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This document discusses various cloud formation and precipitation processes including: adiabatic temperature change caused by air compression/expansion; orographic lifting where winds force air up mountains cooling it; frontal wedging where warm/cold air collide forming storms; convergence where air flows together upward; localized convective lifting forming warm air pockets called thermals; stability based on air density differences; condensation requiring saturated air; the types and heights of clouds; vertical cloud development enhancing movement; fog forming over land or sea; cold/warm cloud precipitation mechanisms; and rain, snow, sleet, glaze and hail depending on atmospheric temperatures.
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4 k jeinnings
This document discusses various cloud formation processes and types of precipitation. It covers topics such as:
1) Adiabatic temperature changes that cause air to expand and cool as it rises, leading to cloud formation.
2) Orographic lifting where air is forced to rise when passing over mountains, dropping rain on the windward sides.
3) Frontal wedging where warmer air overrides cooler air at weather fronts, causing the warmer air to rise.
4) Different types of clouds like cirrus, cumulus, and stratus clouds that form at high, middle and low altitudes and can produce precipitation like rain, snow or hail.
2Kcoldren
This document discusses different types of clouds and cloud formation processes. It describes adiabatic temperature changes, orographic lifting, frontal wedging, convergence, and localized convective lifting as mechanisms for cloud formation. It then defines high, middle, and low clouds and provides examples of cloud types in each category. Fog and vertically developing clouds are also briefly discussed.
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The document provides information over 3 days on cloud formation, types of clouds, and precipitation. It describes how clouds form through condensation on particle surfaces in saturated air. Mountain ranges cause orographic lifting which leads to more rain. Cirrus, altostratus and nimbostratus clouds are described. The Bergeron process explains how ice crystals in supercooled clouds cause water droplets to freeze and grow into precipitation. Rain forms through collision-coalescence in warm clouds above 0°C, while snow and hail form at colder temperatures.
3jbatcsics
This document discusses various types of clouds and precipitation. It explains processes like adiabatic temperature changes, orographic and frontal lifting that cause clouds to form. The document categorizes clouds by height as high, middle and low clouds. It also discusses different types of precipitation like rain, snow, sleet and hail. The key roles of condensation and freezing in the formation of clouds and precipitation are outlined.
2awindfelder
The document discusses various weather phenomena including adiabatic temperature changes, orographic and frontal lifting, convergence, localized convective lifting, stability, condensation, the four main types of clouds, high, middle and low clouds, clouds formed from the bottom up or top down, fog, cold and warm cloud precipitation including rain, snow, sleet, glaze and hail. It also includes citations for related images.
Cloud formation
This document summarizes different types of cloud formation processes and cloud types. It discusses adiabatic temperature changes that cause expansion and cooling, orographic lifting caused by air flowing over elevated terrain, frontal wedging that occurs at storm fronts, and localized convective lifting caused by uneven heating of the surface. It also describes the three main cloud height categories - high, middle, and low clouds - and specific cloud types like cirrus, cumulus, and stratus clouds. Clouds can form through stability or instability in the atmosphere and require water vapor to condense.
Clouds and cloud_formation
Science Fusion Gr.6 Unit.4 Lesson.2
Name Of Lesson:Clouds_ and _Cloud _Formation
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Clouds form through condensation which requires saturated air. Air cools adiabatically when it rises and expands. There are four main mechanisms that can lift air and cause it to rise: orographic lifting from air flowing over mountains, frontal wedging at boundaries between air masses, convergence when air flows together, and localized convective lifting. The stability of the air determines whether it will rise or remain in its original position, and influences the type of clouds and weather that form.
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4 k jeinnings
This document discusses various cloud formation processes and types of precipitation. It covers topics such as:
1) Adiabatic temperature changes that cause air to expand and cool as it rises, leading to cloud formation.
2) Orographic lifting where air is forced to rise when passing over mountains, dropping rain on the windward sides.
3) Frontal wedging where warmer air overrides cooler air at weather fronts, causing the warmer air to rise.
4) Different types of clouds like cirrus, cumulus, and stratus clouds that form at high, middle and low altitudes and can produce precipitation like rain, snow or hail.
2Kcoldren
This document discusses different types of clouds and cloud formation processes. It describes adiabatic temperature changes, orographic lifting, frontal wedging, convergence, and localized convective lifting as mechanisms for cloud formation. It then defines high, middle, and low clouds and provides examples of cloud types in each category. Fog and vertically developing clouds are also briefly discussed.
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The document provides information over 3 days on cloud formation, types of clouds, and precipitation. It describes how clouds form through condensation on particle surfaces in saturated air. Mountain ranges cause orographic lifting which leads to more rain. Cirrus, altostratus and nimbostratus clouds are described. The Bergeron process explains how ice crystals in supercooled clouds cause water droplets to freeze and grow into precipitation. Rain forms through collision-coalescence in warm clouds above 0°C, while snow and hail form at colder temperatures.
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This document discusses various types of clouds and precipitation. It explains processes like adiabatic temperature changes, orographic and frontal lifting that cause clouds to form. The document categorizes clouds by height as high, middle and low clouds. It also discusses different types of precipitation like rain, snow, sleet and hail. The key roles of condensation and freezing in the formation of clouds and precipitation are outlined.
2awindfelder
The document discusses various weather phenomena including adiabatic temperature changes, orographic and frontal lifting, convergence, localized convective lifting, stability, condensation, the four main types of clouds, high, middle and low clouds, clouds formed from the bottom up or top down, fog, cold and warm cloud precipitation including rain, snow, sleet, glaze and hail. It also includes citations for related images.
Cloud formation
This document summarizes different types of cloud formation processes and cloud types. It discusses adiabatic temperature changes that cause expansion and cooling, orographic lifting caused by air flowing over elevated terrain, frontal wedging that occurs at storm fronts, and localized convective lifting caused by uneven heating of the surface. It also describes the three main cloud height categories - high, middle, and low clouds - and specific cloud types like cirrus, cumulus, and stratus clouds. Clouds can form through stability or instability in the atmosphere and require water vapor to condense.
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Name Of Lesson:Clouds_ and _Cloud _Formation
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Clouds form through condensation which requires saturated air. Air cools adiabatically when it rises and expands. There are four main mechanisms that can lift air and cause it to rise: orographic lifting from air flowing over mountains, frontal wedging at boundaries between air masses, convergence when air flows together, and localized convective lifting. The stability of the air determines whether it will rise or remain in its original position, and influences the type of clouds and weather that form.
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This document discusses various cloud formation processes and types of precipitation. It explains that air cools as it rises and warms as it compresses. Clouds form through orographic lifting as air rises over mountains, and through frontal wedging when a cold front meets a warm front. Convergence of air masses also forces air to rise and form clouds. The stability of the atmosphere influences whether clouds produce thunderstorms. Various cloud types are classified by height as high, middle, or low clouds. The processes of collision-coalescence and Bergeron processes produce precipitation from warm and cold clouds respectively. Rain, snow, sleet, glaze and hail are different types of precipitation that form under varying temperature conditions.
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There are three main types of precipitation: orographic, convectional, and cyclonic. Orographic precipitation occurs when warm moist air rises over mountains, cooling and condensing into rain or snow. Convectional precipitation results from warm air near the ground surface rising rapidly into the atmosphere and cooling to form clouds. Cyclonic or frontal precipitation is caused by the collision of warm and cold air masses, where the warm air is forced to rise over the cold air along fronts, cooling and condensing to produce rain or snow.
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3) Frontal wedging where warmer air overrides cooler air at weather fronts, causing the warmer air to rise.
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The document describes the water cycle, which is the continuous movement of water on, above, and below the surface of the Earth. It explains that the sun heats water in the oceans causing evaporation into water vapor which forms clouds. As air rises, it cools and condenses into rain, snow, or other precipitation which falls back to Earth's surface and collects in lakes, rivers, and oceans - completing the cycle. The document also covers related topics like humidity, cloud types, precipitation types, thunderstorms, tornadoes, and hurricanes.
What factors affect different types of weather (the whole lesson)
The document describes the water cycle, which is the continuous movement of water on, above, and below the surface of the Earth. It involves evaporation, condensation, precipitation, and collection of water. Water evaporates from bodies of water and condenses into clouds. It then falls back to Earth's surface as precipitation such as rain, snow, or hail. This precipitation collects in bodies of water, completing the cycle.
Atmospheric moisture
Water vapor is the most important gas in the atmosphere and is the source of all condensation and precipitation. The water cycle begins with evaporation and includes condensation, precipitation, and water running off or sinking into the ground. Clouds are classified based on their height and form, with cirrus, cumulus and stratus being the main cloud types located in the high, middle and low levels of the atmosphere respectively. For precipitation to form, cloud droplets must grow substantially through processes like collision-coalescence in warm clouds and the Bergeron process in cold clouds. The type of precipitation reaching the surface depends on the temperature profile in the lower atmosphere.
RSaugling period 4
This document discusses various cloud formation processes including orographic lifting, frontal wedging, convergence, localized convective lifting, stability, condensation, and adiabatic cooling. It describes how different cloud types like cirrus, stratus, and cumulus form at different heights. It also covers fog, precipitation processes for warm and cold clouds, and the differences between rain, snow, sleet, glaze and hail. Key cloud formation mechanisms involve air masses interacting as they rise over terrain or collide, resulting in adiabatic cooling and condensation.
4rsaugling
This document discusses various cloud formation processes including orographic lifting, frontal wedging, convergence, localized convective lifting, stability, condensation, and adiabatic cooling. It describes how different cloud types like cirrus, stratus, and cumulus form at different heights. It also covers fog, precipitation processes for warm and cold clouds, and the differences between rain, snow, sleet, glaze and hail. Key cloud formation mechanisms involve air masses interacting as they rise over terrain or collide, resulting in adiabatic cooling and condensation.
WATER IN ATMOSPHERE
1) Water exists in the atmosphere in solid, liquid, and gaseous forms. Water vapor accounts for around 4% of the atmosphere and plays an important role in determining weather through condensation and precipitation.
2) The amount of water vapor present in air is known as humidity, which is measured in terms of absolute or relative humidity. Evaporation from oceans and other water bodies adds water vapor to the atmosphere.
3) When air reaches its dew point temperature, water vapor condenses to form precipitation like rain, snow, sleet or hail which then falls to the Earth's surface through processes like convectional, orographic or frontal rainfall. The distribution of rainfall varies globally depending on factors like
Clouds and precipitation by Ian Slavin
This document discusses various cloud formation processes and types of precipitation. It describes how air cools and warms during adiabatic changes and how lifting mechanisms like orographic lifting and frontal wedging cause clouds to form. It also explains different cloud types based on height like high, middle and low clouds. Finally, it discusses precipitation types including rain, snow, sleet, hail and freezing rain.
4aklee
This document discusses various cloud formation processes and types of precipitation. It explains how temperature changes during air expansion and compression can cause clouds to form through processes like orographic lifting and frontal wedging. Different cloud types like cirrus, cumulus and stratus clouds that form at high, middle and low altitudes are described. The document also outlines precipitation processes for warm and cold clouds, and defines types of precipitation including rain, snow, sleet, hail and glaze.
1agoodwin
This document discusses various cloud formation processes and types of precipitation. It explains that adiabatic cooling due to air expansion causes clouds to form during orographic lifting and frontal wedging. Convergence and localized convective lifting can also cause clouds when warm air rises. The document categorizes clouds by height as high, middle, and low clouds. It describes different precipitation types including rain, snow, sleet, glaze and hail.
Clouds and percipitation
This document discusses various mechanisms that cause air to rise and form clouds, including orographic lifting from air flowing over mountains, frontal wedging along weather fronts, convergence of air masses, and localized convective lifting from uneven heating of air. It also describes different types of clouds like cirrus, cumulus, and stratus clouds. High clouds form at high altitudes and have thin wispy forms. Middle and low clouds have thicker forms and occur at lower altitudes. The document outlines processes like condensation and precipitation that lead to rain, snow, sleet, hail and other forms of weather.
clouds formation.pptx
1. Clouds form when air rises and cools to its dew point, causing water vapor to condense. There are several lifting processes that cause cloud formation, including turbulence, convection, orographic uplift, and frontal uplift.
2. Clouds are classified based on height, shape, color, and how they transmit or reflect light. The main cloud forms are cirrus, stratus, and cumulus clouds.
3. Fog forms when air cools to its dew point near the surface of the earth. Common types of fog include radiation fog, advection fog, upslope fog, and frontal fog.
Weather slides
This document discusses key concepts about weather including the four elements of weather, common weather tools, wind, temperature, air pressure, humidity, the water cycle, types of precipitation and clouds. It provides definitions and descriptions of terms like evaporation, condensation, collection and fronts. Violent storms like thunderstorms and tornadoes are also summarized. Weather forecasting is described as involving observations from humans and machines along with past experience to predict future conditions.
Similar to period 4 M Gahmn 5mjoseph (20)
What factors affect different types of weather (the whole lesson)
What factors affect different types of weather (the whole lesson)
What factors affect different types of weather (the whole lesson)
What factors affect different types of weather (the whole lesson)
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This document discusses various atmospheric phenomena including adiabatic temperature changes, orographic lifting, frontal wedging, localized convection, stability, condensation, cloud types, fog formation, precipitation processes like the Bergeron process and warm clouds, and types of precipitation like rain, snow, sleet, glaze and hail. It provides definitions and brief explanations of these terms along with accompanying diagrams and images.
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The document discusses various topics related to weather including:
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This document discusses various cloud formation processes and types of precipitation. It covers topics such as adiabatic temperature changes, orographic lifting, frontal wedging, convergence, convective lifting, stability, condensation, types of clouds including high, middle and low clouds, fog, cold and warm cloud precipitation processes, and forms of precipitation including sleet, glaze and hail. The document provides explanations of key cloud and precipitation concepts and formation mechanisms.
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When air rises and expands, it cools through adiabatic processes. This cooling can cause water vapor in the air to condense into clouds and precipitate out as rain, snow, sleet or hail depending on temperature levels. Clouds are classified based on their height and physical structure into cirrus, altostratus and nimbostratus clouds that form at high, middle and low altitudes respectively.
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This document summarizes different types of cloud formation and precipitation processes. It discusses how adiabatic temperature changes and expansion cause clouds to form. Mountain ranges and frontal systems can also trigger cloud formation through orographic lifting and frontal wedging. The document outlines different cloud types from high to low altitudes and clouds associated with vertical air movement. It then explains various precipitation processes for warm and cold clouds and the differences between rain, snow, sleet, glaze and hail.
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This document summarizes different mechanisms for cloud and precipitation formation. It discusses how adiabatic temperature changes cause air to cool and condense as it rises upward or expands. It also describes how orographic lifting can cause the windward sides of mountains to receive more rain, while rain shadows form on the leeward sides. Finally, it mentions how frontal wedging occurs when warm and cold air masses collide at a front.
Clouds and precipitation-nate mann
This document summarizes different mechanisms for cloud and precipitation formation. It discusses how adiabatic temperature changes cause air to cool and condense as it rises upward or expands. It also describes how orographic lifting can cause the windward sides of mountains to receive more rain, while rain shadows form on the leeward sides. Finally, it mentions how frontal wedging occurs when warm and cold air masses collide at a front.
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This document summarizes several key atmospheric processes:
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Moisture,clouds,and precipitation
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period 4 M Gahmn 5mjoseph
- 2. Adiabatic Temperature Change • Adiabatic temperature change is when the temperature changes without heat being added or subtracted • This happens by air being compressed or the air being expanded
- 3. Orographic Lifting • Is when mountains or high ground act as wind barriers • As the air/ wind goes up the side of the mountain it cools it off creating precipitation and clouds • by time the wind gets to the other side the moister is mostly gone on its decline it puts off warm air
- 4. Frontal wedging • Is when cold and warm air collide with each other becoming a front • This creates the warm air to flow right over the cold air • These fronts can create a middle cyclone storms
- 5. Convergence • Is when air in the lower atmosphere flow together • It happens when air flows from more than one direction an the only place the air can go is up
- 6. Localized Convective Lifting • Is when unequal heating occurs on the earths surface creating warm air pockets • The warm pockets of air will rise above the other because it is less dense when that happens it is called a thermal • Thermals are great for hawks to hunt pray and even good for hang gliding
- 7. Stability Density Differences • Stable air stays the same while the unstable air tends to rise • Clouds wont form in stable air conditions
- 8. condensation • Air must be saturated to form • Saturation happens when air is cooled to its dew point
- 9. Types of Clouds • Cirrus clouds are described as a curl of hair and are high and thin in the atmosphere • Cumulus clouds are rounded individual masses • Stratus is a layer or sheet
- 10. High clouds • Cirrus, cirrostratus and cirrocumulus make up the high cloud family • Often made up of ice crystals making thin and white clouds • High clouds do not create precipitation
- 11. Middle clouds • Altocumulus clouds are composed of rounded masses that are larger and denser then cirrocumulus clouds • Middles clouds range from 2000-6000 meters in the atmosphere • Infrequent light snow or drizzle may occur in this area
- 12. Low clouds • Stratus, stratocumulus, and nimbostratus make up the low cloud family • Light precipitations are created by nimbostratus clouds • Stratus that develops a scalloped bottom are called stratocumulus clouds
- 13. Clouds of vertical development • The more movement and acceleration creates a more vertical range
- 14. Fog • Fog is a cloud with a base at or near the ground • Fog can be produced by moisture from the sea that moves over land • Moisture evaporates as cool air moves over warm air
- 15. Cold cloud precipitation • The Bergeron process relies on super cooling and saturation • Ice crystals cannot exist with water droplets
- 16. Warm cloud precipitation • Collision-coalescence process forms raindrops in clouds • Water absorbing particles remove water vapor from the air • As droplets move through the clouds that join with smaller droplets
- 17. Rain and Snow • The type of precipitation depends on the temperature in the atmosphere • When temperatures are above 4˚C snowflakes melt and continue as rain • A temperature more then -5˚C ice crystals come together in clumps
- 18. Sleet, Glaze, and Hail • Sleet is small particles of clear ice • Glaze (freezing rain) occurs when raindrops are super cooled as they fall • Hailstones begin as small ice droplets that get bigger as they collect super cooled droplets
- 19. The end