Cirrus clouds are thin and wispy, moving from west to east and usually indicating fair weather. Stratus clouds are gray clouds that may cover the sky and resemble fog, sometimes drizzling without reaching the ground. Cumulus clouds are puffy and cotton-like, growing upward and potentially developing into thunderstorms. The document provides descriptions of different cloud types and a game to test cloud identification.
The document discusses the formation of clouds and different types of clouds. It explains that clouds form when warm air rises and cools, causing water vapor to condense into water droplets or ice crystals. There are several main types of clouds including stratus clouds which form a blanket-like layer, cumulus clouds which have a puffy, cotton-ball appearance, and cirrus clouds which are high-altitude clouds with a feathery shape made of ice crystals. The document also defines fog, precipitation, and transpiration and provides some online resources about clouds.
This document discusses clouds and precipitation. It defines evaporation and condensation, and explains how clouds form when air rises and cools to the dew point, allowing water vapor to condense on condensation nuclei. The main cloud types - cirrus, stratus, and cumulus - are identified based on their location in the sky and the weather they predict. The four major types of precipitation - rain, snow, sleet, and hail - are described based on their characteristics and formation processes.
Cumulus clouds are low-level, puffy clouds. Stratus clouds are also low-level clouds that form thick gray layers covering the entire sky and can result from thick fog lifting. Cumulonimbus clouds are middle-level clouds that bring intense weather like lightning, thunder, tornadoes. Cirrus clouds are high-level, thin clouds blown by winds that typically mean fair weather. Fog forms near the ground. High-level clouds above 20,000 feet contain ice crystals due to cold temperatures. Middle-level clouds between 6,500 to 20,000 feet contain water droplets and sometimes ice. Low-level clouds below 6,500 feet contain water droplets and can contain ice or snow in cold conditions.
This document discusses various cloud formation processes including adiabatic temperature changes, orographic lifting, frontal wedging, convergence, localized convective lifting, stability, condensation, and precipitation processes like the Bergeron process and collision-coalescence process. It also covers cloud types like cumulus, cirrus, and stratus clouds as well as fog, rain, snow, sleet, glaze and hail.
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.
There are three main types of clouds: stratus clouds which form a blanket, cumulus clouds which are billowy and puffy, and cirrus clouds which are wispy and feather-like. Clouds can be named by their altitude using prefixes like cirro- for high altitudes and alto- for middle altitudes, or suffixes like -nimbus which indicate storms. Different types of precipitation fall depending on temperature, with rain falling in warm air, sleet forming when rain freezes before hitting the ground, snow falling in cold air, and hail stones growing in size as they are pushed high in the atmosphere and freeze in layers.
Clouds form when water vapor condenses into liquid water droplets or solid ice crystals. There are three main ways that air can be cooled enough for condensation to occur: contact cooling over land or sea surfaces, convection as air rises, and orographic lifting as air rises over mountains. Clouds can be classified based on their shape and height, with low-level clouds like stratus closest to the surface and high-level clouds like cirrus located over 6,000 meters. The major cloud belts around the world are associated with prevailing wind patterns.
There are three main types of clouds: stratus clouds which form a blanket, cumulus clouds which are billowy and puffy, and cirrus clouds which are wispy and feather-like. Clouds can be named by their altitude using prefixes like cirro- for high altitudes and alto- for middle altitudes, or suffixes like -nimbus which indicate storms. The four main types of precipitation are rain, sleet, snow, and hail, which form depending on temperatures and whether water vapor condenses or freezes before reaching the ground. Rainfall amounts are measured using rain gauges, which is important information for farmers.
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.
There are three main types of clouds: cirrus clouds, which are thin and wispy ice crystal clouds found very high in the sky; cumulus clouds, which are puffy cotton-like clouds that can signal either fair weather or rain depending on whether they are white or dark; and stratus clouds, which are the lowest, flat clouds that are often dark and can signal rain or fog if close to the ground.
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.
The document discusses cloud formation. Sun heats surfaces and warms the air, causing water to evaporate into water vapor. The vapor rises with the warm air. As the air cools higher in the atmosphere, the vapor condenses into water droplets, forming clouds. There are three main types of clouds: cumulus, stratus, and cirrus, which differ based on their location and appearance.
Clouds are formed when warm air rises and cools, causing water vapor to condense onto particles in the air. There are four main types of clouds: cumulus, nimbus, cirrus, and stratus. Rain forms when water droplets in clouds grow too heavy and fall to the ground. There are three types of rainfall: relief, conventional, and frontal. Relief rainfall occurs when warm, moist air is forced to rise over hills and cools, condensing into clouds and rain. Conventional rainfall results from the sun heating the ground and warming the air, causing it to rise and condense. Frontal rainfall happens when a warm air mass meets a cold air mass, with the warm air rising over the cold
The document discusses different types of clouds. It describes stratus clouds as gray clouds resembling fog without reaching the ground. Cirrus clouds are thin and wispy, moving from west to east. Cirrostratus clouds are thin and sheet-like, allowing the sun and moon to be seen through them. Cumulus clouds are puffy and cotton-like, sometimes taking shapes.
Clouds are formed when warm air rises and cools, causing water vapor to condense into water droplets. Clouds are classified by their height or shape above the earth's surface. Clouds associated with rain or snow have "nimbus" in their name, such as cumulonimbus clouds which form thunderstorms or nimbostratus clouds which bring rain or snow. Precipitation occurs when cloud droplets grow too large and fall from the sky.
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
What are clouds?
A cloud is a large collection of very tiny droplets of water or ice crystals. The droplets are so small and light that they can float in the air.
Why do clouds float?
A cloud is made up of liquid water droplets. A cloud forms when air is heated by the sun. As it rises, it slowly cools it reaches the saturation point and water condenses, forming a cloud. As long as the cloud and the air that its made of is warmer than the outside air around it, it floats!
There are 3 main types of clouds:
Cirrus or thin feathery clouds
Stratus or layered clouds
Cumulus or fluffy clouds
Cirrus Clouds
Are the most common of the
high clouds. They are composed of ice and are thin, wispy clouds blown in high winds into long streamers. Cirrus clouds are usually white and predict fair to pleasant weather. By watching the movement of cirrus clouds you can tell from which direction weather is approaching. When you see cirrus clouds, it usually indicates that a change in the weather will occur within 24 hours.
Stratus Clouds
are uniform grayish clouds that often cover the entire sky. They resemble fog that doesn't reach the ground. Light mist or drizzle sometimes falls out of these clouds.
Cumulus Clouds
are white, puffy clouds that look like pieces of floating cotton. Cumulus clouds are often called "fair-weather clouds". The base of each cloud is flat and the top of each cloud has rounded towers. When the top of the cumulus clouds resemble the head of a cauliflower, it is called cumulus congestus or towering cumulus. These clouds grow upward and they can develop into giant cumulonimbus clouds, which are thunderstorm clouds.
The Importance of Clouds
Clouds help regulate Earth's energy balance by reflecting and scattering solar radiation and by absorbing Earth's infrared energy.
Clouds are required for precipitation to occur and, hence are an essential part of the hydrologic cycle.
Clouds indicate what type of atmospheric processes are occurring (e.g., cumulus clouds indicate surface heating and atmospheric turbulence).
Clouds help redistribute extra heat from the equator toward the poles.
References
https://www.google.com/search?q=clouds&biw=1366&bih=624&source=lnms&tbm=isch&sa=X&ved=0ahUKEwixqOqjlu3NAhVHNpQKHbtGCE0Q_AUIBigB#imgrc=_
https://www.google.com/search?biw=1366&bih=624&tbm=isch&q=clouds+clipart&sa=X&ved=0ahUKEwir8paml-3NAhXGkJQKHSrFAPUQhyYIHQ&dpr=1#imgrc=WZWIVB52x_MJRM%3A
https://en.wikipedia.org/wiki/List_of_cloud_types
http://www.weatherwizkids.com/weather-clouds.htm
This document discusses cloud classification and describes the different types of clouds. It begins by explaining the Latin prefixes used to classify clouds by altitude, such as "cirro-" for high-level clouds above 20,000 feet composed of ice crystals. Mid-level clouds between 6,500 and 20,000 feet use the prefix "alto-", and can contain water, ice, or a mix. Low clouds below 6,500 feet do not use a prefix. The document then describes the main types of high, mid, and low clouds such as cirrus, altostratus, stratocumulus, and cumulonimbus clouds. It explains the characteristic appearances and formations of each cloud type.
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Still I Rise by Maya Angelou
-Table of Contents
● Questions to be Addressed
● Introduction
● About the Author
● Analysis
● Key Literary Devices Used in the Poem
1. Simile
2. Metaphor
3. Repetition
4. Rhetorical Question
5. Structure and Form
6. Imagery
7. Symbolism
● Conclusion
● References
-Questions to be Addressed
1. How does the meaning of the poem evolve as we progress through each stanza?
2. How do similes and metaphors enhance the imagery in "Still I Rise"?
3. What effect does the repetition of certain phrases have on the overall tone of the poem?
4. How does Maya Angelou use symbolism to convey her message of resilience and empowerment?
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2. Cumulus Large puffy clouds Warm air rises and cools below its dew point then condenses Below 2.5km Showers or snow Cumulonimbus clouds create thunderstorms
3.
4. Stratus A blanket of clouds Warm air slides over cool air and cools Below 2.5km Drizzle
5.
6. Cirrus Light and feathery clouds Formed very high in the atmosphere Above 6km No precipitation
14. Links to cloud games Click here to play the cloud matching game. Click here to play the cloud concentration game.
15. sources Web weather for kids http://eo.ucar.edu/webweather/cloud3.html Types of clouds http://schoolscience.rice.edu/duker/weatypeclouds.html S’Cool http://asd-www.larc.nasa.gov/SCOOL/tutorial/clouds/cloudtypes.html