The atmosphere
The bands of high-speed winds about 10 kilometers above Earth's surface are called jet streams. These fast-flowing air currents are typically located in the upper troposphere and are important for the movement of weather systems.
If the Earth's surface is cold, it will lead to cooling of the air above it due to direct contact and heat transfer. The cold surface will cause the air above it to become cooler, which can affect weather patterns, lead to the formation of fog or dew, and impact temperature gradients in the atmosphere.
Air pressure is greatest at the Earth's surface because the weight of the air above exerts a force on the air below. As you move higher in the atmosphere, there is less air above pushing down on you, so the pressure decreases. At higher altitudes, there are fewer air molecules, resulting in lower air pressure.
The upper surface of water is called the water's surface or water level. It is the boundary where the water meets the air above it.
As the distance from Earth's surface increases, the air pressure decreases. This is because there is less air above pushing down on the air below. The decrease in air pressure is why it becomes harder to breathe at higher altitudes.
The air is thinner the higher you go.
mercury
Fog, mist.
A temperature inversion.
Atmospheric pressure is caused by the force of the air above the earths surface. It is measured by the point in which the air meets the atmosphere.
The weight of the air on Earth's surface is approximately 14.7 pounds per square inch (psi), or 101.3 kilopascals (kPa). This pressure is due to the force exerted by the column of air above us, known as atmospheric pressure.
Because there is more air (which has weight) above you if you are around sea level. If you fly up, or climb a mountain, there is less air above you, therefore less air pressure.
because its hard to breathe thin air above earths surface, the higher you go its hard to breathe oxygen.
The bands of high-speed winds about 10 kilometers above Earth's surface are called jet streams. These fast-flowing air currents are typically located in the upper troposphere and are important for the movement of weather systems.
The dense air sinking towards the Earth's surface is called subsidence. Subsidence can lead to high pressure systems and stable weather conditions.
If the Earth's surface is cold, it will lead to cooling of the air above it due to direct contact and heat transfer. The cold surface will cause the air above it to become cooler, which can affect weather patterns, lead to the formation of fog or dew, and impact temperature gradients in the atmosphere.
how does air above cold surface move