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Mahesh

01/07/22 01:05 AM IST

Cyclones Naming

What are the guidelines to adopt names of cyclones?
  • While picking names for cyclones, here are some of the rules that countries need to follow. If these guidelines are following, the name is accepted by the panel on tropical cyclones (PTC) that finalises the selection:
  •  The proposed name should be neutral to (a) politics and political figures (b) religious believes, (c) cultures and (d) gender
  • Name should be chosen in such a way that it does not hurt the sentiments of any group of population over the globe
  • It should not be very rude and cruel in nature
  • It should be short, easy to pronounce and should not be offensive to any member
  • The maximum length of the name will be eight letters
  • The proposed name should be provided with its pronunciation and voice over
  • The names of tropical cyclones over the north Indian Ocean will not be repeated. Once used, it will cease to be used again. Thus, the name should be new.
  • The 13 names in the recent list that have been suggested by India include: Gati, Tej, Murasu, Aag, Vyom, Jhar (pronounced Jhor), Probaho, Neer, Prabhanjan, Ghurni, Ambud, Jaladhi and Vega.
  • Some of the names picked by India were suggested by the general public. An IMD committee is formed to finalise the names before sending it to the PTC.
  • The first cyclone name which will be chosen will be the one in the first row of the first column — Nisarga by Bangladesh.
  • Next, India’s choice, Gati, will be chosen, and so on. Subsequent cyclones are being named sequentially, column-wise, with each cyclone given the name immediately below that of the previous cyclone. Once the bottom of the column is reached, the sequence moves to the top of the next column.

Bangladesh

Nisarga

Biparjoy

Arnab

Upakul

Barshon

Rajani

Nishith

India

Gati

Tej

Murasu

Aag

Vyom

Jhar

Probaho

Iran

Nivar

Hamoon

Akvan

Sepand

Booran

Anahita

Azar

Maldives

Burevi

Midhili

Kaani

Odi

Kenau

Endheri

Riyau

Myanmar

Tauktae

Michaung

Ngamann

Kyarthit

Sapakyee

Wetwun

Mwaihout

Oman

Yaas

Remal

Sail

Naseem

Muzn

Sadeem

Dima

Pakistan

Gulab

Asna

Sahab

Afshan

Manahil

Shujana

Parwaz

Qatar

Shaheen

Dana

Lulu

Mouj

Suhail

Sadaf

Reem

Saudi 

Jawad

Fengal

Ghazeer

Asif

Sidrah

Hareed

Faid

Sri Lanka

Asani

Shakhti

Gigum

Gagana

Verambha

Garjana

Neeba

Thailand

Sitrang

Montha

Thianyot

Bulan

Phutala

Aiyara

Saming

UAE

Mandous

Senyar

Afoor

Nahhaam

Quffal

Daaman

Deem

Yemen

Mocha

Ditwah

Diksam

Sira

Bakhur

Ghwyzi

Why is it important to name cyclones?

  • Adopting names for cyclones makes it easier for people to remember, as opposed to numbers and technical terms.
  • Apart from the general public, it also helps the scientific community, the media, disaster managers etc.
  • With a name, it is easy to identify individual cyclones, create awareness of its development, rapidly disseminate warnings to increased community preparedness and remove confusion where there are multiple cyclonic systems over a region.

Benefits of naming : Naming of tropical cyclones helps the scientific community, disaster managers, media and general masses to

  • Identify each individual cyclone.
  • Create awareness of its development.
  • Remove confusion in case of simultaneous occurrence of tropical cyclones over a region.
  • Remember a tropical cyclone easily,
  • Rapidly and effectively disseminate warnings to a much wider audience.
  • In the Atlantic and in the Southern hemisphere (Indian ocean and South Pacific), tropical cyclones receive names in alphabetical order, and women and men’s names are alternated. Nations in the Northern Indian ocean began using a new system for naming tropical cyclones in 2000; the names are listed alphabetically country wise, and are neutral gender wise.
  • The common rule is that the name list is proposed by the National Meteorological and Hydrological Services (NMHSs) of WMO Members of a specific region, and approved by the respective tropical cyclone regional bodies at their annual/biennual sessions.

When it was agreed to name the Tropical cyclones ?

  • The WMO/ESCAP Panel on Tropical Cyclones (PTC) at its 27th Session held in 2000 in Muscat, Oman agreed in principle to assign names to the tropical cyclones in the Bay of Bengal and Arabian Sea.
  • The naming of the tropical cyclones over the north Indian Ocean commenced from September 2004.
  • This list contained names proposed by then eight member countries of WMO/ESCAP PTC, viz., Bangladesh, India, Maldives, Myanmar, Oman, Pakistan, Sri Lanka and Thailand.
  • The requirement for a fresh list of tropical cyclones including representation from five new member countries: Iran, Qatar, Saudi Arabia, United Arab Emirates and Yemen (total 13 member countries) was tabled during the 45th session of WMO/ESCAP, held in September 2018. The session was hosted by Oman.
  • The World Meteorological Organization (WMO) and the Economic and Social Commission for Asia and the Pacific (ESCAP) jointly established the Panel on Tropical Cyclones (PTC)in 1972 as an intergovernmental body.
  • Its membership comprises countries affected by tropical cyclones in the Bay of Bengal and the Arabian Sea.
  • The Panel is one of the five regional tropical cyclone bodies established as part of the WMO Tropical Cyclone Programme (TCP) which aims at promoting and coordinating the planning and implementation of measures to mitigate tropical cyclone disasters on a worldwide basis.
  • For this purpose, there are Regional Specialized Meteorological Centre (RSMC)- Tropical cyclone and Tropical Cyclone Warning Centres (TCWC) for different regions.
  • The main objective of the WMO/ESCAP Panel on Tropical Cyclones is to promote measures to improve tropical cyclone warning systems in the Bay of Bengal and the Arabian Sea.

 

 

Where other than Earth cyclones are spotted?
  • Cyclones are not only present on Earth but also spotted on other planets like Mars, Jupiter, and Neptune. The Great Red Spot is the hurricane on Jupiter which is going on from 340 years. Great Black Spot was spotted in the Southern Hemisphere of Neptune.
There are various types of cyclones depending on the type of prevailing low-pressure system.
  • Tropical cyclone- Tropical cyclones are regarded as one of the most devastating natural calamities in the world.
  • They originate and intensify over warm tropical oceans.
  • These are ferocious storms that originate over oceans in tropical areas and move over to the coastal areas causing violent winds, very heavy rainfall, and storm outpourings.
  • Extratropical cyclone- The Extra-Tropical Cyclones are storm systems emerging in the mid and high latitudes, away from the tropics.
  • They are low-pressure systems with associated cold fronts, warm fronts, and occluded fronts.
  • These cyclones are formed along the polar front.
  • In the beginning, the front is stationary.
  • Extra-tropical cyclones are also known as mid-latitude storms or baroclinic storms.
  • In the Northern hemisphere, cold air blows from the north of the front and warm air blows from the south.
  • When the pressure descents along the front, the cold air move towards the south, and the warm air moves northwards setting in motion an anticlockwise cyclonic circulation.
  • The cyclonic circulation results in a well-built extratropical cyclone, with a cold front and a warm front.
  • There are pockets of warm air compressed between the forward and the rear cold air.
  • The warm air climbs over the cold air and a series of clouds appear over the sky ahead of the warm front and cause rainfall.
  • The cold front approaches the warm air from behind and pushes the warm air up.
  • As an outcome, cumulus clouds develop along the cold front.
  • The cold front moves faster than the warm front eventually surpassing the warm front.
  • The warm air is entirely lifted and the front is occluded and the cyclone dissipates.
  • They can originate over the land and sea and cover a larger area.
Tornadoes
 Cyclone Formation
  • When it comes to the formation or strengthening of a cyclone, Cyclogenesis plays a crucial role. It is an umbrella term to identify several different processes that result in a cyclone.
  • Tropical cyclones are formed over warm ocean water near the equator. Warm moist air near the surface of the ocean rises upwards. This creates a low-pressure area near the surface.
  • This results in the movement of cooler air from surrounding areas into the low-pressure area.
  • Now even this cool air becomes warm and moist and rises up. The above cycle keeps continuing.
  • The warm moist air which rises up, cools the water in the air, resulting in the formation of clouds.
  • This whole system of clouds and winds spins and grows. This entire cycle continues resulting in a cyclone.
  • When the winds reach a speed of 63 mph, it is called a tropical storm, when the winds reach a speed of 119 kmph it is called a tropical cyclone or hurricane.

Who categorises cyclones in India over Bay of Bengal and Arabian Sea?

  • Indian Meteorological Department (IMD), classified the low-pressure systems in the Bay of Bengal and the Arabian Sea on the basis of maximum sustained wind speed.

Type of disturbance

Wind speed

Low-pressure area

Less than 31 km per hour

Depression

31-49 km per hour

Deep depression

50-61 km per hour

Cyclonic storm

62-88 km per hour

Severe cyclonic storm

89-117 km per hour

Severe cyclonic storm

118-167 km per hour

Very severe cyclonic storm

168-221 km per hour

Super cyclonic storm

222 km per hour and higher

  •  IMD, one of the six Regional Specialised Meteorological Centres (RSMC) in the world, is mandated to issue advisories and name tropical cyclones in the north Indian Ocean region.
  • The advisories are issued to 13 member countries under WMO/ESCAP Panel including Bangladesh, India, Iran, Maldives, Myanmar, Oman, Pakistan, Qatar, Saudi Arabia, Sri Lanka, Thailand, United Arab Emirates and Yemen.

India Meteorological Department (IMD)

  • Formed in 1875, the India Meteorological Department (IMD) is the national meteorological service of the country and it is the chief government agency dealing in everything related to meteorology, seismology, and associated subjects.
  • The administrative responsibilities of the Department are under the supervision of the Ministry of Earth Sciences of the Indian Government. The IMD is headquartered in New Delhi.

 IMD Mandate

  • The mandate and functions of the IMD are discussed below-
  • Taking meteorological observations and providing current information and forecasting information for the most favorable operation of weather-dependent activities such as irrigation, agriculture, aviation, shipping, offshore oil exploration, and so on.
  • Giving warnings against severe weather phenomena such as tropical cyclones, dust storms, heat waves, cold waves, heavy rains, heavy snow, etc.
  • Providing met-related statistics needed for agriculture, industries, water resources management, oil exploration, and any other strategically important activities for the country.
  • Engaging in research in meteorology and allied subjects.
  • Detection and location of earthquakes and evaluation of seismicity in various parts of the country for developmental projects.

 

How are the cyclones named?

  • In 2000, a group of nations called WMO/ESCAP (World Meteorological Organisation/United Nations Economic and Social Commission for Asia and the Pacific), which comprised Bangladesh, India, the Maldives, Myanmar, Oman, Pakistan, Sri Lanka and Thailand, decided to start naming cyclones in the region.
  • After each country sent in suggestions, the WMO/ESCAP Panel on Tropical Cyclones (PTC) finalised the list.
  • The WMO/ESCAP expanded to include five more countries in 2018 — Iran, Qatar, Saudi Arabia, United Arab Emirates and Yemen.
  • The list of 169 cyclone names released by IMD last month, in April, were provided by these countries — 13 suggestions from each of the 13 countries.
  • The new list included the last name from the previous list (Amphan) as it remained unused at the time of release.
  • Incidentally, the IMD has issued an alert for Cyclone Amphan, which is forming over the southeast Bay of Bengal and adjoining south Andaman sea.

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