Several sections of India have recently experienced significant heat waves. The temperatures in urban areas and cities are higher than in rural areas. “Urban Heat Island” is the name given to this phenomena.
These temperature differences, according to experts, are produced by differences in heating across highly urbanised and semi-urbanized areas, as well as the relative availability of open and green spaces in the surrounding areas.
An urban heat island is a localised and transient phenomena in which particular areas of a city have higher heat loads than the surrounding area.
This spike in temperature is primarily caused by concrete buildings and dwellings in cities, where heat is trapped and cannot easily evaporate.
The urban heat island is caused by trapped heat between concrete structures.
Temperature changes of 3 to 5 degrees Celsius are possible.
Construction activity has increased dramatically: Carbon-absorbing materials such as asphalt and concrete are required for the evolution of cities, from small urban residences to complex infrastructures. They trap a lot of heat, which raises the average surface temperature of cities.
Dark surfaces: Many buildings in urban areas have dark surfaces, which reduce albedo and increase heat absorption.
Buildings with dark surfaces heat up more quickly and require more air conditioner chilling, which consumes more energy from power plants, resulting in more pollution. Furthermore, air conditioners exchange heat with ambient air, resulting in additional local heating. As a result, the spread of urban heat islands is aided by a cascading effect.
Plantation and efforts to increase the area under green cover are the most important requirements for reducing heat load in metropolitan settings.
Passive Cooling to Reduce Heat Islands in Cities: Passive cooling, a widely utilised approach for creating naturally ventilated buildings, can be a vital alternative for residential and commercial buildings to alleviate the urban heat island.
In the context of global warming, the IPCC report highlights ancient Indian architectural designs that utilised this technology, which may be adapted to current facilities.
Heat islands are becoming more common in Delhi’s urban areas, according to NASA.
The temperature in the city of Delhi was substantially greater than in the surrounding farmlands.
NASA’s Ecosystem Spaceborne Thermal Radiometer Experiment (Ecostress) captured the image, which shows a large red area over Delhi and smaller red patches near neighbouring cities Sonipat, Panipat, Jind, and Bhiwani.
NASA launched Ecostress, a radiometer-equipped gadget, to the International Space Station in 2018.
Ecostress is in charge of determining the temperature of plants, as well as their water requirements and the impact of the climate on them.
These red regions in the Ecostress data exhibited higher temperatures, indicating urban heat islands, whereas rural areas around cities had lower temperatures.
Twin cyclones named cyclone Asani and cyclone Karim have been captured in recent satellite photographs in the Indian Ocean region, one in the northern hemisphere and the other in the southern hemisphere.
When the vorticity in both the Northern and Southern hemispheres is positive, as it is with Rossby waves, the moist air in the boundary layer is elevated slightly.
That is sufficient to initiate a feedback loop.
Water vapour condenses when the air is elevated slightly, forming clouds. The latent heat of evaporation is released as it condenses.
The atmosphere warms, the parcel of air rises, and the process triggers positive feedback. Because it is lighter than the surrounding air, the warmer parcel of air can rise higher and form deeper clouds.
If you have westerly winds at the lower level and easterly winds at the upper level, cyclones will not form if the difference between them is too great.
Cyclones will form even if the difference is small.
There will be a large, tall vortex inside with a variety of clouds. They will spin faster and faster as they grow stronger, eventually becoming large storms.
Yes, they will normally go west once formed. They will have a somewhat northerly component of motion in the Northern Hemisphere, whereas they will have a slightly southern component in the Southern Hemisphere.
As a result, the cyclone in the northern hemisphere is travelling north and west, while the one in the southern hemisphere is moving south and west.
The MJO is a huge cloud and convection cluster that spans 5,000-10,000 kilometres.
It’s made up of a Rossby wave and a Kelvin wave, both of which are types of wave structures seen in the ocean. The Kelvin wave is on the MJO’s eastern side, while the Rossby wave is on the MJO’s western, trailing edge, with two vortices on either side of the equator.
The MJO does not, however, cause all tropical cyclones. It’s occasionally just a Rossby wave with two eddies on each side.
The country’s first 5G testbed was recently inaugurated, allowing start-ups and industrial companies to test their products locally, minimising reliance on facilities outside.
5G technology would have a positive impact on the country’s governance, as well as the convenience of living and doing business.
Agriculture, health, education, infrastructure, and logistics all stand to benefit from this.
This will also improve convenience while also creating several job chances.
Researchers have discovered a molecular signature in the blood that could aid in the identification of newborn newborns at risk of Sudden Infant Death Syndrome (SIDS).
SIDS is the sudden death of a seemingly healthy baby under the age of one year, generally while sleeping.
Because newborns frequently die in their cribs, SIDS is also known as crib death.
Butyrylcholinesterase (BChE) is an enzyme that is involved in the arousal pathway in the brain.
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