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A thermometer may show a low temperature in the thermosphere because the density of particles is so low that it cannot effectively transfer heat to the thermometer. The thermosphere is highly influenced by solar activity, leading to high temperatures despite the low density of particles.
The thermosphere is an upper layer of the atmosphere where the heavier molecules (notably oxygen) are dense enough to absorb a significant part of the high-intensity radiation from the Sun. But this part of the atmosphere is still so thin than an object placed there would encounter very few of the high-energy (high temperature) molecules. Despite the air molecules present, the thermosphere is essentially a vacuum. The International Space Station orbits within the thermosphere, at an altitude of 280 to 460 kilometers (175 to 285 miles). The range of the thermosphere is from about 100 to 600 kilometers (60 to 360 miles) above the Earth's surface.
The temperature in the Thermosphere can rise to 2,000° C.
As you move from the Earth's surface to the lower thermosphere, the temperature generally decreases with increasing altitude in the troposphere and mesosphere due to the decreasing density of air molecules. However, in the stratosphere, the temperature can increase with altitude due to the absorption of solar radiation by ozone. In the thermosphere, temperatures can vary widely depending on solar activity, reaching very high temperatures due to interactions with solar radiation.
Individual molecules of gas might be very hot, but there are too few of them to affect a thermometer much. Then the energy lost through black body radiation is more than the energy gained from the few molecules around it, making the thermometer temperature decrease until the lower equilibrium temperature is reached.
Because the particles in the thermosphere are very spaced out. A normal thermometer would even measure it below zero, but it has a very high temperature.
The Thermosphere feels very cold to us because of its low Thermal Energy.There are very few particles in the Thermosphere, so even if they were very, very hot, it would feel cold.
A thermometer may show a low temperature in the thermosphere because the density of particles is so low that it cannot effectively transfer heat to the thermometer. The thermosphere is highly influenced by solar activity, leading to high temperatures despite the low density of particles.
the thermosphere gets it's name from it's extrmely high temperature, which cn be above 1,000'c.
yes
Because it gets drunk
In the thermosphere, temperature increases with altitude due to the absorption of high-energy solar radiation by the sparse gas molecules present at that height. Despite this temperature increase, the thermosphere may feel very cold to us as the low density of molecules means that there is not enough matter to transfer heat efficiently.
The thermosphere is the layer of the atmosphere that can reach temperatures of up to 2000 degrees Celsius. This high temperature is due to the absorption of solar radiation by gases in this region. The air in the thermosphere is very thin, and high-energy solar particles contribute to the extreme heat.
Temperatures in the thermosphere can vary widely, ranging from about 500°C (932°F) during the day to 2000°C (3632°F) or more during periods of high solar activity. However, it is important to note that the thermosphere is not like a typical environment on Earth where we feel the temperature – the sparse density of gas molecules means that the "hot" thermosphere would not feel hot to our skin.
The thermosphere is an upper layer of the atmosphere where the heavier molecules (notably oxygen) are dense enough to absorb a significant part of the high-intensity radiation from the Sun. But this part of the atmosphere is still so thin than an object placed there would encounter very few of the high-energy (high temperature) molecules. Despite the air molecules present, the thermosphere is essentially a vacuum. The International Space Station orbits within the thermosphere, at an altitude of 280 to 460 kilometers (175 to 285 miles). The range of the thermosphere is from about 100 to 600 kilometers (60 to 360 miles) above the Earth's surface.
The thermosphere has high temperature because the few molecules present can absorb high-energy solar radiation. However, since there are so few molecules, the heat energy is not readily transferred to a thermometer, so it would not feel hot to us.
The temperature in the Thermosphere can rise to 2,000° C.