Earth's atmosphere is a delicate veil of air consisting of multiple layers determined by temperature. This vital shield is indispensable for the existence of life on the planet, as it safeguards living things from the Sun's heat and radiation while also providing breathable air.
Although oxygen is essential for sustaining life, it is not the predominant constituent of our atmosphere. According to Vision Learning, Earth's atmosphere primarily comprises around 78% nitrogen, 21% oxygen, 0.93% argon, and 0.04% carbon dioxide, along with trace quantities of neon, helium, methane, krypton, ozone, hydrogen, and water vapor.
Below are the six atmospherical layers of Earth as per NASA:
Earth's Atmosphere: Facts About the Protective Layer of the Planet That Make Life Possible
Troposphere
The troposphere, which begins at the surface of the Earth and reaches a height of 5 to 9 miles (8 to 14.5 kilometers), is the densest layer of the atmosphere and encompasses the majority of weather phenomena.
The gases within the troposphere are in constant motion, resulting in a continuous mixing process, and it is within this atmospheric layer that the majority of Earth's weather occurs.
Stratosphere
Located directly above the troposphere, the stratosphere spans from the upper boundary of the troposphere to an altitude of 31 miles (50 kilometers). It is within this region that the ozone layer is situated, serving as a protective shield that absorbs and disperses solar ultraviolet radiation.
Mesosphere
The mesosphere, the third layer of Earth's atmosphere, stretches from the top of the stratosphere to approximately 53 miles (85 km) above the Earth's surface. According to the National Center for Atmospheric Research, it is the coldest part of the atmosphere, with temperatures averaging around minus 130 degrees F (minus 90 degrees C).
The mesosphere poses challenges for direct analysis due to its altitude, but it is known to be the region where meteors burn up and where unique high clouds called noctilucent clouds occasionally form.
Thermosphere
As per NOAA, the thermosphere is located between approximately 53 miles (85 km) and 375 miles (600 km) above the Earth's surface. It is the upper atmosphere where gases become denser as one moves closer to the Earth, resulting in the absorption of high-energy radiation from the Sun and a significant increase in temperature that can range from -184°F (-120°C) at the bottom to as high as 3,600°F (2,000°C) near the top.
However, despite the high temperature, the scarcity of molecules in this layer would not provide sufficient heat to warm our skin.
Ionosphere
The ionosphere, spanning from approximately 30 miles (48 kilometers) to 600 miles (965 kilometers) above the Earth's surface, is a dynamic layer abundant with electrons and ionized particles, and crucial for radio communications.
This layer expands and contracts based on solar activity and is divided into sub-regions based on the absorption of different wavelengths of solar radiation, playing a significant role in Sun-Earth interactions.
Exosphere
The exosphere, the outermost layer of Earth's atmosphere, stretches about 6,200 miles (10,000 km) above the surface and consists of sparsely distributed hydrogen and helium particles that seldom interact. As Space.com reported, this atmospheric layer consists of highly dispersed hydrogen and helium particles that exhibit rare collisions due to their wide distribution.
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