Above 100,000 feet altitude (20 miles).
The higher the altitude the lower the temperature.
Altitude describes an object's position relative to sea level. An object in a position higher than sea level would have a positive altitude, sea level would have an altitude of zero, and any object below sea level would have a negative altitude.
Density Altitude is the altitude relative to the standard atmosphere conditions (ISA) at which the air density will be equal to the indicated at the place of observation.
The Challenger explosion occurred at an altitude of about 46,000 feet.
Yes
Mount Fuji
An airplane with a high climb rate will provide the greatest gain in altitude in the shortest distance after takeoff. This means it can climb quickly and efficiently, getting to a higher altitude in a shorter amount of time and distance compared to an airplane with a lower climb rate.
The atmospheric pressure is greatest at sea level, which is at the Earth's surface. As altitude increases, atmospheric pressure decreases.
The Netherlands has the greatest percentage of land at an elevation below 200 meters altitude, with a significant portion of the country being below sea level. Other countries with large areas below 200 meters altitude include Bangladesh and some coastal regions in countries like Egypt and Vietnam.
Air density is greatest at lower altitudes, such as sea level. As you increase in altitude, the density of the air decreases due to the decrease in atmospheric pressure.
The absolute ceiling
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Currently, Mount Everest is measured as standing 8846 meters (29,028 ft) above sea level.
Air pressure does not vary significantly depending on whether you are at the beach or elsewhere. However, factors such as altitude and weather conditions can affect air pressure.
Air pressure is typically greatest at sea level, where it averages around 1013.25 millibars. As altitude increases, the air pressure decreases due to the reduction in the weight of the air column above.
The thermosphere is the layer of the atmosphere that has the greatest range in temperature, with temperatures increasing with altitude due to the absorption of solar radiation. Temperature in the thermosphere can vary from below -100°C at the bottom to over 2,500°C at higher altitudes.