They cool or it gets colder
When warm air hits the side of a mountain, it is forced to rise due to the slope. As the air rises, it cools adiabatically, leading to the formation of clouds and precipitation on the windward side of the mountain. This process is known as orographic lifting and can result in significant rainfall or snowfall.
Traveling on a road that winds around a mountain allows the car to gradually ascend at a gentler slope, reducing the strain on the vehicle's engine and transmission. In contrast, a road that goes straight up one side of the mountain requires the car to overcome a steep incline, which can put more stress on the engine, increase fuel consumption, and potentially cause overheating.
The fact that the a tornado spins means that the winds move in all directions at different points within the tornado, as they make a full 360 degree rotation. In the northern hemisphere tornadoes spin counterclockwise, so winds on the north side of a tornado blow east to west, those on the west side blow north to south, those on the south side blow west to east, and those on the east side blow south to north. This is reversed in the southern hemisphere where tornadoes spin clockwise.
As the air moves down the leeward side of a mountain, it gets compressed due to higher pressure at lower altitudes. This compression leads to increased temperature and decreased relative humidity, causing the air to warm up and dry out. This process is known as the Foehn effect.
As the air is forced to rise over the mountain range, it undergoes adiabatic cooling, leading to the condensation of water vapor and the formation of clouds and precipitation on the windward side of the mountain. This process is known as orographic lifting and can result in enhanced rainfall on the windward side and a rain shadow effect on the leeward side of the mountain.
The prevailing winds will force the clouds to climb when they reach the mountain range. As the clouds rise they drop their moisture. So the windward side of the mountain will get rain, and the leeward side of the mountain will be drier.
The prevailing winds will force the clouds to climb when they reach the mountain range. As the clouds rise they drop their moisture. So the windward side of the mountain will get rain, and the leeward side of the mountain will be drier.
windward
Prevailing winds can bring moisture and temperature changes to different regions, affecting precipitation patterns and temperatures. Mountain ranges can block prevailing winds, leading to the creation of rain shadows where one side of the mountain receives more precipitation, while the other side experiences drier conditions. This can result in distinct climate differences on either side of the mountain range.
The downwind side of a mountain is known as the leeward side of the mountain. This is where deserts and steppes begin to form due to the rain shadow.
Because all the moisture falls on the side where the prevailing winds come from (windward side).
As prevailing winds rise up a mountain range, they cool and condense, leading to increased precipitation on the windward side. This phenomena is known as orographic precipitation. As the air descends on the leeward side, it warms and dries out, creating a rain shadow effect that results in decreased precipitation on that side of the mountain range.
it becomes a leeward.
deserts
the windward side gets lot of rainfall
The warm dry winds that blow down the side of the mountain (leeward side) are known as Foehn Winds.
i thinks is snow