Cyclone Michaung
Cyclone
Michaung
Why
in News:
The
India Meteorological Department (IMD) has issued an “orange” alert for Tamil
Nadu and coastal and interior Andhra Pradesh due to the potential landfall of
cyclone Michaung.
About
Cyclone Michaung
·
Uncommon Intensity:
December cyclones in the North Indian Ocean typically do not reach high
intensities. Michaung, with its severe storm classification, is an exception.
·
Upgraded Intensity:
Initially predicted as a tropical cyclone, IMD upgraded Michaung to a ‘severe’
storm due to its unexpected intensification.
·
Heat Index Contribution:
The intensification is attributed to the above-normal heat index values off the
southern Andhra Pradesh coast.
Cyclone:
·
It is a large-scale
system of air that rotates around the centre of a low-pressure area.
·
It is usually accompanied
by violent storms and bad weather.
·
As per the National
Disaster Management Authority (NDMA)-
·
A cyclone is
characterised by inward spiralling winds that rotate anticlockwise in the
northern hemisphere and clockwise in the southern hemisphere.
·
It classifies cyclones
broadly into two categories: tropical cyclones and extratropical cyclones.
Tropical
cyclones:
·
These develop in the
regions between the Tropics of Capricorn and Cancer.
·
They are the most
devastating storms on Earth.
·
According to the US
National Oceanic and Atmospheric Administration (NOAA)-
·
Such cyclones develop
when thunderstorm activity starts building close to the centre of circulation,
and the strongest winds and rain are no longer in a band far from the centre.
·
The storm's core turns
warm, and the cyclone gets most of its energy from the “latent heat” released
when water vapour that has evaporated from warm ocean waters condenses into
liquid water.
·
Warm fronts or cold
fronts are not associated with tropical cyclones.
·
Tropical cyclones have
different names depending on their location and strength.
·
For instance, they are
known as hurricanes in the Caribbean Sea, the Gulf of Mexico, the North
Atlantic Ocean and the eastern and central North Pacific Ocean. In the western
North Pacific, they are called typhoons.
·
The conditions favourable
for the formation and intensification of tropical storms are -
·
Large sea surface with a
temperature higher than 27° C.
·
Presence of the Coriolis
force.
·
Small variations in the
vertical wind speed.
·
A pre-existing weak
low-pressure area or low-level-cyclonic circulation.
·
Upper divergence above
the sea level system.
Extratropical
cyclones:
·
Also known as
mid-latitude cyclones, extratropical cyclones occur outside the tropics, i.e.,
beyond the areas that fall under the Tropic of Cancer and the Tropic of
Capricorn.
·
According to the US
National Oceanic and Atmospheric Administration (NOAA)-
·
They have cold air at
their core and derive energy from releasing potential energy when cold and warm
air masses interact.
·
Such cyclones always have
one or more fronts connected to them.
·
A front is a weather
system that is the boundary between two kinds of air masses, where one front is
represented by warm air and the other by cold air.
·
Such cyclones can occur
over land and ocean
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