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Why are the on coastal sides of a mountain often foggy?
The cool air from the ocean is forced up the mountain slopes, where it cools and condenses to form fog. This process, known as orographic lifting, occurs because the air on the ocean side of the mountain is moister and cooler than the air on the other side. As a result, coastal sides of mountains often experience foggy conditions.
How would a prevailing north wind affect the climate?
A prevailing north wind would generally bring colder temperatures to a region, especially if the wind originates from polar or arctic regions. It may also cause increased cloud cover and precipitation on the windward side of mountain ranges. Overall, it could result in cooler and potentially wetter conditions depending on the specific location and weather patterns.
How are lenticular galaxies formed?
Those are the clouds that look like flying saucers. I love them a lot. They’re usually formed in mountainous environments—the relatively moist air from lower in the atmosphere flows up the mountain and cools down significantly, making it condense into a cloud in that iconic saucer shape.These clouds are somewhat elusive because they’re typically short-lived and localized. As the air moves down the other side of the mountain and sinks lower in the atmosphere, it “dries out,” and the cloud disappears.So now if you see one, you’ll know what it is, but you can still pretend it’s a spaceship. I sure will.
A student thinks that the sun is hidden behind the clouds at night why is this unlikely?
The sun does not hide behind the clouds at day because the sun goes around the Earth. It is night time when the sun is on the other side :) im intelligent. ... hahahah
Does cumulus cloud give rain?
You have only to look up into the sky to try your luck at weather forecasting. Clouds give us a clue about what is going on in our atmosphere and how the weather might change in the hours or even days to come. Each type of cloud forms in a different way, and each brings its own kind of weather.Cool CondensationClouds are water. As you probably know, we can find water in three forms: liquid, solid and gas. Water as a gas is called water vapor. Clouds form when water vapor turns back into liquid water droplets. That is called condensation. It happens in one of two ways: when the air cools enough, or when enough water vapor is added to the air. You've seen the first process happen on a summer day as drops of water gather on the outside of a glass of ice tea. That's because the cold glass cools the air near it, causing the water vapor in the air to condense into liquid. Unlike the drops on the side of your glass though, the droplets of water in a cloud are so small that it takes about one million of them to form a single raindrop. Most clouds form this way, but the cooling comes not from ice in a glass, but as the air rises and cools high in the sky. Each tiny cloud droplet is light enough to float in the air, just as a little cloud floats out from your breath on a cold day.Too Clean for Clouds?Our air has to be just a little bit dirty for clouds to form. That's because water vapor needs a surface on which to condense. Fortunately, even the cleanest air has some microscopic particles of dust, smoke or salt for water droplets to cling to, so the air is rarely too clean for clouds to form.Cloud ClassificationsMeteorologists name clouds by how high in the sky they form and by their appearance. Most clouds have two parts to their name. Usually the first part of the name has to do with the height and the second part refers to the appearance.If clouds form at the highest levels, they get the prefix "cirro" as the first part of their name. Middle clouds get the prefix "alto." Low clouds don't get a prefix.There are two cloud appearance types: cumulus and stratus, which are also the basic names of the low clouds. Sometimes they appear higher in the atmosphere and get a combination name with a prefix. For example, middle cumulus clouds are called "altocumulus" and high stratus clouds are "cirrostratus." If a cloud produces rain or snow it gets either "nimbo" at the beginning or "nimbus" at the end.Cumulus clouds are low individual billowy globs that are low, have flat bases and look a little like cauliflower. They are at least as tall as they are wide and form on sunny days from pockets of rising air. Their constantly changing outlines are fun to watch because they can take the shapes of almost anything, including animals and faces. Cumulus clouds usually signal fair weather. If they build into the middle or high part of the atmosphere they get the name cumulonimbus. A cumulonimbus cloud is tall, deep and dark and can bring lightning, heavy rain and even severe weather such as hail, damaging winds or tornadoes. It is a sign of rapidly rising and sinking air currents.Stratus clouds are layered and cover most of the sky. They are much wider than they are tall. If you see them in broken or puffy layers, they are stratocumulus clouds. If you see them in thin high layers that turn the sky solid white, they're cirrostratus clouds. The tiny prisms of ice in a cirrostratus layer can bend the sun's light. As a result, often you can see a halo or veil of rainbow colors around the sun. When stratus clouds are very thick, they become dark nimbostratus clouds, which can produce rain, drizzle or snow.Cirrus clouds are high and thin and made entirely of ice crystals. Forming above 20,000 feet in the atmosphere, they often look like wisps of white hair. Cirrus clouds, which are a sign of warm moist air rising up over cold air, are sometimes an early signal that thickening clouds could bring light rain or snow within one or two days.Try to learn the names of the different clouds, and the next time you look up into the sky, take notice of what kind of clouds you see. And if you try, you might be able to guess what kind of weather they will bring
Explain why the land on the windward side of a mountain range is usually green and lush while the other side is usually drier.?
The land on the windward side of a mountain range is usually green and lush while the other side is usually drier because the clouds tend to pile up on the windward side. The clouds then drop their moisture before they cross the mountains, making the windward side wet and the other side dry.
What side of mountain has lush plant life?
windward windward windward
How does a mountain range in the path of prevailing winds affect precipitation on either side of the mountains?
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.
How does a mountain range in the path of prevailing winds affect precipitation in the either Side of 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.
True or False A rain shadow is the side of the mountain that has clouds or rain?
False. A rain shadow is the dry area on the leeward side of a mountain caused by the blocking of moisture-laden air by the mountain, leading to little or no precipitation. The side of the mountain with clouds and rain is the windward side.
How does a mountain range in the path of prevailing winds affect precipitation on either side of mountains?
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.
Which side of the mountain is considered windward?
It is the sloped side of a mountain that is colder and gets more rain. Why? Because the leeward side is the opposite of the windward side and is also dryer because when the clouds climb the mountain range (windward side) they loses all their water so there is none left for the leeward side.
On what side of a mountain do deserts often form?
Deserts often form on the leeward side of a mountain.
How did mountains add desertification?
Due to the change in atmospheric conditions a mountain can cause, the windward side of the mountain received the rain while the leeward side of the mountain does not receive the moisture creating a desert landscape. As the moisture rises to overtake the mountain the clouds condense creating rain on the windward side which creates an atmosphere of little to no moisture on the leeward side of the mountain.
What happens on the windward side of a mountain?
the windward side gets lot of rainfall
Why is the windward side of a mountain wetter and greener then the leeward side?
Winds blow clouds towards the windward side of mountains. The clouds are forced to rise and have to release their water as rain or snow. This makes the windward side of mountains wetter and greener.
Explain why the land on the windward side of a mountain range is usually green and lush while the other side is usually drier?
The land on the windward side of a mountain range is usually green and lush while the other side is usually drier because the clouds tend to pile up on the windward side. The clouds then drop their moisture before they cross the mountains, making the windward side wet and the other side dry.
