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Published byRoxanne Booth Modified over 9 years ago
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What is the Atmosphere? The layer of gases that surrounds our planet.
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Why is it important? Our atmosphere makes life possible on our planet.
Provides us with oxygen. Keeps surface warm so water can exist as a liquid. Protects the surface from dangerous radiation from the sun.
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What is the Composition of the Atmosphere?
Nitrogen makes up 78% of our atmosphere Oxygen makes up 21% Argon makes up almost 1% All other gases have only trace amounts
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What was Earth’s Early Atmosphere?
The Precambrian atmosphere was composed mainly of nitrogen and carbon dioxide, along with some methane and ammonia. Volcanoes spewed water vapor, carbon monoxide, and even more nitrogen and carbon dioxide into the air. So where did the abundant oxygen that has made life as we know it come from?
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What was Earth’s Early Atmosphere cont?
The first life on Earth was cyanobacteria (blue-green algae). They used photosynthesis to turn CO2 into the food and energy they needed to survive. Photosynthesis gives off oxygen as a waste product. So over the millions of years, oxygen given off by algae built up in the atmosphere, while the amount of CO2 declined.
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What are the Layers of the Atmosphere?
Exosphere- lowest density Thermosphere (Ionosphere) Mesosphere Stratosphere Troposphere -highest density
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Layers Bun Mayonnaise Lettuce Tomato Hamburger Bun
The typical hamburger might look like this: bun, hamburger meat, tomato, lettuce, mayonnaise and bun. Hamburger Bun
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Exosphere Thermosphere Mesosphere Stratosphere Troposphere Earth
Name The Different Layers as they come in, also explain that the Exosphere is not really a layer but is the beginning of outer space. Troposphere Earth
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Exosphere 500-520 kilometers above earth
This outermost layer of the atmosphere is the closest to space and has the least amount of gas atoms and molecules In the exosphere, molecules and atoms escape into space. This layer is also where satellites orbit the Earth. Hottest layer due to sun’s light being converted to thermal
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Thermosphere The thermosphere occurs from 85 to 500 kilometers from the surface of the Earth. This atmospheric layer is called the upper atmosphere. The thermosphere contains thin layers of gases, which absorb much of the sun’s light. This causes the thermosphere to be significantly warmer than other layers. But not as hot as exosphere Auroras occur and the space shuttle orbits in this layer of the atmosphere.
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Mesosphere The mesosphere layer lies from kilometers above the Earth. Meteors leave trails when hitting this layer of atmosphere, as the thick gases slow them down and they eventually burn up.
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Stratosphere The stratosphere extends from 10 to 50 kilometers above the surface of the Earth. Aircraft fly in this layer Weather balloons penetrate the stratosphere, relaying pertinent information to scientists. Contains the ozone layer which scatters harmful ultra-violet radiation
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Troposphere The troposphere is the layer of the atmosphere where the weather happens. Lying just above Earth, this layer extends from the surface to 10 kilometers above. The gases thin and temperatures drop as altitude increases. This layer contains half of the gases in the atmosphere and they are generally well blended. This layer is heated from the ground.
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What is weather? It is the state of the atmosphere (troposphere) at a specific time and place. Components of weather include air pressure, wind, temperature, humidity and precipitation
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Sun’s role in weather! Solar energy from the sun strikes the Earth’s surface. This transfer in energy drives the production of all weather conditions. Examples: water cycle, wind, temperature, etc. What would happen if there wasn’t a sun? What type of weather would the Earth have?
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Sun’s role clip
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What happens to the Solar Energy?
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Why does the amount and intensity of sunlight vary throughout the year?
Tilt of the Earth’s axis Position in revolution (orbit) around the sun Which place receives the same amount and intensity of sunlight throughout the year? The equator
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(sun aims directly at equator)
The Tilting affect! Fall (sun aims directly at equator) Summer (northern hemisphere tilts toward sun) Spring (sun aims directly at equator) 23.5º Winter tilts away from sun) Solar radiation seasons animation length of day animation
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What is climate? What is Ohio’s climate?
1. Climate is long-term weather conditions 2. Temperature and precipitation are the most important expressions of climate What is Ohio’s climate? Temperate Cold winters Hot summers Average rain/snowfall
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HOW DOES CLIMATE INFLUENCE OTHER ASPECTS OF THE ENVIRONMENT?
Vegetation is the most visible expression of climate Animal life adapts to both climate and vegetation Soils develop in response to climate and vegetation Landforms Water resources
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Distribution of Biomes based on climate
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What is the water cycle? It is the movement of water to and from the lithosphere and the atmosphere. 1.Energy from the sun drives the cycle causing water to evaporate. 2.The water vapor eventually condenses when it cools to form clouds. 3.Eventually the water droplets get to heavy and fall back to the earth as precipitation. 4.The water from the precipitation eventually runs-off into bodies of water.
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The water cycle! water cycle animation evaporation
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Air Pressure Clips (fwd)
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What is Air Pressure air pressure is caused by the weight of the air pressing down on the Earth, the ocean and on the air below the pressure depends on the amount of air above the measuring point and falls as you go higher air pressure changes with weather air pressure is measure in pounds per square inch. Average air pressure is p.s.i.
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Air Pressure High Pressure areas: Dense Sinking air masses which make it difficult for air to rise and form clouds. Results - Clear sunny weather is the result. Low Pressure Areas: Less dense air is able to rise resulting in cloud formation Results - Cloudy weather is the result.
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Different Temperatures - Different Pressures
Less Dense Pressure Cool Air Denser More Pressure Warm Air
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Moist surface warmed by sun Flows toward low pressure,
picks up moisture and heat Warm, dry air Hot, wet air Falls, is compressed, warms Rises, expands, cools Heat released radiates to space LOW PRESSURE HIGH Cool, dry Condensation and precipitation
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View pressure systems
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How does differences in air pressure create wind?
Wind moves from high pressure areas to low pressure areas because there is less molecules in the low pressure area. What are isobars? Isobars connect areas of equal pressure Close together = greater difference in air pressure STRONG winds Far apart = less difference in air pressures Light winds
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Isobars and Wind
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Measuring devices Anemometer: measures wind speed
Barometer: measures air pressure
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Air masses clip
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Air masses
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What is an air mass? Air mass – a section of air that has similar characteristics to the area it formed over(warm dry, warm moist, cold dry, and cold moist) Which air mass would be the most dense? Least dense?
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Continental Arctic (cA):
Frigid – record low temperatures Dry - very low dew points Dense - very high barometric pressure Usually originate north of the Arctic Circle Siberian Express Usually once or twice a winter very rarely form during the summer because the sun warms the Arctic.
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Continental polar (cP):
Cold and dry - stable Usually originates in NW Territory of Canada Influences mainly the northern USA Responsible for clear and pleasant weather during the summer Usually in winter Creates troughs in the polar jet stream Lake effect snow in Great Lakes areas
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Maritime polar (mP): Cool and moist - unstable
Originate over N. Atlantic and N. Pacific Main Influence - the Pacific Northwest and the Northeast. can form any time of the year Generally not as cold as cP air masses
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Maritime tropical (mT):
Warm and very moist – unstable Originate in the Gulf of Mexico and the Southern Atlantic Ocean Influences the eastern USA Most prevalent during summer Responsible for hot, humid summer days across the South and the East.
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Continental Tropical (cT):
Very Hot and very dry – stable aloft Originates in Desert Southwest and northern Mexico Occurs in the summer, rarely in winter Usually keeps the Desert Southwest scorching above 100oF during summer Generally clear skies, hot, low humidity
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Coriolis Effect Clip (Moving Air masses)
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What is humidity? Humidity refers to the amount of moisture that is in the air (water vapor) It is measured with a device called a hygrometer What temperature of air will be more humid ? why? What is the temperature when the water vapor condenses?
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Fronts clip
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Fronts: Cold Warm Stationary The leading edge (front) of an air mass
Characterized by shift/change in weather Cold Warm Stationary
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Fronts and their symbols
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How does it affect the weather?
What is a warm front? It is the leading edge of a warm air mass How does it affect the weather? lower pressure Warmer temperatures Possibly long, steady precipitation Stratus clouds Light winds
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Graphic Depiction!
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Warm Front
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Warm Front
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How does it affect the weather?
What is a cold front? It is the leading edge of a cold air mass How does it affect the weather? Higher pressure The temperature drops rapidly Precipitation can be heavy at the front, but short lasting (ex. Thunderstorms, tornados, etc.) Cumulonimbus clouds Strong winds
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Cold Front
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Cold Front (Fozzy)
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Cold Front
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In the summer, cold fronts can trigger:
thunderstorms large hail dangerous winds tornadoes
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Stationary Front
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What is a stationary front?
When a warm or cold front stops moving, it becomes a stationary front
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What is humidity and how is it measured?
Humidity is the amount of water vapor that exists in the air. The warmer the air, the more moisture can be present. Think about muggy days in August vs. Frigid days of January. Humidity is measured with a hygrometer
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Clouds clip
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HOW ARE CLOUDS FORMED Water evaporates Water vapor rises
Water vapor loses energy (cools) and condenses Clouds form (clouds are actually liquid water)
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CLOUD CLASSIFICATION Cirrus-high level clouds that have bases below 7,000 feet Cumulus- mid-level clouds that have bases between ,000 feet Straus-low level clouds that have bases below 6,500 feet Cumulonimbus-tallest of all clouds that can go up to 60,000 feet.
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Cloud classification root words!
Latin Root Translation Example cumulus heap Fair weather cumulus stratus Layer Altostratus cirrus Curl of hair Cirrus nimbus Rain Cumulonimbus
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CIRRUS High altitude and wispy Some have a wavelike appearance
Are usually thin allowing moonlight and sun to shine through Associated with fair weather
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CUMULUS Usually puffy Noticeable vertical development
Have popcorn appearance Can be widely scattered or clumped Associated with fair weather
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STRATUS warm front clouds
Lowest of the low clouds Appear as an overcast, but can be scattered Can be in layers Associated with long periods of rain fog
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CUMULONIMBUS cold front clouds
Can produce lightning, heavy rains, hail, strong winds, and tornados. They are the tallest of all clouds
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What is weather forecasting
Weather forecasting is the application of science and technology to predict the state of the atmosphere for a future time and a given location. Forecasts become less accurate as the difference in time between the present moment and the time for which the forecast is being made (the range of the forecast) increases. Why?
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Why is weather forecasting important?
Air traffic Boating Military Agriculture Public safety
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Who is responsible for predicting the weather?
Meteorologists – they analyze weather data and make weather forecasts based on the data
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What tools are used for weather forecasting?
A weather balloon measures weather high in the troposphere. A satellite orbiting Earth takes pictures of clouds from space to help us see where and how fast clouds are moving. A radar shoots a microwave into a cloud to shows where precipitation is falling and how much. The wave bounces back when it hits the precipitation. It can also spot severe storms and how fast they are moving.
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How is temperature measured and displayed on a map?
Thermometer measures the temperature of an air mass! The reading should be taken in the shade. Isotherms connect areas of equal temperatures on a map just like isobars!
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Weather Satellite Doppler radar Weather Balloon
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