950 South-West Indian Ocean cyclone seasons References 1936 Category:North Indian Ocean cyclone seasons Category:Tropical cyclones in 1936 Category:Meteorological events in 1936