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Amphan Cyclone Image Courtesy: NASA, satellite image from MODIS onboard Aqua satellite |
Development:
For the development of a tropical cyclone, following conditions are to
be met:
- This type of storm typically
develops over oceans between 10° and 20° N and S latitudes and no closer
than 5° from the Equator.
- Tropical cyclones form over
the sea where a threshold sea surface temperature of ~26.5° Celsius is
reached.
- An unstable environmental
lapse rate is also required
- Weak winds with little
change in speed or direction with height are also needed
- The atmosphere must have a high-water
content through the bottom 5 km of the atmosphere.
Category:
To assess the intensity of tropical cyclones ranked on Saffir–Simpson scale which rank storms from category 1 (weak) to category 5 (devastating). Amphan has been ranked category 5. The intensity of a tropical cyclone is based on the central pressure of the storm, mean wind speed, and height of the accompanying sea-level rise. Further, Amphan has been classified as "Super Cyclone"; cyclones in the North Indian Ocean with winds surpassing 220 kilometers per hour are considered “super cyclonic”—the highest classification in the north Indian basin. On May 18, Amphan sustained winds of 265 km per hour. Amphan and, the last super cyclonic storm recorded was Odisha in 1999.
Track of Amphan:
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