5 LAYERS OF THE ATMOSPHERE




As indicated in one of my posts the atmosphere is a mixture of nitrogen (78%), oxygen (21%), and other gases (1%) that surrounds Earth. High above the planet, the atmosphere becomes thinner until it gradually reaches space. It is divided into five layers. It is thickest near the surface and thins out with height until it eventually merges with space. Most of the weather and clouds are found in the first layer.

The atmosphere is an important part of what makes Earth livable. It blocks some of the Sun's dangerous rays from reaching Earth. It traps heat, making Earth a comfortable temperature. And the oxygen within our atmosphere is essential for life.

The 5 layers are:

·         TROPOSPHERE

·         STRATOSPHERE

·         MESOSPHERE

·         THERMOSPHERE

·         EXOSPHERE

TROPOSPHERE

It is the first layer above the surface of the Earth. Weather occurs in this layer. The troposphere starts at Earth's surface and goes up to a height of 12 km ( 7 miles) above sea level. Most of the mass (about 75-80%) of the atmosphere is in the troposphere. The troposphere is the lowest layer of Earth's atmosphere.

STRATOSPHERE

 The stratosphere is the second layer, as one moves upward from Earth's surface of the atmosphere. The stratosphere is above the troposphere and below the mesosphere. Many jet aircrafts fly in the stratosphere because it is very stable. The top of the stratosphere occurs at 50 km (31 miles) altitude. Ozone, an unusual type of oxygen molecule that is relatively abundant in the stratosphere, heats this layer as it absorbs energy from incoming ultraviolet radiation from the Sun. Temperatures rise as one moves upward through the stratosphere. This is exactly the opposite of the behavior in the troposphere in which we live, where temperatures drop with increasing altitude.

 MESOSPHERE

 The mesosphere is above the stratosphere layer. The layer above the mesosphere is called the thermosphere. The mesosphere starts at 50 km (31 miles) above Earth's surface and goes up to 85 km (53 miles) high. Meteors or rock fragments burn up in the mesosphere.

THERMOSPHERE

 The space shuttle and the International Space Station both orbit Earth within the thermosphere The thermosphere is directly above the mesosphere and below the exosphere. It extends from about 90 km (56 miles) to between 500 and 1,000 km (311 to 621 miles) above our planet.   Much of the X-ray and UV radiation from the Sun is absorbed in the thermosphere.  The auroras (the Southern and Northern Lights) primarily occur in the thermosphere. Charged particles (electrons, protons, and other ions) from space collide with atoms and molecules in the thermosphere at high latitudes, exciting them into higher energy states. Those atoms and molecules shed this excess energy by emitting photons of light, which we see as colorful auroral displays.

EXOSPHERE

 The atmosphere merges into space in the extremely thin exosphere. This is the upper limit of our atmosphere. The exosphere is almost a vacuum. The "air" is very, very thin there. When air is thin, it doesn't transfer much heat to objects in the air, even if the air is very, very hot. The region where atoms and molecules escape into space is referred to as the exosphere. The exosphere is on top of the thermosphere. It extends from the exobase, which is located at the top of the thermosphere at an altitude of about 700 km above sea level, to about 10,000 km (6,200 mi; 33,000,000 ft.).

Between the layers there are boundaries. The boundaries are the tropopause, top of the troposphere; the stratopause, top of the stratosphere; the mesopause, the top of the mesosphere; the exobase, the top of the thermosphere.

Within the 5 layers there are secondary layers. Some of them are- ozone layer, ionosphere, homosphere and heterosphere.

The Earth’s atmosphere, commonly called air, is not a vast homogeneous expanse. It is layered. It has 5 layers. The atmosphere has been so layered as to make the Earth livable. The first layer, from the surface of the Earth, the troposphere, makes 75-80% of the mass of the whole atmosphere. The exosphere, the upper limit of our atmosphere merges into space. The troposphere is where you and I hang out; that is where humans hang out. Humans are tied to the troposphere.



Reference:
windows2universe.org

en.wikipedia.org

 

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