At an altitude of 550 kilometers, you are well into the thermosphere, where temperatures can reach up to 1,500 degrees Celsius (2,732 degrees Fahrenheit) or even higher. However, due to the very low density of air at this altitude, this temperature does not feel hot in the way it would at lower altitudes. Instead, the sparse air molecules absorb and retain heat differently, making it a unique environment.
Mount St. Helen had an altitude of 2 950 m before the eruption.After the eruption the altitude decreased to 2 550 m.
At standard temperature.
Temperature will decrease as the altitude increases at all levels due to the thinning of atmospheric gasses.
The altitude cannot be determined based solely on temperature and relative humidity. Altitude is primarily based on air pressure, not temperature and humidity. Additional information, such as air pressure or location, would be needed to accurately determine altitude.
The rate at which temperature decreases with increasing altitude is known as the lapse rate.
the temperature in the atmosphere approaches -90 degrees Celsius at an altitude of about answer is 80 kilometers
The lowest part of the thermosphere is called the lower thermosphere, which extends from about 80 to 550 kilometers above the Earth's surface. This region is characterized by a rapid increase in temperature as altitude increases.
Mount St. Helen had an altitude of 2 950 m before the eruption.After the eruption the altitude decreased to 2 550 m.
Answer: 550 yd = 0.50292 km
The mesosphere starts at an altitude of about 31 miles (50 kilometers) above the Earth's surface and extends up to about 53 miles (85 kilometers) high. This layer is characterized by decreasing temperatures with altitude.
550 meters is 0.55 kilometers.
The higher the altitude the lower the temperature.
A 0.52 kg bird flying at an altitude of 550 m
the way the altitude changes the temperature changes
550
Around 80 km in height in the mesosphere is the third layer of the atmosphere of Earth. The temperature decreases as you go up, as in the troposphere. It can be up to -90 ° C. It is the coldest part of the atmosphere.
In the exosphere, temperature increases with altitude. This is because the particles in the exosphere are far apart, so there is no transfer of heat through conduction or convection. Instead, the few particles present gain energy from solar radiation, causing an increase in temperature as altitude increases.