Warmer
cooler
Created when warm, moist air is forces to rise over a barrier. (mountain).
A rain-shadow is on the leeward side of the mountain. Most of the rain will fall on the windward side, before the clouds can rise over the mountain. This means that there is little rain left for the leeward side.
Orographic precipitation occurs when an air mass is forced to rise over a mountain barrier, leading to cooling and condensation, which results in precipitation on the windward side of the mountain.
Califronia has 100 mountain peaks and the tallest mountain goes over 10000 feet! hope it helps
The rain shadow effect occurs when moist air is forced to rise over a mountain range, causing it to cool and release precipitation on the windward side of the mountain. As the air descends on the leeward side, it becomes warmer and drier, creating a rain shadow where little precipitation falls. This results in a contrast in vegetation and climate on either side of the mountain range.
This phenomenon is known as orographic rainfall. As moist air is forced to rise over a mountain range, it cools and condenses, leading to greater rainfall on the windward side or the side facing the prevailing wind. The leeward side, or the side sheltered from the wind, experiences less precipitation as the air descends, warms, and becomes drier.
The slope of a line increases when the line becomes steeper, meaning that the rise over run ratio of the line becomes larger. This can happen when the line becomes more vertical. Conversely, the slope decreases when the line becomes less steep, which occurs when the line becomes more horizontal.
If you're talking about slope, it is rise over run. But why is it not the other way run over rise?
Yes, a mountain can form when a volcanic eruption occurs under the ocean, as the accumulation of volcanic material can build up over time and create an underwater mountain. Over millions of years, this underwater mountain can rise above sea level, forming an island or a larger landmass.
The windward side of a mountain typically receives more precipitation due to orographic lifting, which occurs as air is forced to rise over the mountain. This can create a wetter, cooler climate with more vegetation and potentially more cloud cover on the windward side of the mountain.
Neville Chamberlain