Altocumulus Ac The altocumulus cloud has a base that begins between and m to 23, ft. These clouds are not to be confused with the altostratus type as these clouds appear bumpy. They may also be confused with stratocumulus clouds; however, these are larger. Because these clouds also have a high moisture content but tend not to precipitate, they often appear on very humid mornings where thunderstorms are expected by afternoon.
Latin Derivatives: altus - "high" and cumulus - "heap". Altostratus As The base of an altostratus cloud is found within the same levels as the altocumulus cloud.
These clouds are much larger in size as they may stretch for miles, similar to stratus clouds. They are comprised of ice crystals and water droplets. In thinner altostratus clouds, the sun may be dimly visible, commonly referred to as a "watery sun". If this cloud begins to precipitate, the base usually lowers, classifying it as a nimbostratus. Latin Derivatives: altus - "high" and stratus - "layer".
Cirrus Ci Cirrus clouds are composed mainly of ice crystals due to their height in the atmosphere m, 20, ft and above. The dryness of the air higher in the atmosphere contributes to their thin, wispy look. These clouds generally occur with fair weather and are the ones usually responsible for those beautiful midwestern sunsets.
Although they both vary in terms of precipitation, they are featherless clouds. While the stratus clouds produce light precipitation, the nimbostratus clouds can produce heavy downpours. Share with your loved ones, friends, and colleagues so that they can also learn about the stratus cloud. Download our app. July 23, 5 min read. What Are Stratus Clouds? How Do Stratus Clouds Form?
What Weather is Associated with Stratus Clouds? How Stratus Clouds Are Categorized Stratus clouds can be categorized into two types, which are: Stratus Fractus Stratus fractus clouds feature a broken stratus layer, which gives them an irregular shape or fragmented appearance. They can be found at times under heavy rain clouds like the nimbostratus or the cumulonimbus clouds.
Share on facebook. Share on twitter. Share on linkedin. Stratus clouds form in calm, stable conditions when gentle breezes raise cool, moist air over colder land or ocean surfaces. These clouds can exist in a variety of thicknesses and are sometimes opaque enough to darken days, allowing for little light to pass through.
Stratus clouds are uniform and flat, producing a gray layer of cloud cover which may be precipitation-free or may cause periods of light precipitation or drizzle. Thick, dense stratus or stratocumulus clouds producing steady rain or snow often are referred to as nimbostratus clouds. Stratus clouds are a type of low-level cloud, occurring below 6, feet.
They are characterized by uniform layers of grayish clouds. Stratus cloud layers are generally thin but cover the entire sky, known as overcast. The list of cloud types groups the main genera as high cirrus, cirro- , middle alto- , multi-level nimbostratus, cumulus, cumulonimbus , and low stratus, strato- according to the altitude level or levels at which each cloud is normally found. Fog and clouds are both made of tiny water droplets — like the ones you can sometimes see or feel in a hot, steamy shower.
Fog and mist are both created by water droplets, differing only in their overall locations and density. Mist forms wherever water droplets are suspended in the air by temperature inversion, volcanic activity, or changes in humidity. Characteristics of world weather and climate. Cloud Types. Clouds are the visible collections of water droplets or ice particles in the atmosphere. Meteorologists classify cloud types according to shape and altitude.
People often confuse climate and weather - the two really are quite different.
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