hot and dry
The windward side of a mountain is typically the west side of the mountain, receiving the various weather as weather moves west to east. The leeward side of a mountain opposes the windward side, making it the east side of the mountain, receiving little weather, blocking weather (rain) and warming air rapidly as it moves down this side of the mountain. The leeward side of mountains causes deserts, dry places, little rain, etc., for it releases warm air unto these places, and blocks weather (rain) from moistening them (I.E. Las Vegas, etc. on the eastern side of the mountain ranges).
The difference is that windward gets more rain, is wetter, and is the side of the mountain that is closest to the ocean. On the other hand the leeward is the farthest from shore and is drier but still gets rain.
Condensation occurs on the windward side of a mountain because the rising air cools by adiabatic expansion, so the air becomes saturated and the water vapor condenses. The lee side is dry because the air that has had its moisture squeezed out in going over the mountain warms by compression, so becomes relatively drier.
what 2 mountain ranges are located in india?
A mountain system is an area of interconnected mountain ranges. The mountain system has a series of ranges linked together by geological features.
The two sides of a mountain range are typically referred to as the windward side and the leeward side. The windward side faces the prevailing winds and receives more precipitation, while the leeward side is sheltered from the wind and tends to be drier.
Mountain ranges can affect climate by blocking the movement of air masses, leading to differences in temperature and precipitation on either side of the range (rain shadow effect). Mountains can also enhance cloud formation and precipitation through orographic lifting. Additionally, mountains can create microclimates due to changes in elevation, slope, and aspect.
the coastal mountain ranges stand between it and the Pacific Ocean
Mountain ranges can influence climate by blocking moisture-laden air, leading to rainfall on one side (windward side) and creating a rain shadow on the other side (leeward side) with less rainfall. They can also affect temperature by creating different microclimates at different elevations, causing temperature changes with altitude. Additionally, mountain ranges can act as barriers to air masses, influencing wind patterns and regional climate systems.
can be ranges
rain shadows usually occur on the leeward side of the mountain ranges.
rain shadows usually occur on the leeward side of the mountain ranges.
The windward side of a mountain is typically the west side of the mountain, receiving the various weather as weather moves west to east. The leeward side of a mountain opposes the windward side, making it the east side of the mountain, receiving little weather, blocking weather (rain) and warming air rapidly as it moves down this side of the mountain. The leeward side of mountains causes deserts, dry places, little rain, etc., for it releases warm air unto these places, and blocks weather (rain) from moistening them (I.E. Las Vegas, etc. on the eastern side of the mountain ranges).
Mountain ranges usually have a cold climate in its surrounding areas. They also help diminish winds coming in from the seas.
because there pretty
the answer is tha pressure of the mountain ranges or low land is minus it is 7 degreee
cascade range, coastal range