If the air layers in the diagram were relabeled to illustrate normal atmospheric conditions, the correct labeling from the air layer closest to the earth’s surface to the one farthest from the earth’s surface would be

General
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if the air layers in the diagram were relabeled to illustrate normal atmospheric conditions, the correct labeling from the air layer closest to the earth’s surface to the one farthest from the earth’s surface would be

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If the air layers in the diagram were relabeled to illustrate normal atmospheric conditions, the correct labeling from the air layer closest to the earth’s surface to the one farthest from the earth’s surface would be:

The atmosphere consists of different layers, each with its own characteristics. From the air layer closest to the Earth’s surface to the one farthest from the Earth’s surface, the correct labeling would be as follows:

  1. Troposphere: This is the closest layer to the Earth’s surface and extends up to an altitude of about 7-20 kilometers (4-12 miles). It is where we live and where weather phenomena occur. The temperature generally decreases with increasing altitude in this layer.

  2. Stratosphere: The next layer above the troposphere is the stratosphere, which extends from about 20-50 kilometers (12-31 miles) above the Earth’s surface. The ozone layer is located in this layer, which absorbs most of the Sun’s harmful ultraviolet radiation. The temperature remains relatively constant or even increases with increasing altitude in this layer.

  3. Mesosphere: Above the stratosphere is the mesosphere, extending from about 50-85 kilometers (31-53 miles) above the Earth’s surface. In this layer, the temperature decreases with increasing altitude.

  4. Thermosphere: The thermosphere is the next layer, extending from about 85-600 kilometers (53-373 miles) above the Earth’s surface. This is where the International Space Station orbits the Earth. The temperature in this layer increases with increasing altitude due to absorption of high-energy solar radiation.

  5. Exosphere: The outermost layer of the Earth’s atmosphere is the exosphere, which extends beyond the thermosphere. In this layer, the particles are very sparse, and it gradually merges with the vacuum of space.

It’s important to note that the boundaries between these layers are not sharp and can vary depending on factors such as latitude, season, and solar activity. However, this is the general representation of the layers from closest to the Earth’s surface to the farthest.