Social Sciences, asked by vidhitandon27, 2 months ago

study the impact of cyclone in Odisha that occurred in the year 1999 and find out other such events.​

Answers

Answered by scarlet02
4

Answer:

The 1999 Odisha cyclonewas the most intense recorded tropical cyclone in the North Indian Ocean and among the most destructive in the region.The 1999 Odisha cyclone organized into a tropical depression in the Andaman Sea on 25 October, though its origins could be traced back to an area of convection in the Sulu Sea four days prior. The disturbance gradually strengthened as it took a west-northwesterly path, reaching cyclonic storm strength the next day. Aided by highly favorable conditions, the storm rapidly intensified, attaining super cyclonic storm intensity on 28 October, before peaking on the next day with winds of 260 km/h (160 mph) and a record-low pressure of 912 mbar. The storm maintained this intensity as it made landfall on Odisha on 29 October. The cyclone steadily weakened due to persistent land interaction and dry air, remaining quasi-stationary for two days before slowly drifting offshore as a much weaker system; the storm dissipated on 4 November over the Bay of Bengal. Although its primary effects were felt in a localized area of India, the outer fringes of the super cyclone impacted Myanmar and Bangladesh. Ten people were killed in the former, while two were killed in the latter by the storm's rainbands. The storm was the most severe to strike Odisha in the 20th century, raking the state and adjacent areas with high storm surge, powerful winds, and torrential rainfall. The storm's impacts exacerbated the damage caused by a very severe cyclone that struck the same region less than two weeks earlier. The 5–6 m (16–20 ft) surge brought water up to 35 km (20 mi) inland, carrying along with it coastal debris and inundating towns and villages. The surge combined with heavy rains to produce widespread flooding, damaging around 1.6 million homes and causing rivers to breach 20,005 flood embankments. The storm's effects destroyed numerous crops, including sugar cane, rice, and other winter-time harvests. Although estimates of the death toll varied significantly—at times suggesting 30,000 fatalities—the Government of India enumerated 9,887 fatalities in the country, of which a majority were caused by storm surge; over 8,000 deaths occurred in Jagatsinghpur. The total damage cost of the destruction wrought by the super cyclone amounted to US$4.44 billion.

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Answered by AneesKakar
0

The impact of the Paradip Cyclone was devastating to the land of Odhisa and also caused significant damages in neighboring Bangladesh and Myanmar.

  • The 1999 Odisha cyclone was the most intense recorded tropical cyclone in the North Indian Ocean and among the most destructive in the region.
  • The storm was the most severe to strike Odisha in the 20th century, raking the state and adjacent areas with high storm surges, powerful winds, and torrential rainfall.
  • Often termed as the black Friday tragedy, the cyclone flattened lakhs of houses, uprooted trees, and destroyed infrastructure. Thousands of livestock were killed, paddy and other crop fields were submerged and hundreds of people were affected by the disaster.
  • Life in coastal Orissa was brought to a standstill. Large areas along the coastline were inundated. The cyclone destroyed or caused damage to lives and properties in the coastal districts such as Balasore, Bhadrak, Kendrapara, Jagatsinghpur, Puri, and Ganjam.
  • Although estimates of the death toll varied significantly—at times suggesting 30,000 fatalities—the Government of India enumerated 9,887 fatalities in the country, of which a majority were caused by storm surges; over 8,000 deaths occurred in Jagatsinghpur.
  • The surge combined with heavy rains produced widespread flooding, damaging around 1.6 million homes and causing rivers to breach 20,005 flood embankments. The storm's effects destroyed numerous crops, including sugar cane, rice, and other winter-time harvests.
  • The 1999 Odisha cyclone organized into a tropical depression in the Andaman Sea on 25th October, though its origins could be traced back to an area of convection in the Sulu Sea four days prior. The disturbance gradually strengthened as it took a west-northwesterly path, reaching cyclonic storm strength the next day.
  • Aided by highly favorable conditions, the storm rapidly intensified, attaining super cyclonic storm intensity on 28 October, before peaking on the next day with winds of 260 km/h (160 mph) and a record-low pressure of 912 mbar.
  • The storm maintained this intensity as it hit on Odisha on 29 October. The cyclone steadily weakened due to persistent land interaction and dry air, remaining quasi-stationary for two days before slowly drifting offshore as a much weaker system; the storm dissipated on 4 November over the Bay of Bengal.
  • The storm's impacts exacerbated the damage caused by a very severe cyclone that struck the same region less than two weeks earlier. The 5–6 m (16–20 ft) surge brought water up to 35 km (20 mi) inland, carrying along with it coastal debris and inundating towns and villages.
  • Although its primary effects were felt in a localized area of India, the outer fringes of the supercyclone impacted Myanmar and Bangladesh. Ten people were killed in the former, while two were killed in the latter by the storm's rainbands.
  • The total damage cost of the destruction wrought by the supercyclone amounted to US$4.44 billion.

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