None whatsoever. The terrain has an effect on the weather but it can't be resumed as precipitation per altitude because what works one way with the wind from one direction, may work the other way with the wind from another direction.
The effect of the terrain on the weather is called the orographic effect, from oro-, that means 'mountain' in Greek. As the air rises, being pushed up over a mountain range, the air cools down by adiabatic effect and moisture condenses into clouds and, perhaps, precipitations. On the lee side of the mountain, the air sinks and if it has lost much of its moisture in precipitation, it does it at the dry adiabatic lapse rate, which is twice that of moist air. It means that it is warmer at the lee side of the mountain. This is called a Foehn wind, in Europe, and a Chinook wind in Canada and the US.
Depending of the altitude of the land and how steep the rise is, it may rain on the weather side, or on a plateau, on the top. Sometimes it is not enough to produce precipitations, only what is called orographic fog. For example, I visited Sao Antonio on the Cape Verde islands and while the islands are extremely dry, they manage to grow some vegetables on the top of the volcanic mountains because there is a constant fog and plants absorb the dew on their leaves.
Not too sure if this is correct. Research more before writing this down. fanks babes.
Convection rainfall occurs when warm air rises, cools, condenses, and forms clouds. Orographic rainfall happens when moist air is forced to rise over a barrier like a mountain, cooling and creating precipitation on the windward side. Both processes result in rainfall, but the cause of the rising air and subsequent cooling differs between the two.
The relationship between precipitation and humidity affects weather patterns in a region because higher humidity levels can lead to more moisture in the air, which can result in increased chances of precipitation like rain or snow. This can influence the type and amount of precipitation a region receives, ultimately shaping its weather patterns.
Frontal rainfall occurs when warm and cold air masses meet, leading to the warm air rising and cooling, causing condensation and precipitation. Orographic rainfall happens when moist air is forced to rise over a barrier, such as a mountain range, leading to cooling, condensation, and rainfall on the windward side of the barrier.
Runoff abstractions refer to the portion of precipitation that is prevented from entering a water body due to interception, infiltration, or evaporation. It is essentially the amount of water that does not contribute to surface runoff. The relationship between runoff abstractions and precipitation is that as precipitation increases, the amount of water available for abstractions also increases, potentially impacting the overall runoff volume.
Orographic lifting occurs when an air mass is forced to rise over a topographic barrier, such as a mountain range. The rising air mass expands and cools, with water condensing and forming droplets as the temperature drops below the dew point.
BHS?
The relationship between elevation and climate has to do with temperature. The higher up the elevation is the colder the temperature is.
Temperature decreases as the elevation increases.
the sky
by the water
As a general rule in the atmosphere, the higher the elevation the lower the temperature. However, certain atmospheric conditions may produce an 'inversion', where temperature increases with elevation.
If the base of the elevation is at a distance d from the observer, then the highest point is at a height = d*tan(angle of elevation)
The relationship between water pressure and elevation is that as elevation increases, water pressure decreases. This is because the weight of the water above exerts less force at higher elevations. The change in water pressure per foot of elevation is approximately 0.433 pounds per square inch (psi) for every foot of elevation gained.
As elevation increases, temperature tends to decrease at a rate of about 3.5°F per 1,000 feet gained in elevation. This relationship is known as the lapse rate and is influenced by factors such as air pressure, humidity, and geography.
Convection rainfall occurs when warm air rises, cools, condenses, and forms clouds. Orographic rainfall happens when moist air is forced to rise over a barrier like a mountain, cooling and creating precipitation on the windward side. Both processes result in rainfall, but the cause of the rising air and subsequent cooling differs between the two.
The relationship between precipitation and humidity affects weather patterns in a region because higher humidity levels can lead to more moisture in the air, which can result in increased chances of precipitation like rain or snow. This can influence the type and amount of precipitation a region receives, ultimately shaping its weather patterns.
Frontal rainfall occurs when warm and cold air masses meet, leading to the warm air rising and cooling, causing condensation and precipitation. Orographic rainfall happens when moist air is forced to rise over a barrier, such as a mountain range, leading to cooling, condensation, and rainfall on the windward side of the barrier.