UV radiations hit the ozone layer in the stratosphere. The energy is turned into heat energy. The mesosphere has no heat source in itself and is far away from the Earth and the Sun. Both heat sources.
Ozone (O3) is a gas that causes an increase in temperature in the stratosphere. This is because ozone absorbs incoming ultraviolet (UV) radiation from the sun, which heats up the stratosphere.
In the stratosphere, the temperature increases with altitude. This is due to the absorption of ultraviolet radiation by the ozone layer, which warms the upper stratosphere. As you ascend, the air becomes less dense, and the increased energy from the ozone causes the temperature to rise, contrasting with the troposphere below, where temperature typically decreases with altitude.
The temperature of the stratosphere increases primarily due to the absorption of ultraviolet (UV) radiation by ozone molecules. As UV radiation from the sun is absorbed, it causes the ozone layer to warm up, leading to an increase in temperature in the stratosphere. This temperature inversion is a key characteristic of the stratosphere, contrasting with the troposphere below, where temperature typically decreases with altitude.
In a divergent nozzle, pressure will decrease as the flow area increases. This is due to the conservation of mass principle, where an increase in area causes a decrease in velocity and thus a decrease in pressure according to Bernoulli's equation.
The decrease of ozone causes UV to enter the earth. These are fatal radiations of the sun.
In the stratosphere, temperature increases with height due to the absorption of ultraviolet (UV) radiation by the ozone layer, which warms this region. In contrast, the mesosphere sees a decrease in temperature with height because it is farther from the Earth’s surface and lacks significant heat sources, leading to less absorption of solar energy. As a result, the mesosphere is cooler, especially at its upper levels.
The stratosphere is warmer than the mesosphere because it contains the ozone layer, which absorbs and retains heat from the sun. This causes the temperature to increase with altitude in the stratosphere. In contrast, the mesosphere is colder because it is above the ozone layer and lacks significant heat-absorbing molecules.
Ozone (O3) is a gas that causes an increase in temperature in the stratosphere. This is because ozone absorbs incoming ultraviolet (UV) radiation from the sun, which heats up the stratosphere.
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In the stratosphere, the temperature increases with altitude. This is due to the absorption of ultraviolet radiation by the ozone layer, which warms the upper stratosphere. As you ascend, the air becomes less dense, and the increased energy from the ozone causes the temperature to rise, contrasting with the troposphere below, where temperature typically decreases with altitude.
When air rises, it expands and cools, which causes its density to decrease. Conversely, when air descends, it compresses and warms, which causes its density to increase.
The temperature of the stratosphere increases primarily due to the absorption of ultraviolet (UV) radiation by ozone molecules. As UV radiation from the sun is absorbed, it causes the ozone layer to warm up, leading to an increase in temperature in the stratosphere. This temperature inversion is a key characteristic of the stratosphere, contrasting with the troposphere below, where temperature typically decreases with altitude.
The answer is simple: Food.
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The increase in magnification cause a decrease in the field of view.
Ammunition and cleaning are the two biggest causes.
Fire and fire prevention.