Cyclone Dana

Context: The severe cyclonic storm Dana started landfall close to Bhitarkanika and Dhamara along the Odisha coast, the India Meteorological Department said.

Key facts about Cyclone Dana

Cyclone Dana
  • Six hours prior to the landfall, the outer layer of the cyclonic storm surrounded Odisha’s coastal region, causing widespread rain and wind. 
  • The Bay of Bengal had become turbulent with waves violently crashing on to the shore. 
  • Trees were uprooted and power infrastructure was hit at isolated places in Bhadrak and Kendrapara districts, while disaster response forces cautiously moved to remove obstructions on roads.
  • As a precautionary measure, the Odisha government had evacuated 5.84 lakh people to different cyclone shelters where food and other facilities were made available.

Tropical cyclone

A tropical cyclone is a type of low-pressure weather system that forms over tropical or subtropical waters. They are characterized by strong winds, heavy rainfall, and a low-pressure centre. Different names know tropical cyclones depending on their location, such as hurricanes in the Atlantic and north-eastern Pacific, Willy-willy in North West Australia, typhoons in the northwest Pacific, and cyclones in the South Pacific and Indian Ocean.

Factors which facilitate their formation:

Warm water: Tropical cyclones form over warm tropical or subtropical waters with a surface temperature of at least 26.5°C. The warmth of water provides the energy needed to fuel the storm.

Moist air: Tropical cyclones require moist air to form. Moisture provides fuel for thunderstorms that make up the storm.

Low wind shear: Wind shear is the change in wind speed or direction with height. Low wind shear is essential for the development of a tropical cyclone because it allows the storm to maintain its organization and strength. (High wind shear removes the heat and moisture they need from the area near their center. Shear also distorts the shape of a hurricane by shearing it (blowing the top away from the lower portion), so that the vortex is tilted. A tilted vortex is usually a less efficient heat engine--the delicate balance of inflowing low-level winds and outflowing upper-level winds that ventilate the storm gets disrupted.)

A pre-existing weather disturbance: Tropical cyclones typically form from pre-existing weather disturbances, such as a tropical wave or an area of low pressure. These disturbances provide the initial rotation and organization needed for a tropical cyclone to form.

Converging winds: Tropical cyclones form in areas where winds are converging and rising, which allows for the development of thunderstorms and the low-pressure area of the tropical cyclone.

Coriolis force: It helps the wind to rotate. This is the reason that cyclones are not formed at the Equator.

It's worth noting that all these conditions have to be met and in the right balance; otherwise, the tropical cyclone would dissipate or fail to form. Also, the storm needs to be in an environment where it can maintain its strength and not be disrupted by other weather systems or wind shear.

Major tracks and frequency of Hurricanes and typhoons

IMD uses a color-coded warning system to classify the severity of tropical cyclones. The system uses four colors: Green, Yellow, Orange, and Red.

IMD uses a color-coded warning system to classify the severity of tropical cyclones. The system uses four colors: Green, Yellow, Orange, and Red.
  • Green: This color is used for cyclones that are not expected to cause significant damage. The IMD issues a "Green" warning for cyclones that are likely to cause light to moderate rainfall and winds of up to 40 km/h.
  • Yellow: This color is used for cyclones that are expected to cause moderate damage. The IMD issues a "Yellow" warning for cyclones that are likely to cause heavy rainfall and winds of 40-60 km/h.
  • Orange: This color is used for cyclones that are expected to cause substantial damage. The IMD issues an "Orange" warning for cyclones that are likely to cause very heavy to extremely heavy rainfall and winds of 60-100 km/h.
  • Red: This color is used for cyclones that are expected to cause severe damage. The IMD issues a "Red" warning for cyclones that are likely to cause extremely heavy rainfall and winds of more than 100 km/h.
  • The warning system is designed to help people prepare for a cyclone, and to take appropriate action to protect themselves, their families, and their property. The color code is based on the forecasted wind speed, rainfall, and surge height. The IMD also issues forecasts and updates on the progress of the storm and provides advice on what actions to take in response to the storm.
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