With increasing altitude in the atmosphere, pressure decreases and so does density. Temperature varies depending on the layer in which the air is. The top of the stratosphere can be -50 degrees C, as where the thermosphere can be well over 500 degrees C.
At ground level (0 feet above sea level) we consider a standard pressure reading to be 29.92 inches of Mercury. At 1000 feet above sea level this pressure would be reduced to 29.82. This is a basic principle of Altimeters for aircraft.
Temperature is slightly trickier, but we also have what is called a standard lapse rate. The factors here depend on many things, but a rule of thumb is about 3 degrees (F) per thousand feet. Using this rule of thumb, you can find the base cf clouds (roughly) by looking at the dew point verses the temp. If the difference is large, clouds will be high. If the difference is small (say 3 Degrees) the clouds will be low, around 1000 feet.
The ozone units is hanging ten on the wave
As the depth increases, the density increases
density determines the state of matter something will be in.
How is density related to the layer if the earth
it has gravity
Its in layers because of the density of the compounds in the earth
the earth freezers layers after density stratification which consists of the core, mantle, and crust
iner core outer core
Density and the composition of the different layers affect the behavior of seismic waves.
The crust is the least dense of the Earth's layers. Each layer is denser than the layer above it. This is very logical, since lighter layers float on top of heavier layers.
Its in layers because of the density of the compounds in the earth
The moon's average density is about the same as the density of mantle of the Earth.
The Earth has layers because it is made up of materials of varying density.
Yes, layers of the Earth haven't identical density.
No
the earth freezers layers after density stratification which consists of the core, mantle, and crust
The core is the densest layer.
The density of Earth's layers
iner core outer core
The density and state of the subtance of the particular layer.
The Crust
Density and the composition of the different layers affect the behavior of seismic waves.