Lower latitudes have high moisture content in the air and the air rises. Lower latitudes near the equator has rising air making the areas have more precipitation.
high altitudes indicate cold temperatures so then that means that water vapor condenses at cooler temperatures and when water vapor condenses then it creates clouds
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because of pressure
Well altitude is the distance above sea level. The higher the altitude, the less air pressure and temperature there's going to be.
Leaving aside the temperature variable, ice melts more rapidly under higher air pressures. The higher the altitude, the lower the air pressure, and the more slowly ice is going to melt.
The Cloud forms from UPDRAFTS of 100 MPH and when it hits the Stratsophere it flattens out to form the top of the anvil.
A good arch is the cure. Also peeing from a higher altitude away from the wind.
every minute clouds are going higher and higher into the atmosphere , (which is extremely cold ). every minute clouds are going higher and higher into the atmosphere , (which is extremely cold ).
Yes.
Altitude affects the composition of clouds because the troposphere is very cold, hence the clouds up higher are made of ice crystals.
It depends on what cumulus type you are talking about. Cumulus humilis clouds are 'fatter' than they are tall. This is what people would usually refer to if they say just 'cumulus'. These are the clouds you see in the morning, and all also called fair weather clouds. You normally see a cumulus humilis cloud at an altitude of 2,000 to 3,500 feet. (600-1,050 m) Cumulus mediocris clouds are an alternate version of the humilis version. These clouds are taller than they are fat. You normally see a cumulus humilis cloud at an altitude of 2,000 to 4,000 feet. (600-1,200 m) Cumulus congestus clouds are the only cumulus clouds that produce substantial precipitation. When you hear someone saying '"cumulus clouds can produce precipitation"', they refer to these clouds. You normally see a cumulus congestus cloud at an altitude of 2,000 to 20,000 feet. (600-6,000 m). If you want to know what my reference is, it is a book called "Weather", by William J. Burroughs, Bob Crowder, Ted Robertson, Eleanor Vallier-Talbot, and Richard Whitaker.
Cirrus Clouds= Above 18,000 ft Status Clouds= Below 6,000 ft
Altitude affects the composition of clouds because the troposphere is very cold, so the clouds up higher are made of ice crystals. The clouds in the lower sections are made of water droplets or a mixture of water droplets and ice crystals.
Cirrus clouds are formed at a higher altitude then stratus clouds. Cirrus clouds are formed at about 8,000 m. Stratus clouds are formed under 2,000m. Fog is actually a stratus cloud that forms near the ground.
Low clouds are no higher than 2000 meters. Clouds which belong to this group include stratus clouds, nimbostratus clouds, and stratocumulus clouds. Varying amounts of precipitation are associated with these clouds.
Yes. Alto clouds form the medium altitude group, but stratus clouds are at low altitudes.
Expert answer is too funny!As for a serious answer - NO - most precipitate yielding clouds tend to be LOW or MID-level clouds (although they can spread into the higher atmosphere).Nimbostratus clouds form in the middle level of the troposphere and spread into both low and high altitude levels during precipitation. They tend to produce more of a steady, longer rain than Cumulonimbus clouds. If it is cold enough, they can produce snow. Nimbostratus clouds can develop from high clouds like cirrostratus and altostratus but they have to actually transition to nibostratus before they will produce rain or snow (or sleet). They tend to be a broad gray expanse thick enough you can't see the disk of the sun through them.Cumulonimbus clouds (aka thunder clouds) stretch even further than nimbostratus clouds from low to high altitudes, that is, the bottom of the cloud is at a relatively low altitude - perhaps around 450 m (~1500 feet) with the top stretching all the way up to 12,000 m (~65,000 feet). As their alternate name (thunder cloud) suggests, these are the type of clouds that produce thunderstorms. They can produce intense rain and sometimes hail. Although not all of them spawn tornadoes, this is the kind of cloud associated with tornadoes. These kind of clouds are VERY thick (refer to how far the stretch from low to high altitude) - thick enough to look "black" and definitely too thick to see the sun through.Clouds that are confined to the high atmosphere like Cirrus, Cirrostratus and Cirrocumulus are wispy and you can usually see the sun - or even moon - pretty well through them. There isn't enough to them to give any precipitation unless (as noted earlier) conditions cause them to transition to a different kind of cloud.Likewise, mid-level clouds like Altostratus and Altocumulus are not really thick enough to drop precipitation. While thicker than the Cirrus type clouds, you can still often see the sun as a bright disk through the clouds. Again - like the Cirrus clouds - if the right conditions are present, they can transition in to a different type of cloud that can then produce precipitation.
The highest clouds are polar mesospheric clouds, which, at heights from 76,000 to 85,000 m (altitude) are much higher than other types of clouds, such as cirrus and cumulonimbus. Cumulonimbus can exceptionally reach 23,000 m at the very top of a peaked formation, but these clouds normally form mainly within the 2,000 to 16,000 m range. Cirrus clouds, at a maximum height of about 18,000 m in tropical zones, are also much lower than polar mesosphericclouds.
The higher you get in the atmosphere, the more cold it is. For example, the earth's core is very very hot, and it gets colder the more away you are from it. Or something like that. :P.
Stratus or "blanket" clouds are usually low, featureless clouds that obscure all or part of the sun and sky. Higher altitude types are "altostratus" and "cirrostratus", which are formed from ice crystals.