Fathima ppt1
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Clouds are formed by the condensation of water vapor around dust particles in the atmosphere. Clouds can be classified based on their form and altitude. There are four main types of clouds based on form - cirrus, stratus, cumulus, and nimbus clouds. Clouds are also classified based on their altitude as high, medium, and low clouds, as well as clouds with great vertical extent.
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Stratus clouds form thick sheets that cover the sky. Stratocumulus clouds are layered clouds. Cirrus clouds are high, thin, and white and can occur in patches.
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This document discusses different types of clouds based on their properties and formation. It describes 10 main cloud types including cirrus, stratus, cumulus and nimbostratus clouds. These cloud types are grouped into high, middle and low clouds based on their average altitude. High clouds like cirrus are made of ice crystals while middle and low clouds contain mostly water droplets. Clouds form through the heating and rising of air masses which leads to the condensation of water vapor. Different cloud formations signal upcoming weather changes or precipitation.
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This document discusses water vapor and its role in atmospheric processes. It describes the three states of matter and how humidity is measured. It explains how clouds form at the dew point and how they are classified by height and type. The document also discusses different forms of precipitation and how they develop within clouds.
Clouds by krista and haley
This document describes three types of clouds: stratus clouds which are flat, hazy and white and found at low altitudes; cumulus clouds which sometimes resemble cotton balls; and cumulonimbus clouds which can form alone or in clusters and are capable of producing lightning, thunder and heavy rain.
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Cirrostratus clouds are very high clouds that can indicate either fair weather or an approaching storm. Altostratus clouds form at middle levels and can let sunlight pass through if not too thick. Fog forms at low levels when air cools to its dew point near the ground.
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Cirrostratus clouds are very high clouds that can indicate either fair weather or an approaching storm. Altostratus clouds form at middle levels and can let sunlight pass through if not too thick. Fog forms at low levels when air reaches its dew point near the ground.
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Stratus clouds form thick sheets that cover the sky. Stratocumulus clouds are layered clouds. Cirrus clouds are high, thin, and white and can occur in patches.
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This document discusses different types of clouds based on their properties and formation. It describes 10 main cloud types including cirrus, stratus, cumulus and nimbostratus clouds. These cloud types are grouped into high, middle and low clouds based on their average altitude. High clouds like cirrus are made of ice crystals while middle and low clouds contain mostly water droplets. Clouds form through the heating and rising of air masses which leads to the condensation of water vapor. Different cloud formations signal upcoming weather changes or precipitation.
Clouds
Clouds form when air rises and cools, causing water vapor to condense on dust particles. There are three main cloud levels: high-level clouds above 6,000 meters made of ice crystals; mid-level clouds between 2,000-6,000 meters made of water droplets; and low-level clouds below 2,000 meters also made of water droplets. Clouds impact the environment by cooling the atmosphere, redistributing heat from the equator to poles, and providing precipitation through the hydrologic cycle.
Ppp on clouds and their classification
1) The document discusses different types of clouds based on their composition, height, and shape. Clouds are classified into high, middle, and low clouds depending on their altitude in the atmosphere.
2) High clouds like cirrus and cirrostratus contain ice crystals and form above 6km. Middle clouds such as altostratus and altocumulus contain water droplets and ice crystals. Low clouds like stratus and cumulus contain mostly water droplets.
3) Common cloud types are described including cirrus, cirrostratus, cirrocumulus, altostratus, altocumulus, stratus, cumulus, nimbostratus, and cumulonimbus. Each
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Clouds are large collections of tiny water droplets or ice crystals that are light enough to float in the air. Clouds form when warm air rises and cools, causing water vapor to condense onto particles. Clouds appear white because they reflect all colors of light equally. Thicker clouds or those with other clouds blocking light above look gray. Clouds move with wind currents and are categorized by height, composition, and appearance into high, mid, low, and vertically developed clouds as well as miscellaneous types like contrails and mammatus clouds.
Clouds
Clouds form when water evaporates into the sky and rises as vapor. There are three levels of clouds - low, mid, and high level clouds. Low level clouds include cumulus clouds, which are puffy and cotton-like, and fog clouds. Mid-level clouds consist of alto cumulus and alto stratus clouds. High level cirrus clouds are thin and wispy ice crystal clouds.
Clouds
There are three main types of clouds: cirrus, cumulus, and stratus. Cirrus clouds form above 20,000 feet and are made of ice crystals. Cumulus clouds form from warm air rising and are puffy cotton-ball shaped clouds, including heavy thunderstorm clouds. Stratus clouds are low, horizontal layers that blanket the sky forming at boundaries where warm air passes over cool air.
Clouds and It's Classification
Clouds can be classified according to their shape or altitude. According to shape, clouds include cirrus which are thin and feathery, cumulus which are thick and puffy like cauliflower, stratus which are dark gray with ragged edges, and nimbus which occur in layers. According to altitude, high clouds form above 6,000 meters, middle clouds are between 2,000-6,000 meters, low clouds are below 2,000 meters, and vertical clouds can extend across all altitudes. Fog is also mentioned as a low-lying cloud.
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This document summarizes different types of clouds and how precipitation forms. It describes the three basic cloud forms - cirrus, cumulus, and stratus - and provides examples of high, middle, and low clouds. It explains that low clouds like stratus and nimbostratus are more likely to produce precipitation as they form closer to the ground. The document also discusses how cloud droplets must grow substantially before falling as precipitation and outlines the Bergeron process relating supercooled clouds and freezing nuclei to cold cloud precipitation formation.
Types of clouds
Cirrus clouds form at high altitudes and indicate deteriorating weather conditions. They appear wispy and white or light gray. Cumulus clouds form at low altitudes and have puffy, cotton-like appearances. They can grow into storm clouds. Nimbus clouds produce precipitation that reaches the ground as rain, hail, snow or sleet. Stratus clouds are low-level, uniform clouds that may produce light drizzle or snow.
The clouds
Clouds can be classified based on their height and appearance. The main cloud types are cirrus (high, wispy), stratus (low, sheet-like), cumulus (low, puffy), and nimbus (rain-bearing). Cirrocumulus and altocumulus appear at middle altitudes in globular masses or rolls. Altostratus and stratocumulus form gray layers or patches. Cumulonimbus clouds produce thunderstorms with ice crystal tops and mushroom shapes. Clouds are differentiated based on their altitude, color, shape, and whether they produce precipitation.
Cloud types
Cirrus clouds are very wispy and high up around 20,000 feet. They are usually white and not associated with rain. Cumulus clouds are the puffy clouds seen around 3,000 feet up on sunny days. Cumulonimbus clouds produce thunderstorms, lightning, tornadoes and bad weather around 1,000 feet up. They can flatten at the top into an anvil shape. Stratus clouds cover the whole sky in a fog-like formation up to 6,000 feet and sometimes produce light drizzle or sprinkles while appearing grey.
Cloud types 1
Cirrus clouds are very high wispy clouds that do not produce rain. Cumulus clouds are puffy clouds sometimes seen on sunny days that can reach heights of 3,000 feet. Cumulonimbus clouds produce thunderstorms with lightning, tornadoes, and thunder and have an anvil shape at the top. Stratus clouds are low, uniform gray clouds that cover the entire sky and can produce light drizzle.
Cloud Types
This document describes different types of clouds:
- Cirrus clouds occur above 20,000 feet and point in the direction of air movement. They are thin and wispy.
- Cumulus clouds are fluffy cotton-like clouds that can be as low as 1,000 feet. They appear fluffy due to rising thermals of air in the cloud.
- Cumulonimbus clouds exist from near the ground to 50,000 feet. They are associated with powerful thunderstorms that can produce snow, rain, hail, lightning and sometimes tornadoes.
Cloud types
This document describes different types of clouds:
- Cirrus clouds occur above 20,000 feet and point in the direction of air movement. They are thin and wispy.
- Cumulus clouds are fluffy cotton-like clouds that can be as low as 1,000 feet. They appear fluffy due to rising thermals of air within the cloud.
- Cumulonimbus clouds exist from near the ground to 50,000 feet. They are associated with powerful thunderstorms that can produce snow, rain, hail, lightning and sometimes tornadoes.
- Stratus clouds form uniform layers below 6,000 feet. Fog results from very low stratus clouds. They are formed when weak
kinds of Cumulus clouds
Cumulus clouds are puffy, cotton-like clouds with flat bases around 1000m above the ground and rounded tower tops. When the tops resemble cauliflower heads, they are called cumulus congestus or towering cumulus clouds. These clouds can grow vertically into giant cumulonimbus clouds, which are thunderstorm clouds. Cumulonimbus clouds form when cumulus congestus clouds continue growing upwards, with bases around 300m and tops over 12,000m high. They release tremendous energy through water vapor condensation and are associated with lightning, thunder, and tornadoes.
About clouds
There are 5 main types of clouds categorized by their height above sea level: low clouds like stratus and cumulus below 6,500 feet, middle clouds such as altostratus from 6,500 to 20,000 feet, and high clouds like cirrus above 20,000 feet. Cumulonimbus clouds are towering clouds that can reach heights over 60,000 feet and produce thunderstorms that bring hail and lightning. Cirrus clouds form above 30,000 feet and are composed primarily of ice crystals.
Clouds
Clouds form when warm air rises and cools, reaching the dew point where water vapor condenses into liquid water or ice droplets. There are three main cloud types - cirrus, stratus, and cumulus - which are classified based on their altitude and appearance. Clouds can combine elements of these types and bring weather like rain or storms. Common cloud types include cumulonimbus thunderheads and nimbostratus rain clouds.
Geometry in clouds
Clouds come in different types based on their altitude and consistency, including stratus, cirrus, and cumulus clouds. Stratus clouds form a thick, even blanket across the sky. Cirrus clouds are thin and wispy, found at high altitudes, taking straight or curvy shapes based on wind. Cumulus clouds have a puffy, built-up appearance and can form tear drop shapes when water droplets within them combine and fall.
Cloud presentation
This document describes the different types of clouds, including cirrus clouds which are high and thin like curly hair, cumulus clouds which consist of rounded masses like cauliflower, and stratus clouds which form sheets or layers across the sky. It also discusses cirrostratus, cumulonimbus, nimbostratus, stratocumulus, and altocumulus clouds and their distinguishing characteristics.
Powerpoint_ bongcawel
Clouds are visible masses of water droplets or ice crystals suspended in the atmosphere above the Earth's surface. Clouds are classified into high, middle, low, and vertical clouds based on their altitude and physical properties. High clouds form between 10,000 to 60,000 feet, middle clouds form between 6,500 to 25,000 feet, low clouds form below 6,500 feet, and vertical clouds can develop at many heights with strong updrafts.
Ch 18 ppt 2012
Water vapor is the most important gas in the atmosphere. Clouds form when air is cooled to its dew point. There are three main types of clouds - cirrus, cumulus, and stratus - which are classified based on their height in the atmosphere. Precipitation forms as cloud droplets grow in size, with the type of precipitation depending on temperature profiles. Common forms of precipitation include rain, snow, sleet, glaze, and hail.
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Clouds
Clouds form when air rises and cools, causing water vapor to condense on dust particles. There are three main cloud levels: high-level clouds above 6,000 meters made of ice crystals; mid-level clouds between 2,000-6,000 meters made of water droplets; and low-level clouds below 2,000 meters also made of water droplets. Clouds impact the environment by cooling the atmosphere, redistributing heat from the equator to poles, and providing precipitation through the hydrologic cycle.
Ppp on clouds and their classification
1) The document discusses different types of clouds based on their composition, height, and shape. Clouds are classified into high, middle, and low clouds depending on their altitude in the atmosphere.
2) High clouds like cirrus and cirrostratus contain ice crystals and form above 6km. Middle clouds such as altostratus and altocumulus contain water droplets and ice crystals. Low clouds like stratus and cumulus contain mostly water droplets.
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Clouds are large collections of tiny water droplets or ice crystals that are light enough to float in the air. Clouds form when warm air rises and cools, causing water vapor to condense onto particles. Clouds appear white because they reflect all colors of light equally. Thicker clouds or those with other clouds blocking light above look gray. Clouds move with wind currents and are categorized by height, composition, and appearance into high, mid, low, and vertically developed clouds as well as miscellaneous types like contrails and mammatus clouds.
Clouds
Clouds form when water evaporates into the sky and rises as vapor. There are three levels of clouds - low, mid, and high level clouds. Low level clouds include cumulus clouds, which are puffy and cotton-like, and fog clouds. Mid-level clouds consist of alto cumulus and alto stratus clouds. High level cirrus clouds are thin and wispy ice crystal clouds.
Clouds
There are three main types of clouds: cirrus, cumulus, and stratus. Cirrus clouds form above 20,000 feet and are made of ice crystals. Cumulus clouds form from warm air rising and are puffy cotton-ball shaped clouds, including heavy thunderstorm clouds. Stratus clouds are low, horizontal layers that blanket the sky forming at boundaries where warm air passes over cool air.
Clouds and It's Classification
Clouds can be classified according to their shape or altitude. According to shape, clouds include cirrus which are thin and feathery, cumulus which are thick and puffy like cauliflower, stratus which are dark gray with ragged edges, and nimbus which occur in layers. According to altitude, high clouds form above 6,000 meters, middle clouds are between 2,000-6,000 meters, low clouds are below 2,000 meters, and vertical clouds can extend across all altitudes. Fog is also mentioned as a low-lying cloud.
18.3[1]
This document summarizes different types of clouds and how precipitation forms. It describes the three basic cloud forms - cirrus, cumulus, and stratus - and provides examples of high, middle, and low clouds. It explains that low clouds like stratus and nimbostratus are more likely to produce precipitation as they form closer to the ground. The document also discusses how cloud droplets must grow substantially before falling as precipitation and outlines the Bergeron process relating supercooled clouds and freezing nuclei to cold cloud precipitation formation.
Types of clouds
Cirrus clouds form at high altitudes and indicate deteriorating weather conditions. They appear wispy and white or light gray. Cumulus clouds form at low altitudes and have puffy, cotton-like appearances. They can grow into storm clouds. Nimbus clouds produce precipitation that reaches the ground as rain, hail, snow or sleet. Stratus clouds are low-level, uniform clouds that may produce light drizzle or snow.
The clouds
Clouds can be classified based on their height and appearance. The main cloud types are cirrus (high, wispy), stratus (low, sheet-like), cumulus (low, puffy), and nimbus (rain-bearing). Cirrocumulus and altocumulus appear at middle altitudes in globular masses or rolls. Altostratus and stratocumulus form gray layers or patches. Cumulonimbus clouds produce thunderstorms with ice crystal tops and mushroom shapes. Clouds are differentiated based on their altitude, color, shape, and whether they produce precipitation.
Cloud types
Cirrus clouds are very wispy and high up around 20,000 feet. They are usually white and not associated with rain. Cumulus clouds are the puffy clouds seen around 3,000 feet up on sunny days. Cumulonimbus clouds produce thunderstorms, lightning, tornadoes and bad weather around 1,000 feet up. They can flatten at the top into an anvil shape. Stratus clouds cover the whole sky in a fog-like formation up to 6,000 feet and sometimes produce light drizzle or sprinkles while appearing grey.
Cloud types 1
Cirrus clouds are very high wispy clouds that do not produce rain. Cumulus clouds are puffy clouds sometimes seen on sunny days that can reach heights of 3,000 feet. Cumulonimbus clouds produce thunderstorms with lightning, tornadoes, and thunder and have an anvil shape at the top. Stratus clouds are low, uniform gray clouds that cover the entire sky and can produce light drizzle.
Cloud Types
This document describes different types of clouds:
- Cirrus clouds occur above 20,000 feet and point in the direction of air movement. They are thin and wispy.
- Cumulus clouds are fluffy cotton-like clouds that can be as low as 1,000 feet. They appear fluffy due to rising thermals of air in the cloud.
- Cumulonimbus clouds exist from near the ground to 50,000 feet. They are associated with powerful thunderstorms that can produce snow, rain, hail, lightning and sometimes tornadoes.
Cloud types
This document describes different types of clouds:
- Cirrus clouds occur above 20,000 feet and point in the direction of air movement. They are thin and wispy.
- Cumulus clouds are fluffy cotton-like clouds that can be as low as 1,000 feet. They appear fluffy due to rising thermals of air within the cloud.
- Cumulonimbus clouds exist from near the ground to 50,000 feet. They are associated with powerful thunderstorms that can produce snow, rain, hail, lightning and sometimes tornadoes.
- Stratus clouds form uniform layers below 6,000 feet. Fog results from very low stratus clouds. They are formed when weak
kinds of Cumulus clouds
Cumulus clouds are puffy, cotton-like clouds with flat bases around 1000m above the ground and rounded tower tops. When the tops resemble cauliflower heads, they are called cumulus congestus or towering cumulus clouds. These clouds can grow vertically into giant cumulonimbus clouds, which are thunderstorm clouds. Cumulonimbus clouds form when cumulus congestus clouds continue growing upwards, with bases around 300m and tops over 12,000m high. They release tremendous energy through water vapor condensation and are associated with lightning, thunder, and tornadoes.
About clouds
There are 5 main types of clouds categorized by their height above sea level: low clouds like stratus and cumulus below 6,500 feet, middle clouds such as altostratus from 6,500 to 20,000 feet, and high clouds like cirrus above 20,000 feet. Cumulonimbus clouds are towering clouds that can reach heights over 60,000 feet and produce thunderstorms that bring hail and lightning. Cirrus clouds form above 30,000 feet and are composed primarily of ice crystals.
Clouds
Clouds form when warm air rises and cools, reaching the dew point where water vapor condenses into liquid water or ice droplets. There are three main cloud types - cirrus, stratus, and cumulus - which are classified based on their altitude and appearance. Clouds can combine elements of these types and bring weather like rain or storms. Common cloud types include cumulonimbus thunderheads and nimbostratus rain clouds.
Geometry in clouds
Clouds come in different types based on their altitude and consistency, including stratus, cirrus, and cumulus clouds. Stratus clouds form a thick, even blanket across the sky. Cirrus clouds are thin and wispy, found at high altitudes, taking straight or curvy shapes based on wind. Cumulus clouds have a puffy, built-up appearance and can form tear drop shapes when water droplets within them combine and fall.
Cloud presentation
This document describes the different types of clouds, including cirrus clouds which are high and thin like curly hair, cumulus clouds which consist of rounded masses like cauliflower, and stratus clouds which form sheets or layers across the sky. It also discusses cirrostratus, cumulonimbus, nimbostratus, stratocumulus, and altocumulus clouds and their distinguishing characteristics.
Powerpoint_ bongcawel
Clouds are visible masses of water droplets or ice crystals suspended in the atmosphere above the Earth's surface. Clouds are classified into high, middle, low, and vertical clouds based on their altitude and physical properties. High clouds form between 10,000 to 60,000 feet, middle clouds form between 6,500 to 25,000 feet, low clouds form below 6,500 feet, and vertical clouds can develop at many heights with strong updrafts.
Ch 18 ppt 2012
Water vapor is the most important gas in the atmosphere. Clouds form when air is cooled to its dew point. There are three main types of clouds - cirrus, cumulus, and stratus - which are classified based on their height in the atmosphere. Precipitation forms as cloud droplets grow in size, with the type of precipitation depending on temperature profiles. Common forms of precipitation include rain, snow, sleet, glaze, and hail.
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Fathima ppt1
- 1. welcome
- 3. CLOUDS One of the forms of condensation. Formed by the condensation of water vapour around the dust particles in the atmosphere.
- 4. TYPES OF CLOUDS Clouds can be classified according to their form and height. Based on form there are mainly 4types of clouds 1. Cirrus clouds. 2. Stratus clouds. 3. Cumulus clouds. 4. Nimbus clouds.
- 5. TYPES OF CLOUDS Based on altitude. 1. High clouds (20000 to 40000 ft.) 2. Medium clouds (7000 to 20000 ft.) 3. Low clouds (<7000ft.) 4. Clouds with great vertical extent (2000 to 30000ft).
- 6. CIRRUS CLOUDS These are feather – like clouds in the upper atmosphere in clear weather conditions. STRATUS CLOUDS These appear in the layers in the lower part of the sky.
- 7. CUMULUS CLOUDS These clouds resemble huge cotton bundles and are formed due to strong convection currents. They have large vertical currents.
- 8. NIMBUS CLOUDS Dark rain clouds in the lower atmosphere. These clouds appear dark. It does not allow sunlight to pass through due to thick concentration of water droplets.
- 10. Thank you