The ionosphere
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The charged layers in the thermosphere are called the ionosphere. This region of the Earth's atmosphere is characterized by high concentrations of ions and free electrons, which are produced by the interaction of solar radiation with the gas molecules. The ionosphere plays a crucial role in radio wave propagation and aurora formation.
The thermosphere consists of two layers: the lower layer, called the mesosphere, extends from about 50-85 kilometers above the Earth's surface. The upper layer, known as the thermosphere, starts around 85 kilometers and extends to about 600 kilometers. These layers experience extreme temperatures, are where the auroras occur, and are important for satellite communication and navigation.
The five layers are called Troposphere, Stratosphere, Mesosphere, Thermosphere, and Exosphere.
The region within the lower portion of the thermosphere where particles become electrically charged is called the ionosphere. This layer of the atmosphere contains a high concentration of ions and free electrons, which allows it to reflect radio waves and facilitate long-distance communication.
The layers of the Earth's atmosphere are named troposphere, stratosphere, mesosphere, thermosphere, and exosphere.
The four layers of Earth's atmosphere from lowest to highest are the troposphere, stratosphere, mesosphere, and thermosphere.