1977 Andhra Pradesh cyclone

From Wikipedia, the free encyclopedia
Jump to navigation Jump to search
1977 Andhra Pradesh cyclone
Super cyclonic storm (IMD scale)
Category 3 tropical cyclone (SSHWS)
Satellite image of the storm on 19 November, prior to making landfall in Andhra Pradesh
Formed14 November 1977 (1977-11-14)
Dissipated21 November 1977 (1977-11-21)
(Remnant low after 20 November 1977 (1977-11-20))
Highest winds3-minute sustained: 250 km/h (155 mph)
1-minute sustained: 205 km/h (125 mph)
Lowest pressure919 hPa (mbar); 27.14 inHg
Fatalities10,000 (official)
(Estimated up to 50,000)
Damage$196.29 million (1977 USD)
Areas affectedAndhra Pradesh
Part of the 1977 North Indian Ocean cyclone season

The 1977 Andhra Pradesh cyclone was a devastating tropical cyclone that hit Andhra Pradesh in November 1977, killing at least 10,000 people.[1]

Meteorological History[edit]

Map plotting the track and the intensity of the storm, according to the Saffir–Simpson scale

The origins of the 1977 Andhra Pradesh cyclone can be traced to a weak tropical disturbance which was first noted on satellite imagery on the morning of 14 November while located roughly 520 km (320 mi) southwest of the Nicobar Islands.[nb 1][2] Traveling due west at 25 km/h (15 mph) along the southern periphery of the mid-tropospheric subtropical ridge, the disturbance steadily organized, with increased banding noted on satellite imagery. This increase in organization prompted the India Meteorological Department (IMD) to report that the disturbance had intensified into a deep depression later that morning,[nb 2][4] and the Joint Typhoon Warning Center (JTWC) to issue a Tropical Cyclone Formation Alert for the system at 1310 UTC that afternoon.[nb 3] At 0800 UTC on 15 November, the JTWC issued its first advisory on the system as satellite data indicated that the storm had continued to strengthen, with estimated one-minute sustained wind speeds of 75 km/h (45 mph).[2]

While the system was initially developing, an upper tropospheric trough had formed over northern and central India and produced a break in the subtropical ridge. As the storm traveled towards this break in the ridge on 15 November, the mid-tropospheric anticyclone over the system weakened, reducing the storm's steering flow and causing the system to slow to a 7 km/h (5 mph) northwestwards movement. In addition, the divergent southwesterly flow produced by the trough resulted in the system beginning a period of rapid intensification. Early on 16 November, the system intensified into a Category 1-equivalent tropical cyclone on the Saffir-Simpson Hurricane Scale; an eye was observed on satellite imagery later that morning.[2]

Satellite image of the cyclone at peak intensity on 18 November

For the next two days, the tropical cyclone continued to strengthen while traveling generally towards the north-northwest. During this time period, increased organization, such as tighter banding features and a progressively more distinct eye, were observed on satellite imagery. At 1030 UTC on 17 November, the ship Jagatswami reported winds of 190 km/h (120 mph) and a minimum barometric pressure of 941 hPa (27.79 inHg) off the Indian coast.[6][7] The next evening, the JTWC estimated that the system had attained its peak intensity as a Category 3-equivalent tropical cyclone, with one-minute sustained winds of 200 km/h (125 mph), while located roughly 140 km (85 mi) off the coast of Andhra Pradesh.[2] Around this time, the IMD estimated that the system had three-minute sustained winds of 250 km/h (155 mph)—which would classify the system as a modern-day super cyclonic storm—and a minimum barometric pressure of 919 hPa (27.14 inHg).[4][8][9] This barometric pressure made the cyclone the most intense ever recorded in the North Indian Ocean at the time; the 1991 Bangladesh cyclone and the 1999 Odisha cyclone would both subsequently produce lower barometric pressures.[7]

As the cyclone approached the Indian coast, it accelerated to 17 km/h (10 mph) while slightly weakening from its peak intensity. The storm made landfall near Chirala, in the Prakasam district of central Andhra Pradesh, around 1100 UTC on 19 November with one-minute sustained winds of 195 km/h (120 mph). Moving northwards over flat agricultural lands, the storm weakened, with the JTWC issuing its final warning at 2000 UTC that evening.[2] The IMD continued tracking the system, reporting that it weakened into an area of low pressure on the evening of 20 November before dissipating over southeastern Madhya Pradesh and Odisha the next evening.[6]


The worst affected areas were in the Krishna River delta region. The island of Diviseema, which was hit by a six-metre-high (20 ft) storm surge, experienced a loss of life running into the thousands. Hundreds of bodies were floating in the waters and bodies bloated beyond recognition were consigned to mass pyres. Landslides ripped off the railway lines in the Waltair-Kirandal route. About 100 people who had left their homes to seek shelter in a church in Bapatla town were killed when the building collapsed. Fields of paddy and cash crops were submerged by the tidal waves. Thirteen sailing vessels, including some foreign ones, went missing in the storm.

About 100 villages were marooned or washed away by the cyclonic storms and the ensuing floods and a total of 10,841 killed or missing, and 34 lakh rendered homeless. According to the Janata party, at least 50,000 people were believed to have been killed by the storm, substantially higher than reported by the government.[10]


The large loss of life prompted the establishment of early warning meteorological stations on the coast of Andhra Pradesh. Cyclone shelters and other measures for disaster management were also taken. A memorial, at the point of furthest advance of the tidal wave, near the town of Avanigadda, was built in memory of the people who died in the storm.

The next cyclone (1990) that also occurred in Andhra Pradesh, showed that there was a large improvement in disaster management, effective warnings ahead of time, and better meteorological equipment which dramatically reduced the death rate (compared to the cyclone in 1977).[7]

In the wake of the disaster, officials in India were accused of covering up the scale of damage and loss of life. Members of the Janata party, an opposing political group to the state government in place at the time, claimed that the cover up was to hide criminal negligence which resulted in tens of thousands of fatalities.[10] Following these accusations, five high-ranking government officials resigned from their positions.[11]

See Also[edit]


  1. ^ All dates are based on Coordinated Universal Time unless otherwise noted.
  2. ^ The India Meteorological Department is the official Regional Specialized Meteorological Center for the northern Indian Ocean.[3]
  3. ^ The Joint Typhoon Warning Center is a joint United States Navy – United States Air Force task force that issues tropical cyclone warnings for the western Pacific Ocean and other regions.[5]


  1. ^ The storm in Orissa. Economist, 00130613, 11/6/1999, Vol. 353, Issue 8144
  2. ^ a b c d e Morford, Dean R.; Lavin, James K. (1978). 1977 Annual Typhoon Report (PDF). Naval Oceanography Operations Command (Report). Guam, Mariana Islands, United States: Joint Typhoon Warning Center. pp. 51–54. Retrieved 2 March 2019.
  3. ^ "RSMCs and TCWCs". World Meteorological Organization. 2011. Retrieved 2 March 2019.
  4. ^ a b Johns, B.; Dube, S. K.; Mohanty, U. C.; Sinha, P. C. (October 1981). "Numerical simulation of the surge generated by the 1977 Andhra cyclone". Quarterly Journal of the Royal Meteorological Society. 107 (454): 919–934. doi:10.1002/qj.49710745411.
  5. ^ "Joint Typhoon Warning Center Mission Statement". Joint Typhoon Warning Center. United States Navy. 2011. Archived from the original on 26 July 2007. Retrieved 2 March 2019.
  6. ^ a b India Meteorological Department. "Historical records of Severe Cyclones which formed in the Bay of Bengal and made landfall at the eastern coast of India during the period from 1970-1999". Archived from the original on 25 September 2014. Retrieved 2 March 2019.
  7. ^ G.S. Mandal & Akhilesh Gupta (1996). "The Wind Structure, Size and Damage Potential of Some Recent Cyclone of Hurricane Intensity in the North Indian Ocean". Advances in Tropical Meteorology. New Delhi, India: Indian Meteorological Society (50): 421.
  8. ^ "Cyclones, storm surges, floods, landslides" (PDF). Global Facility for Disaster Reduction and Recovery. September 2011. p. 9. Archived from the original (PDF) on 26 April 2012. Retrieved 2 March 2019.
  9. ^ a b The Associated Press (November 28, 1977). "Coverup alleged in India's cyclone disaster". Bangor Daily News. Retrieved November 14, 2010.
  10. ^ Staff Writer (December 2, 1977). "5 in India Resign Over Cyclone Aid". Los Angeles Times.