Weather and climate

Weather is this hour-to-hour, day today condition of the atmosphere.It can change dramatically from day today.The average weather condition of a place for a longer time period represents the climate of a place.


The degree of hotness and coldness of the air is known as temperature.The temperature of the atmosphere changes not only between day and night, but also from season to season. An important factor that influences the distribution of temperature is insolation.Insolation is the incoming solar energy intercepted by the earth.The amount of insolation decreases from the equator towards the poles. Therefore the temperature decreases in the same manner. Temperature in cities is much higher than that of villages.The concrete and metals in buildings and the asaphalt of roads get heated up during the daywhich is released during the night. Also, the crowded high rise buildings of the citiestrap the warm air, and thus raise the temperature of the cities.

The standard unit of measuring temperature is degree Celsius. It was invented by Anders Celsius. On the Celsius scale the water freezes at 00 C and boils at 1000 C.

Thermometer measures the temperature.Barometer measures atmospheric pressure.Rain gauge measures the amount of rainfall.Wind vane shows the direction of the wind.

Air pressure

Air pressure is defined as the pressure exerted by the weight of air on the earth’s surface.As we go up the layers of atmosphere, the pressure falls rapidly.The air pressure is highest at sea level and decreases with height. Horizontally, the distribution of air pressure is influenced by temperature of air at a given place.In areas where temperature is high, the air gets heated and rises. This creates a low pressure area.

In areas having low temperature, the air is cold. It is therefore heavy.The air always move from high pressure areas too low pressure areas. On the moon, there is no air and  hence no air pressure. Astronauts have to wear special protective spacesuits filled with air when they go to the moon. If they did not wear these space suits, the counter pressure exerted by the body of the astronauts would make the blood vessels burst.The astronauts would bleed.


The movement of air from high pressure areas to low pressure area is called wind.

The wind is named after the direction from which it blows. Example the wind blowing from the West is called westerly.

Wind can be broadly divided into 3 types:-

Permanent winds

The tradewinds, westerlies and easterlies are the permanent winds that blow constantly throughout the year in a particular direction.

Seasonal winds

These winds change their direction in different seasons, for example, monsoons in India.

Local winds

These blow only during a particular period of the day or year in a small area. For example, land and sea breeze.The hot and dry local winds of northern plains of India is called Loo.


When water evaporates from land and different water bodies, it becomes water vapour.Moisture in the air at any time is known as humidity. When the air is full of water vapour, we call it humid day.As the air gets warmer, its capacity to hold the water vapour increases, so it becomes more and more humid.When the water vapour rises, it starts cooling. The water vapour condenses causing formation of droplets of water. Clouds are just masses of such water droplets. When these droplets of water becomes too heavy to float in air then theycome down as precipitation.Precipitation that comes down to the Earth in liquid form is called rain. Other forms of precipitation are snow, sleet and hail.

There are 3 types of rainfall:-

The convectional rainfall
The orographic rainfall
The cyclonic rainfall.

Importance of rainfall

It is very important for the survival of plants and animals. It brings freshwater to the earth’s surface.If rainfall is less- water scarcity and draught occur. On the other hand if it is more, floods take place.

Cyclone- Nature’s Fury

Odisha, located on the eastern sea coast of India, is prone to cyclones that originate in the Bay of Bengal.On 17-18 October 1999, cyclone hits five districts of the state.Another super cyclone occurred on the 29th October 99.The damages caused were mainly due to three factors: wind velocity, rain and tidal surge.The winds of upto 260 km per hour lasted for over 36 hours.These high velocity winds uprooted trees and damaged the Kutcha houses.Rooftops of several industrial sheds and other houses were also blown away.Heavy rains occur under the influence of cyclone for 3 days continuously. These Rains lead to the flooding in the major rivers of Odisha.The cyclonic winds caused tidal waves that swept 20 km inland and brought massive destruction to the coastal areas.7 to 10 m high tidal waves intruded suddenly and cause massive damage to the standing paddy crops.

The Super Cyclone swep the entire cost of Odisha, including the cities of Bhubaneswar and Cuttack and 28 coastal towns. About 13 million peoples were affected. A large number of livestock were killed,standing crops of paddy, vegetables and fruits were heavily damaged. Due to salination caused by tidal surge, large tracts of agricultural land, has turned infertile.Last tracts of sal, teak can bamboo plantation have disappeared. The mangrove forestsbetween Paradeep and Konark vanished.

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