Answer:
I hope this will help you out.
Explanation:
Since warm air can hold more water vapor than cool air, raising or lowering temperature can change air's relative humidity. The temperature at which air becomes saturated with water is called the air's dew point.
Answer:
e
Explanation:
the correcto asnmwer is ed
Answer:
subsidence. sinking of rock layers. tension. stress at a divergent plate boundary.
Answer:
he motion of air through atmosphere is atmospheric circulation. It is depend on three things: energy from the sun, the rotation of the Earth on its axis, and topography.
Explanation:
The motion of air through atmosphere is atmospheric circulation. It is depend on three things: energy from the sun, the rotation of the Earth on its axis, and topography.
The sun shines more closely on fields near the equator due to the tilting of earth. The air above such areas spreads and increases with more energy from the sun As it grow rises far from the ground, it cools down and is driven away by warmer air
. At near 30 degree latitude, the dense (cool) air falls to the surface, where it moves back towards the equator. This type of circular motion called a Hadley Cell.
More air dropping at a latitude around 30 degrees continues to remain north or south. When it approaches the latitude of 60 degrees, it meets much dense air from the poles. This point of impact is known as the Polar Front.
<span>Erosion is the displacement of solids (soil, mud, rock and other particles) by the agents of wind, water or ice, by downward or down-slope movement in response to gravity or by living organisms (in the case of bioerosion).
Deposition, also known as sedimentation, is the geological process whereby material is added to a landform. This is the process by which wind, water or ice create a sediment deposit, through the laying down of granular material that has been eroded and transported from another geographical location.
Deposition occurs when the forces responsible for sediment transportation are no longer sufficient to overcome the forces of particle weight and friction, which resist motion. Deposition can also refer to the build up of a sediment from organically derived matter or chemical processes. For example, chalk is made up partly of the microscopic calcium carbonate skeletons of marine plankton, the deposition of which has induced chemical processes (diagenesis) to deposit further calcium carbonate.</span>