What is the phenomena of La Niña’s triple dip? Talk about how it will probably affect various parts of the world. (Answer in 150 words)
According to WMO (World Meteorological Organization)- "Cyclone is a low pressure system with sustained winds of atleast 34 knots (63 km/h) and a closed circulation pattern." Favourable conditions for the formation of Tropical Cyclones- High Humidity i.e around 60-80%. Vertical Wind Shear should be lRead more
According to WMO (World Meteorological Organization)- “Cyclone is a low pressure system with sustained winds of atleast 34 knots (63 km/h) and a closed circulation pattern.”
Favourable conditions for the formation of Tropical Cyclones-
- High Humidity i.e around 60-80%.
- Vertical Wind Shear should be low (< 10 m/s).
- Warm Ocean waters with temperature ≥ 26.5 °C .
- Low pressure area.
- Convergence of winds with the upper level of divergence.
- Presence of Coriolis Force.
Differences between Tropical and Temperate Cyclones –
- Origin – Tropical cyclones form only on seas with temperature more than 26.5 °C in between 10° to 30° N and S of the equator ex-Hurricanes whereas Temperate cyclones can be formed both on land as well as seas in between 35° to 65° N and S of equator ex- European Windstorms .
- Shape – Tropical cyclones are elliptical in shape where as Temperate cyclones are in shape of of inverted V .
- Lifespan – Tropical cyclones doesn’t last for more than 1 week whereas Temperate cyclones may last for 2 to 3 weeks .
- Movement – Tropical cyclones move westward then poleward whereas Temperate cyclones move eastward then northeastward.
- Intensity – Tropical cyclones are more intense(Category 1 to 5) as compared to the Temperate cyclones.
Understanding these favourable conditions and differences will help us to predict,prepare and track the movements of cyclones by using effective mitigation strategies like – early warning system,storm shelters, evacuation drills,remote sensing etc .
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La Niña refers to the large-scale cooling of ocean surface temperatures in the central and eastern equatorial Pacific Ocean, coupled with changes in the tropical atmospheric circulation, namely winds, pressure and rainfall. The current La Niña episode started in September 2020 and has continued forRead more
La Niña refers to the large-scale cooling of ocean surface temperatures in the central and eastern equatorial Pacific Ocean, coupled with changes in the tropical atmospheric circulation, namely winds, pressure and rainfall. The current La Niña episode started in September 2020 and has continued for a third consecutive year and has thus been classified as a ‘triple dip’ La Niña. According to the World Meteorological Organization (WMO), the first “triple-dip” La Niña of the 21st century will continue to affect different parts of the world as given below:
In light of these impacts, concerns are raised about the unfolding humanitarian catastrophe for millions of people in different parts of the world especially in the Horn of Africa, which is witnessing one of the longest and the most severe droughts. It is necessary to provide tailored information to the humanitarian sector and to support sensitive sectors like agriculture, food security, health, and disaster risk reduction.
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