Recently in October 2013, Tropical cyclone Phailin struck the coast of Odisha and Andhra destroying many homes, lives and caused loss of property. It originated in the Gulf of Thailand and gradually grew in intensity as it moved over Andman Sea in Bay of Bengal. It was a Category 5 storm with 200 Kmph winds and rainfall.
What is a Tropical Cyclone?
Tropical Cyclones are low pressure systems that are formed over the warm tropical waters due to gale force winds (winds of tropical force i.e in the range 200 kmph or greater). They generally extend hundreds of kilometer and generally persist for six hours. However they die out when they travel through land & Cold Ocean or cold area.
Many people call tropical cyclone by various names; such as hurricanes, typhoons or cyclones. It depends on the location of the storm. But the scientific name is “tropical cyclone”. Storms that flow over Atlantic Ocean or eastern Pacific Ocean are called “hurricanes” (Hurricane in the Atlantic, Typhoon in the Pacific and Cyclone in the Indian Ocean).
TERMINOLOGIES ASSOCIATED WITH TROPICAL CYCLONE
- Circular Eye: It is the centre of tropical cyclone. Owing to its round shape, its size is generally expressed in diameter which ranges from 10 -100 km.
- Eye wall: Circular eye is surrounded by thick ring of cloud called eye wall. Area under it experiences extreme winds & heaviest rainfall.
CATEGORIES OF TROPICAL CYCLONE
|Wind Speed (miles per hour)||Damage at Landfall||Storm Surge (feet)|
Generally when the winds in the rotating storm have the speed of 39 mph then they are called tropical storm & when the speed reaches 74 mph it is called tropical cyclone.
CLASSIFICATION OF TROPICAL CYCLONES
Important feature of tropical cyclones is their degree of intensity. So tropical cyclones are classified according to their degree of intensity. Following are its types:
- Tropical Disturbance: It has weak wind circulation & low velocities.
- Tropical Depression: It has a definite wind circulation with velocities less than 63 kilometers per hour (kph)
- Tropical Storm: It is a moderate tropical cyclone with maximum wind speed of 118 kph.
- Typhoon: It is an intense tropical cyclone with maximum wind speed exceeding 118 kph.
CONDITIONS FOR DEVELOPMENT OF TROPICAL CYCLONES
Following things are required for tropical cyclones to develop:-
- Very large ocean areas with surface temperature more than 26 C.
- They need warm tropical oceans to feed them energy without which they will cease to exist.
- Tropical cyclone can exist only when there is proper combination of circulation, divergence and convergence of air which is maintained over a considerable period of time on a proper scale.
FORMATION OF TROPICAL CYCLONES
Formation of tropical cyclones can be explained by convective theory or the frontal or counter-current theory.
According to Convective theory:
- a large mass of air becomes convectively unstable and moist compared with its surroundings, which results in an upward motion of air.
- The air from the surroundings tend toward the low pressure area formed, so that, a cyclonic circulation is formed.
- The combined effects of the earth's rotation and the centrifugal force, retards the movements of air towards the center causing further pressure fall.
- The process continues until a vigorous cyclonic wind system is developed. Likewise, the outward flow of air from the center at high levels also makes the pressure lower.
According to Frontal or Counter-Current Theory:
- many tropical cyclones form along the front between the trade winds and the equatorial air in the doldrums.
- Winds develop along this front and when conditions are favorable, forms into tropical cyclones.
- The convergence of the two air masses results in the upward motions which in addition to the deflective effect of the earth's rotation, centrifugal force, and divergence at the upper levels results in allow pressure area with a spiral circulation toward the center.
LIFE-CYCLE OF A TROPICAL CYCLONE
Cyclones of severe category pass through four stages. But in cases of non-severe category cyclone various constraints hamper its development such as movement over land or cooler place or making landfall, etc. Following are the stages of a typical severe tropical cyclone:-
|1||The Formative Stage||
|2||The Immature Stage||
|3||The Mature Stage||
|4||The Decay Stage||
DIFFERENCE BETWEEN TEMPERATE AND TROPICAL CYCLONES
|Sr.No||Temperate Cyclone||Tropical Cyclone|
|1||Formed in mid-latitudes i.e. 40 degree to 60 degree North and South.||Formed in lower latitudes i.e. 10 degree to 30 degree North and South.|
|2||Formed due to convergence of the warm (tropical) and Cold (Polar) air masses.||Formed due to the convergence of warm dry and warm moist air masses.|
|3||The isobars of temperate cyclones are Wedge shaped or oval shaped.||The isobars of tropical cyclones are circular.|
|4||Have strong fronts||Have weak fronts|
|5||Primarily get their energy from horizontal gradients in temperature.||Primarily get their energy from the heat that is released when water vapour that has been evaporated from the ocean surface|
NAMING OF TROPICAL CYCLONE – WHY, HOW ?
|1||Why name cyclones ?||
|2||How do they name cyclones ?||
|3||What happens to the name afterwards?||Names usually retire after the event has occurred. It is replaced by a new name when it occurs again.|
|4||Do they run out of names?||No. The World Meteorological Organization maintains the lists.|
CYCLONE DANGERS AND IMPACTS
|1||Destructive winds||Wind velocities vary from 90 km/h to more than 280 km/h & converts airborne debris into potential missiles|
|2||Heavy rainfall with flooding||Heavy rainfall causes extensive flooding.|
|3||Storm surges||Storm surge is a raised dome of water about 60 to 80 km across and typically about 2 to 5 m higher than the normal tide level. If the surge occurs at the same time as a high tide then the area inundated can be quite extensive, particularly along low-lying coastlines.|
Indian National Center for Ocean Information Services (INCOIS)
An autonomous organization of the Government of India, under the Ministry of Earth Sciences, located in Hyderabad. It provides ocean information and advisory services to different strata of the society such as industry, government and scientific community through sustained ocean observations and constant improvisation of its deliverables by means of systematic and focused research.
|Sr. No.||Services / Programs started by INCOIS||Description|
|1||Potential Fishing Zone (PFZ)||This service was started by INCOIS to identify potential fishing zone so that better produce can be obtained by fishermen.|
|2||Tsunami Early Warning Centre (TEWS)||In the aftermath of Tsunami of 2004, this system was put in place to give early signs of any possible stormsurges.|
|3||Ocean State Forecast (OSF)||For knowing state of Ocean as India has been surrounded on three sides by water & this information is vital for its commercial activities.|
|4||Ocean Observation Group (OOG)||The main activity of this group in INCOIS is to measure and monitor the surface temperature and salinity of the upper 2000 meters of the ocean. This system was named as Argo.|
|5||Satellite Data Acquisition, Processing System (SDAPS)||This will help to get real time data from satellites. These real-time data help the INCOIS to predict sea surface temperature and other geophysical parameters.|