Layers of atmosphere model 3d - science project for exhibition - diy - simple | howtofunda
Layers of Atmosphere model making Science Project | Model of earth's atmosphere | Diorama Atmosphere
Easy Model of layers of atmosphere |layer of atmosphere | science project |
earth atmosphere layers model making science project | DIY cardboard | howtofunda | still model
Layers of atmosphere Model project | Model of earth's atmosphere | atmosphere exhibition model
Layers of the atmosphere model | 2D and 3D model | Atmosphere Layers | DIY project model
Atmospheric Layers.... TLM... For effective teaching... #diy #teacher #papercraft #craft #teaching
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Material Required :
1) Cardboard
2) Plastic Cricket ball
3) Thermocol
4) Water color
5) Chart paper
Explanation :-
1) Troposphere
Though the sunlight reaches the Earth’s surface from top to bottom, the troposphere is primarily heated at the bottom. The Earth’s surface is much better at absorbing a wide range of solar radiation than the air. When the parcel of warm air moves upwards, it expands, and when air expands, it cools. Due to this reason, the base of the troposphere is warmer than its base because the air on the surface of the Earth absorbs the sun’s energy, gets heated up, and moves upward, which cools down.
2) Stratosphere
The Stratosphere lies above the troposphere and extends up to a height of 50 km. This layer is free of clouds and devoid of any weather-related phenomenon. Due to this, aeroplanes fly in the Stratosphere for a smooth ride. The Stratosphere also houses the ozone layer that protects us from the harmful effect of the sun’s rays.
3) Mesosphere
The temperature in the mesosphere grows colder with the altitude. This is because there are few gas molecules in the mesosphere to absorb the Sun’s radiation. The only heat source is the stratosphere below. The mesosphere is extremely cold, especially at the top, dropping to a temperature as low as -90°C.
4) Thermosphere
The density of molecules in the thermosphere is very low. One gas molecule can go about a distance of 1 km without colliding with another molecule. Because so little energy is transferred, the air feels freezing. Satellites are found orbiting in the upper part of the thermosphere.
5) Exosphere
The exosphere is the final frontier of the Earth’s gaseous envelope. There is no clear-cut distinction between the Earth’s atmosphere layers and outer space. The air in the exosphere is constantly but gradually leaking out of the Earth’s atmosphere into outer space
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