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Published byPeter Hill Modified over 9 years ago
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Made up of mainly two gases: – Nitrogen 78% – Oxygen 21% – Trace Gases 1%
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made up of 5 layers: – Troposphere – Stratosphere – Mesosphere – Ionosphere – Thermosphere
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The atmospheric layer we live in. Almost all weather occurs here. Contains water vapor and oxygen. Highest density Temps decrease as you increase altitude until you reach the top of the layer called the tropopause.
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Within the troposphere a temperature inversion may occur. This is a condition where warmer air traps cooler air near the Earth’s surface. This can cause air to get thick with pollution, where it can’t escape.
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– Lacks O 2 and water vapor. (no weather) – Contains the ozone (O 3 ) layer. (this layer absorbs solar UV radiation) – Temperatures increase as you gain altitude. – Higher altitude than most aircraft would fly
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– The coldest of layer of the atmosphere. (-80 0 C) – Temperature decreases with altitude
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Consists of upper mesosphere and lower thermosphere. Contains charged ions that reflect radio waves allowing transmissions to travel great distances. Radio waves will travel farther at night than during the day. (less ions) Where the aurora borealis can be seen. (excited photons)
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Most outer layer. Hottest layer (980 0 C) temperatures will increase with increase altitude It absorbs solar radiation
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Early atmosphere was much different during Earth’s early days. Volcanic eruptions released H 2, ammonia, methane. CO, CO 2 and N 2. No oxygen was present
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Around 2.5 billion years ago single celled organisms evolved to capture the suns energy and CO 2 to start the photosynthesis process Then plants began appearing releasing oxygen into the atmosphere.
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350 million years later aerobic organisms came along and balanced the atmosphere. They took in oxygen and released carbon dioxide as a by product during respiration. And thus the O 2 and CO 2 cycle was created.
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Protects us from UV radiation. Can be destroyed by chlorofluorocarbons or CFC’s Used during 1950s thru 1980s in refrigerators and spray cans. CFCs are now banned in most countries Ozone layer is repairing itself
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Ozone while helpful in stratosphere, is very toxic if trapped in the troposphere. Main gas pollutant from cars, trucks, factories that causes smog.
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The process by which the atmosphere traps some of the energy from the sun in the troposphere. CO 2, water vapor, and other gases absorb the suns energy (greenhouse gases) Keeps the planets climate balanced
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We are adding more and more CO 2 and other greenhouse gases into the atmosphere: – Forest fires and volcanoes – Air Pollution from fossil fuel burning – Increasing human population – Decrease in plant life and rain forest – Increase of cattle grazing
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The continuous movement of water from atmosphere to Earth and back. 4 mechanisms of travel
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Water enters the atmosphere: 1. Evaporation Evaporation occurs at the lakes, rivers, and oceans. 2. Transpiration evaporation of water through plant’s leaves.
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Water Exits: 3. Condensation Water vapor rises until it is cool enough to condense to form clouds. 4. Precipitation When the cloud become full of water droplets they will release moisture back down to Earth in the form of rain, sleet, ice, or snow.
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Condensation Evaporation
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Water vapor is always in the air Humidity – The quantity/amount of water vapor in the atmosphere Relative humidity (percentage) – is the actual amount of water in the atmosphere compared to maximum amount it can hold. The higher the temperature, the more water that can be held in the air.
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The temperature at which water vapor molecules start to form liquid water. Higher the humidity the higher the dew point. dew point dew point
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Made up of tiny condensed droplets of liquid water. 3 main types
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highest altitude clouds appear wispy and light.
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layered or sheet like clouds form at lower altitudes.
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white and fluffy appear at many levels.
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Other clouds are a combination of the 3 cloud types. The root nimbus means the cloud contains precipitation. (grayer color) Ex. cumulonimbus produce thunderstorms
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The pressure due to the weight of the atmosphere. Measured with an instrument called a barometer. Air pressure decreases with altitude in the troposphere
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Caused by differences in air pressure between air masses. The greater the difference the stronger the wind. Air always flows from high pressure to low pressure – Pressure inside a plane is greater, so air would be sucked out if a window broke
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Coriolis effect. the change in direction of an object’s path due to Earth’s rotation.
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Winds in the Northern hemisphere curve right. Winds in the southern hemisphere curve left.
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The condition of the atmosphere at any given time Weather is caused by traveling air masses. – Large bodies of air with the same general characteristics throughout.
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A boundary where two air masses with different densities meet. Fronts cause precipitation, change in temperature, and a change in wind direction.
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Warm front -warm air moves over cooler air forming clouds. -Produces steady rain or snow for a couple of days. Cirrus and cirrostratus clouds
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Cold fronts -Cold air moves under slow moving warm air -Brings high winds, thunderstorms, and possible tornadoes. Cumulonimbus clouds
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Two air masses meet Neither is displaced Air masses move side by side Similar to warm front weather
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Lightening is caused by a build up of electrical charges from water droplets and ice crystals in clouds. When opposite charges are found on the ground or other clouds, lightening strikes. Thunder is the sound of lightening.
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If you count to 10 or less after seeing lightning before hearing thunder, then the storm is less than two miles away.
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Form during severe thunderstorms. Form from cool air from the north, and warm air from south. Tornadoes begin as a funnel cloud that intensifies until it touches ground Most violent winds on Earth 310mi/hr Most common in the Midwest
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Very large storms with high winds. Also known as cyclones and typhoons Form in the tropics Created by rising warm water vapor from warm ocean water. Then powered by the energy released from water vapor condensing into clouds
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Produced by meteorologists to help forecast weather. They use many variables – Precipitation and cloud cover – Wind speed -Air pressure (isobars) – fronts
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Average weather condition over many years for a particular region. It is not measured day by day.
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1. Latitude (closeness to equator) Angle at which the sun hits Earth 2. Cycling of seasons and season Length The tilt of the earth’s axis as it travels a revolution around the sun is the reason that we have seasons. 3. Yearly rainfall 4. Topography (type of land) Elevation, amount of water, mountains or flatness
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