Layers of Atmosphere and Their Characteristics Leverage Edu
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This diagram illustrates some of the features and phenomena found in the various layers of Earth's atmosphere. Starting from ground level, the layers include the troposphere, stratosphere, mesosphere and thermosphere. The exosphere, which is above the thermosphere, is not shown in the diagram.
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Start drawing - roughly sketch out the space, and slowly add detail - pay attention to the perspective, and overall composition of your scene.
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The atmosphere of the Earth is divided into four layers: troposphere, Stratosphere, Mesosphere and Thermosphere, and they are separated based on temperature. Weather processes occur in the lower layers of the atmosphere while interesting events such as the beautiful aurora occur higher. By understanding how the atmosphere's temperature.
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4 Layers of the Atmosphere (With Diagram) The atmosphere is the gaseous realm. It consists of a mixture of gases that completely surround the earth. Of much greater significance to metabolism, however, are the gaseous cycles of the atmosphere. The air consists mainly of oxygen (about 20 per cent), carbon dioxide (about 0.03 per cent), nitrogen.
Layers of Atmosphere and Their Characteristics Leverage Edu
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Earth's atmosphere is composed of a series of layers, each with its own specific traits. Moving upward from ground level, these layers are called the troposphere, stratosphere, mesosphere, thermosphere, and exosphere. The exosphere gradually fades away into the realm of interplanetary space. The layers of the atmosphere: the troposphere.
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The ionosphere is an abundant layer of electrons and ionized atoms and molecules that stretches from about 48 kilometers (30 miles) above the surface to the edge of space at about 965 km (600 mi), overlapping into the mesosphere and thermosphere.
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This layer holds 19 percent of the atmosphere's gases but very little water vapor. In this region, the temperature increases with height. Heat is produced in the process of the formation of ozone, and this heat is responsible for temperature increases, from an average -60°F (-51°C) at tropopause to a maximum of about 5°F (-15°C) at the top of the stratosphere.
