Above 100,000 feet altitude (20 miles).
The higher the altitude the lower the temperature.
Cirrus clouds are wispy and high-altitude clouds composed of ice crystals. They are often associated with fair weather. Cumulonimbus clouds are vertically-developed clouds that can bring thunderstorms, heavy rain, and severe weather. They have a dense, towering appearance.
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.
low height. below sea level
Green is a non example of altitude.
This characteristic is called altitude or elevation.
Well, darling, a non-example of altitude would be something like the temperature of a boiling pot of water or the color of a ripe banana. Basically, anything that has absolutely nothing to do with how high or low something is above sea level. Hope that clears things up for you!
Length, weight, color
One characteristic of non-metals is that they are generally gaseous at room temperature. Non-metals will also typically bond with metals easily.
PHYSICAL (smell, color, texture, size, etc)--NON CHARACTERISTIC GENERAL (general stuff about the substance all together)-CHARACTERISTIC Characteristic properties help us identify pure substances or the group it belongs to. Non-characteristic properties cannot help us identify pure substances or the group it belongs to.
One main characteristic of non-Euclidean geometry is hyperbolic geometry. The other is elliptic geometry. Non-Euclidean geometry is still closely related to Euclidean geometry.
3 non characterstic prperties of water would be :
The characteristic that distinguishes living things from non-living things is the ability to grow, reproduce, and respond to stimuli.
Air pressure decreases uniformly with altitude in the standard atmosphere model. However, in the real atmosphere, variations such as temperature inversions or weather systems can cause non-uniform changes in air pressure with altitude in specific regions and times.
It's characteristic