Explained: ‘NISARGA’ And Everything You Need To Know About Tropical Cyclones

by Swarajya Staff - Jun 4, 2020 04:54 PM +05:30 IST
Explained: ‘NISARGA’ And Everything You Need To Know About Tropical CyclonesCyclone Nisarga (Source: @SriyanshiP/Twitter)

Yesterday (3 June), cyclone NISARGA reached Maharashtra and the resulting landfall caused heavy rains and gusty wind, TOI reported.

The cyclone hit Mumbai and was expected to move towards Thane and Palghar, but it curved to east towards Pune.

Strong winds and rain were also witnessed in Kutch district, Gujarat.

By the late evening, Indian Meteorological Department said that the 'Nisarga' was moving north-east and likely to impact Nashik, Dhule and Nandurbar districts, which witnessed showers with gusty winds.

Around ten in the night, the severe cyclonic storm ‘Nisarga’ had weakened into a cyclonic storm near Pune. It further weakened into a deep depression over west Vidarbha region around noon today.

How are cyclones formed?

There are broadly two types of cyclones — temperate and tropical.

The temperate cyclones are formed in the middle and high latitudes (35° to 65°) in both the hemispheres due to complex interaction of air masses of different temperatures (hot and cold).

These air masses don’t just bump into each other head-on, but under the influence of Coriolis force — the force exerted due to the rotation of the earth. This interaction often results in formation of heavy-rain causing clouds and strong winds.

Temperate cyclones can form over both sea and land, however, tropical cyclones can only form over the sea.

The formation of the tropical cyclones is temperature driven. They are rapidly rotating violent storms driven by the heat energy with a closed low-pressure centre and steep pressure gradients.

Source: pmfias.com
Source: pmfias.com

Oceans having water temperature higher than 27 °C and sufficient depth of the warm water serve as the source of this heat energy.

A low pressure centre develops on the ocean with rapidly converging winds from all directions. Under the influence of the Coriolis force, the winds carry out cyclonic motions around the centre where hot moist air rapidly moves upwards.

With upward movement, this hot air cools down, and the released latent heat of condensation drives the storm. This is why cyclonic storms become weaker after they hit the ground — there is no more warm water and the latent heat of condensation.

Cyclones this time of the year and hitting Maharashtra are uncommon, then why this year?

As compared to Bay of Bengal, the Arabian Sea is much much less prone to cyclones. The ratio is 4:1. This is because:

  • Bay of Bengal also sees remnants of typhoons over Northwest Pacific that move across south China
  • The Arabian Sea is cooler than Bay of Bengal by 1-2 °C because of the monsoon winds
  • The monsoon winds constantly drive away the moisture of Arabian Sea towards India
  • The Arabian Sea also has higher salinity than the Bay of Bengal as comparatively less fresh water comes to it from rivers; and high salinity reduces rate of evaporation
  • High Salinity in Arabian sea also increases vertical mixing (because of density), while cyclone requires a deep enough layer of warm water

However, last year, the Arabian Sea saw the most frequent and intense cyclonic activity in more than 100 years. Five cyclones originated in the area in 2019 — Vayu, Hikka, Kyarr, Maha and Pavan – as opposed to the normal of one or two.

Last year, scientists had identified El Nino-Modoki conditions prevailing in the tropical Pacific when the central region of the ocean warms up more than usual. El Nino Modoki years are conducive for cyclone formation over the Arabian Sea.

Scientists at IMD said that a strong Indian Ocean dipole supported the cyclone formation by warming the west Indian Ocean and Arabian Sea. The cross equatorial also aided the formation of cyclones.

What determines the path of a cyclone?

Tropical cyclones generally follow a parabolic path. Coriolis force and different types of winds (easterlies etc.) affect the path of the cyclone.

In the northern hemisphere, tropical cyclones generally start with a westward movement under the influence of easterly winds, and turn northward at around 20° latitude and further north-eastwards at around 25° latitude under the influence of Coriolis force.

At around 30° latitude, they turn eastward because of westerly winds. Beyond this, cyclones encounters cooler waters and subside.

A tropical cyclone may also continue moving westward instead of turning east (Cyclone Gaja in 2017, for example, crossed over from Tamil Nadu coast to Arabian Sea).

Are all cyclones dangerous?

Cyclones bring with them strong winds, heavy rains and large storm surges that eventually lead to loss of life and property.

The IMD categorises the cyclones as follows:

Source: www.rsmcnewdelhi.imd.gov.in
Source: www.rsmcnewdelhi.imd.gov.in

Cyclone Amphan that hit West Bengal, Odisha and Bangladesh weeks ago was classified as a super cyclone. A super cyclone causes extensive structural damage, potential damage to power and communication infrastructure and total suspension of fishing operations.

Cyclone Nisarga at Maharashtra coast was classified as a severe cyclonic storm by the IMD.

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