The coldest layer of the atmosphere located above the stratosphere is the mesosphere. Temperatures in the mesosphere can drop as low as -90 degrees Celsius (-130 degrees Fahrenheit) due to its high altitude and low density of gases.
You are asking for comparatives. Each state can be any when compared to another state except the extremes. Liquid or gas either lower or higher depending on what you compare it to.
what is the high concentration of the other metal in the mesosphere
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No, the temperature in the mesosphere actually decreases with altitude. The mesosphere is the third layer of Earth's atmosphere, located above the stratosphere, and it is where temperatures can drop as low as -90 degrees Celsius due to its decreasing density and distance from the Earth's surface.
The coldest layer of the atmosphere located above the stratosphere is the mesosphere. Temperatures in the mesosphere can drop as low as -90 degrees Celsius (-130 degrees Fahrenheit) due to its high altitude and low density of gases.
The air pressure in the mesosphere is low compared to the pressure at lower altitudes. This is because the mesosphere is located at an altitude where the density of the atmosphere is much lower, resulting in lower air pressure.
The temperature in the mesosphere can vary greatly, but on average it can range from about -90°C to -120°C (-130°F to -184°F). This layer of the atmosphere is known for its extremely low temperatures due to its high altitude and low density.
The air density in the mesosphere, which extends from about 50 to 85 kilometers (31 to 53 miles) above the Earth's surface, decreases with altitude. At the lower boundary, the density is approximately 0.01 kg/m³ and can drop to about 0.001 kg/m³ near the mesosphere's upper limits. This low density is due to the decreasing pressure and temperature as altitude increases in this layer of the atmosphere.
The density of the mesosphere is lower than the density of the trophosphere or stratosphere. As you go higher into the atmosphere, the density decreases.
The density in the mesosphere, which extends from about 50 to 85 kilometers (31 to 53 miles) above Earth's surface, decreases with altitude. At its lower boundary, the density is approximately 0.1 kg/m³, and it continues to decline as one moves higher. This layer is characterized by temperatures that decrease with altitude, contributing to the low density of air in this region. Overall, the mesosphere has significantly lower density compared to the layers above and below it.
The mesosphere is the third layer of Earth's atmosphere and is characterized by its very low density. The density of the mesosphere ranges from about 1 x 10^-10 kg/m^3 to 1 x 10^-13 kg/m^3 at different heights within the layer.
Charcoal has a low density because it is porous and lightweight.
The thermosphere is located between the mesosphere and exosphere in Earth's atmosphere. Temperatures in the thermosphere can reach very high levels due to absorption of solar radiation, but the air density is extremely low. This region is also where the auroras occur.
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Quite low density: 0.968 g·cm−3
The coldest layer of the Earth's atmosphere is the mesosphere, located between the stratosphere and thermosphere. Temperatures in the mesosphere can drop as low as -90 degrees Celsius (-130 degrees Fahrenheit) due to its low density and distance from the sun.