| Basin: | NIO |
| Year: | 1960 |
| First Storm Formed: | April 22, 1936 |
| Last Storm Dissipated: | December 31, 1936 |
| Strongest Storm Name: | Two |
| Strongest Storm Winds: | 65 |
| Strongest Storm Pressure: | 979 |
| Average Wind Speed: | 3 |
| Total Disturbances: | 20 (18 official, 2 unofficial) |
| Total Depressions: | 8 |
| Total Storms: | 6 |
| Total Hurricanes: | 3 |
| Total Intense: | 3 |
| Fatalities: | 293 total |
| Damages: | 0.075 |
| Damagespre: | > |
| Five Seasons: | 1934, 1935, 1936, 1937, 1938 |
| Atlantic Season: | 1936 Atlantic hurricane season |
| East Pacific Season: | 1936 Pacific hurricane season |
| West Pacific 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.
bar:Month width:5 align:center fontsize:S shift:(0,-20) anchor:middle color:canvas from:01/04/1936 till:30/04/1936 text:April from:01/05/1936 till:31/05/1936 text:May from:01/06/1936 till:30/06/1936 text:June from:01/07/1936 till:31/07/1936 text:July from:01/08/1936 till:31/08/1936 text:August from:01/09/1936 till:30/09/1936 text:September from:01/10/1936 till:31/10/1936 text:October from:01/11/1936 till:30/11/1936 text:November from:01/12/1936 till:31/12/1936 text:December from:01/01/1937 till:30/01/1937 text:Jan' 1937
The 1936 North Indian Ocean cyclone season took place during the neutral phase of the El Niño–Southern Oscillation,[1] which is correlated with less activity in the basin. Additionally, ENSO-neutral conditions are also correlated to a higher chance of landfall in the eastern coast of India, hence the fact that a majority of the systems impacted land. 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.
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. A month after that system dissipated, another very severe cyclonic storm formed in late May, making landfall in East India prior to dissipating. Three depressions would form in June, with two developing into cyclonic storms. In July, three depressions would form, with one of them developing into a deep depression prior to dissipating. In August, two systems would form, with one of them becoming a deep depression prior to making landfall in Andhra Pradesh. September would feature three systems. The first and second systems, weak depression, would not be of much importance. However, the third system would peak as a very severe cyclonic storm prior to striking Odisha in early October. In October, only one system, a deadly cyclonic storm would form. However, November and December would be more active, featuring two depressions each. The last system, a weak depression offshore Sri Lanka, would form on December 30 and dissipate early the next day.
1936 Burma cyclone
| Basin: | NIO |
| Formed: | 22 April |
| Dissipated: | 26 April |
| 3-Min Winds: | 65 |
| Pressure: | 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. Further development occurred, and on 00:00 UTC the next day, the disturbance developed into a depression west of the Nicobar Islands.[2] Undergoing rapid intensification, by 12:00 UTC that same day, the cyclone had peaked as a very severe cyclonic storm with sustained winds of . It later attained a minimum pressure of at 21:00 UTC that day. Soon after, the cyclone recurved, with its intensity remaining the same as it tracked northeastward the next few days. At 03:00 UTC on April 26, the cyclone made its first landfall over Cheduba Island near peak intensity, producing intense winds there. Soon after, it made its second landfall along the coast of Myanmar, somewhere between Thandwe and Kyaukphyu. Rapidly weakening, it dissipated later that day.
The most intense storm to strike Myanmar prior to 1970,[3] immense property damage occurred in Thandwe and Kyaukphyu. Many villages along the coast were destroyed either due to the cyclone's winds or storm surge. Over 150,000 were affected by the resulting flooding that came from it.[4] 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, however, more modern reports stated that only 36 people had actually died.
| Basin: | NIO |
| Formed: | 22 May |
| Dissipated: | 29 May |
| 3-Min Winds: | 65 |
| Pressure: | 979 |
On May 22, due to the southwest monsoon strengthening, an area of unsettled weather formed over the Bay of Bengal. Just a few hours later, this disturbance developed into a depression. However, further intensification was slow to occur, as it would not become a cyclonic storm until May 25. 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 .[5] Despite weakening into a severe cyclonic storm as it made landfall along the coast of eastern India on May 27, it attained a minimum pressure of at that time. Tracking northeastward after landfall, it weakened rapidly once inland, eventually dissipating over Mymensingh on May 29.
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 in Cherrapunji and 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.
| Basin: | NIO |
| Formed: | 11 June |
| Dissipated: | 17 June |
| 3-Min Winds: | 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. As it tracked northwest towards India,[6] it intensified into a deep depression a few hours later. As a result, prior to making landfall southeast of Balasore, it peaked as a minimal cyclonic storm early on June 13 with peak winds of . However, once inland, it rapidly weakened, becoming a depression by June 14. The weakening depression would persist northwestwards, dissipating over Westcentral India on June 17.
Due to the cyclone, the southwest monsoon was able to establish itself in North and Central India, causing torrential rainfall. As a result, a country boat travelling in the Gomal River capsized, causing 20 deaths.[7] Locally heavy rain would also occur in the Central Provinces and Orissa, peaking in Kumhari, which received of rainfall. The cyclone, which at the time was expected to impact Mount Everest, prevented Hugh Ruttledge and his fellow climbers from successfully completing their expedition.[8]
| Basin: | NIO |
| Formed: | 25 June |
| Dissipated: | 28 June |
| 3-Min Winds: | 25 |
| Prewinds: | ≤ |
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, becoming a depression on June 25. 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.
| Basin: | NIO |
| Formed: | 28 June |
| Dissipated: | 4 July |
| 3-Min Winds: | 45 |
On June 28, a land depression was first identified over the west Central Provinces. As it tracked northwestwards and then westwards,[9] it began deepening over Deesa. As a result, early on July 1, it developed into a cyclonic storm over Badin, peaking with sustained winds of later that day. However, weakening soon commenced, and as it crossed into the Arabian Sea on July 2, it weakened into a deep depression. The weakening cyclone would traverse westwards prior to dissipating over Oman on July 4.
Heavy rainfall associated with the storm caused three deaths in Ernakulam and uprooted several trees. Additionally, three country boats carrying merchandise were capsized.[10]
| Basin: | NIO |
| Formed: | 2 July |
| Dissipated: | 5 July |
| 3-Min Winds: | 25 |
| Prewinds: | ≤ |
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. As a result of this, on July 2, a depression formed over the bay. 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.
| Basin: | NIO |
| Formed: | 7 July |
| Dissipated: | 11 July |
| 3-Min Winds: | 25 |
| Prewinds: | ≤ |
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.
| Basin: | NIO |
| Formed: | 21 July |
| Dissipated: | 29 July |
| 3-Min Winds: | 30 |
On July 20, a cyclonic circulation was first identified offshore Orissa. Developing, it soon became a depression the next day. Developing as it initially moved near-stationary, on 03:00 UTC that same day, it became a deep depression.[11] Soon after, it tracked northwestwards, making landfall along the coast of Puri and Gopalpur two days later. Once inland, the depression slowly weakened as it tracked northwestwards, slowly tracking northwards prior to dissipating on July 29.
| Basin: | NIO |
| Formed: | 17 August |
| Dissipated: | 18 August |
| 3-Min Winds: | 25 |
| Prewinds: | ≤ |
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.
| Basin: | NIO |
| Formed: | 26 August |
| Dissipated: | 1 September |
| 3-Min Winds: | 30 |
On August 25, an area of unsettled weather with a weak low-level circulation formed over the northern Bay of Bengal. Developing into a shallow depression early the next day, it initially stalled prior to deepening. As a result, as it tracked southwestwards prior to recurving on August 28,[12] it peaked as a deep depression. However, as it neared the coast, the system weakened into a depression, prior to making landfall near Kalingapatnam on 03:00 UTC on August 29. Tracking northwestwards soon after, it persisted inland prior to dissipating on September 1.
| Basin: | NIO |
| Formed: | 5 September |
| Dissipated: | 9 September |
| 3-Min Winds: | 25 |
| Prewinds: | ≤ |
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.
| Basin: | NIO |
| Formed: | 29 September |
| Dissipated: | 1 October |
| 3-Min Winds: | 25 |
| Prewinds: | ≤ |
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.
1936 Odisha cyclone
| Basin: | NIO |
| Track: | 11B 1936 path.png |
| Formed: | 29 September |
| Dissipated: | 7 October |
| 3-Min Winds: | 65 |
| Pressure: | 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, the latter one would track northeastwards due to favorable upper-level conditions. As a result, on October 2, it would deepen into a deep depression, developing into a cyclonic storm a few hours later. Further developing, the next day, the system intensified into a severe cyclonic storm, peaking with sustained winds of .[13] On 21:00 UTC that same day, the cyclone would make landfall alongside the coast of Odisha. Rapidly weakening once inland, by the next day, the cyclone had weakened into a deep depression, further weakening as it recurved northeastwards. It would finally dissipate over Bangladesh on October 7.
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. In Bangladesh, many areas in Noakhali District were inundated due to the cyclone's storm surge.[14] In West Bengal, the cyclone produced a tornado which capsized several country boats carrying jute.[15] In total, the cyclone caused one death.[16]
1936 Andhra Pradesh cyclone
| Basin: | NIO |
| Formed: | 25 October |
| Dissipated: | 31 October |
| 3-Min Winds: | 45 |
On October 25, due to the northeast monsoon establishing itself, a cyclonic circulation developed in the southern Bay of Bengal. Developing into a depression later that day, the cyclone would develop into a cyclonic storm as it tracked north-northwestwardly. Soon after, it peaked with sustained winds of on October 27.[17] Tracking northwestwardly for a while, it later made landfall near Machilipatnam on 06:00 UTC the next day. Weakening soon after, it became a deep depression over Hyderabad, finally dissipating over the Central Provinces on October 31.
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.[18] In total, the storm killed 233 people in India.[19] In the storm's aftermath, Mahatma Gandhi visited flooded areas to bring help pay for flood relief.[20]
| Basin: | NIO |
| Formed: | 3 November |
| Dissipated: | 15 November |
| 3-Min Winds: | 30 |
| Pressure: | 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. Further deepening as it tracked northwards towards the coast of Gujarat, it attained a minimum pressure of on November 12. However, soon after, it rapidly weakened, dissipating on November 15 over Kutch.
| Basin: | NIO |
| Formed: | 4 November |
| Dissipated: | 7 November |
| 3-Min Winds: | 25 |
| Prewinds: | ≤ |
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.
| Basin: | NIO |
| Formed: | 2 December |
| Dissipated: | 4 December |
| 3-Min Winds: | 25 |
| Prewinds: | ≤ |
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.
| Basin: | NIO |
| Formed: | 30 December |
| Dissipated: | 31 December |
| 3-Min Winds: | 25 |
| Prewinds: | ≤ |
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.
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.
|-| One || || bgcolor=#| || bgcolor=#|65kn || bgcolor=#| 993comma=off|| Myanmar || Unknown || 36 |||-| Two || || bgcolor=#| || bgcolor=#|65kn || bgcolor=#| 979comma=off|| Myanmar, Bangladesh, North India || Unknown || None |||-| Three || || bgcolor=#| || bgcolor=#|35kn || bgcolor=#| Not specified || North India, Central India, Bangladesh || Unknown || 20 |||-| Four || || bgcolor=#| || bgcolor=#|≤25kn || bgcolor=#| Not specified || Myanmar || Unknown || None |||-| Five || || bgcolor=#| || bgcolor=#|45kn || bgcolor=#| Not specified || India (primarily Gujarat and Kerala), Pakistan, Oman || Unknown || 3 |||-| Six || || bgcolor=#| || bgcolor=#|≤25kn || bgcolor=#| Not specified || Myanmar, West Bengal || Unknown || None |||-| Seven || || bgcolor=#| || bgcolor=#|≤25kn || bgcolor=#| Not specified || North India || Unknown || None |||-| Eight || || bgcolor=#| || bgcolor=#|30kn || bgcolor=#| Not specified || India || Unknown || None |||-| Nine || || bgcolor=#| || bgcolor=#|≤25kn || bgcolor=#| Not specified || East India (primarily Odisha), Myamnar (primarily Rakhine) || Unknown || None |||-| Ten || || bgcolor=#| || bgcolor=#|30kn || bgcolor=#| Not specified || North India (primarily Odisha and Andhra Pradesh), Myamnar || Unknown || None |||-| Eleven || || bgcolor=#| || bgcolor=#|≤25kn || bgcolor=#| Not specified || East India (primarily Odisha), North India || Unknown || None |||-| Twelve || || bgcolor=#| || bgcolor=#|≤25kn || bgcolor=#| Not specified || Myanmar || Unknown || None |||-| Thirteen || || bgcolor=#| || bgcolor=#|65kn || bgcolor=#| 986comma=off|| Myanmar, Odisha, West Bengal, Bangladesh || Unknown || 1 |||-| Fourteen || || bgcolor=#| || bgcolor=#|45kn || bgcolor=#| Not specified || India (primarily Andhra Pradesh) || $75,000 || 233 |||-| Fifteen || || bgcolor=#| || bgcolor=#|30kn || bgcolor=#| 1005comma=off|| Sri Lanka, West India (primarily Gujarat) || Unknown || None |||-| Sixteen || || bgcolor=#| || bgcolor=#|≤25kn || bgcolor=#| Not specified || Tamil Nadu || Unknown || None |||-| Seventeen || || bgcolor=#| || bgcolor=#|≤25kn || bgcolor=#| Not specified || Thailand, Andaman Islands || Unknown || None |||-| Eighteen || || bgcolor=#| || bgcolor=#|≤25kn || bgcolor=#| Not specified || Sri Lanka || Unknown || None |||-