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Why does the windward side of a mountain receive more rain than the leeward side?
This is false most of the precipitation from moisture laden winds from the sea does not fall on the leeward side of mountains. Many deserts are located in the interior of continents, far from moisture- laden winds blowing from the ocean.
What is the temperature range in the Thar Desert?
The Hadley Cell affects temperatures in the desert because air rises, cools and condenses over the rainforests at 0° and warm dry air descends over the tropics because the moisture has been used up. Deserts are usually found at the tropics in rain shadows. Rain shadows are areas on the other side of a mountain, or an area of high ground, where there is no relief rainfall. Warm moist air rises, cools and condenses over the mountain so it rains at the top, and dry warm air descends on the other side. There is no moisture left, and so there is no rain. This area is called a rain shadow, and this is where deserts usually are. The atmosphere contains little humidity to block the Sun's rays and desert surfaces receive a little more than twice the solar radiation received by humid regions.
What was the mood during the blind side?
The mood of the blind side is warm for a place to let Michael live, bedroom, and with lots courage to Michael from learning .
How do fronts cause weather changes?
When fronts meet, the cool air undercuts the warm air and causes the warm air to rise and create tornadoes, associated with rain.
Pressure differences between warm and cold air masses cause what?
Pressure differences between warm and cold air masses cause fronts or high/low pressure systems. A warm front is when a warm, moist air mass slides up and over a cold air mass, and a cold front is the opposite.
What happens to warn moist air which rises up the western side of a mountain?
The warm moist air rises along the western side of the mountain, cools as it gains altitude, and condenses, forming clouds and precipitation. This process is known as orographic lifting, and it leads to increased rainfall on the windward side of the mountain.
Why is the leeward side of a mountain warm?
The leeward side of a mountain is warm because as air moves up and over the mountain, it loses moisture and heat, resulting in warmer and drier air on the leeward side. This process is known as the rain shadow effect and contributes to the warmer temperatures experienced on the leeward side of the mountain.
What happens to warm moist air which rises up the western side of a mountain?
As warm, moist air rises up the western side of a mountain, it cools due to the decrease in atmospheric pressure at higher altitudes. This cooling causes the moisture in the air to condense, forming clouds and often resulting in precipitation. This process is known as orographic lift. Once the air descends on the eastern side of the mountain, it warms up and becomes drier, leading to a rain shadow effect.
What happens warm air hits the side of a mountain?
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.
What is it when warm air flows up a mountain during the day?
This process is called upslope flow, where warm air rises up a mountain slope due to heating from the Sun. As the warm air ascends, it cools, condenses, and forms clouds, potentially leading to precipitation on the windward side of the mountain.
How do convection currents form downdrafts in deserts near tall mountain ranges?
Warm air expands and rises from the base on one side of the mountain. It cools and contracts in the clouds above the mountain and sinks back down but on the desert side of the mountains. This way both sides of the mountain are heated properly.
The rain shadow effect occurs because?
moist air flows over a mountain range and cools, causing it to release precipitation on the windward side. As the air descends down the leeward side of the mountain, it warms and loses moisture, creating a rain shadow where little precipitation falls.
Is there a lot of humidity when air mass rises up a mountain side?
When an air mass rises up a mountain side the air cools as it rises. Cool air can not hold as much moisture as warm air so the humidity will increase until the dew point is reached whereupon the water will come out of the air (as mist/clouds and rain/snow). On the other side of the mountain the air comes down again and as it has lost its water it is now very dry this side of the mountain is called a rain shadow.
When a warm moist air mass moves toward a mountain range what happens?
As the warm moist air mass rises over the mountain range, it cools and condenses, leading to the formation of clouds and precipitation on the windward side of the mountains. This process is known as orographic lifting and can result in heavy rainfall on the mountainsides. On the leeward side of the mountains, the air mass descends and warms, creating a rain shadow effect with drier conditions.
Windward and leeward side of a mountain?
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).
Explain with the aid of a diagram how relief rainfall occurs?
Relief rainfall occurs when moist air is forced to rise over a mountain barrier. As the air rises, it cools and condenses to form clouds and eventually rain. The diagram would show warm, moist air approaching the mountain, rising, cooling, condensing, and then raining on the windward side of the mountain. The leeward side of the mountain would be in a rain shadow, receiving significantly less rainfall.
How does the rainfall differ on the windward and leeward sides of a mountain?
The windward side of a mountain typically receives more rainfall because as moist air rises up the mountain, it cools and condenses, leading to precipitation. On the leeward side, the air is drier and descends, which causes it to warm and retain less moisture, resulting in a rain shadow effect and less rainfall.
