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Bell Work In which layer of the atmosphere does most of the weather we see occur? In which layer of the atmosphere is the Aurora produced? The air is made up of predominantly what type of gas?
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Atmosphere – Air Masses and Fronts
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Which has more heat, a small cup of hot water (at 80⁰C) or a large tub of hot water (also at 80⁰C)?
Which object contains the most heat, a boiling pot of water (0.5kg, at 100⁰C) or a gigantic iceberg (109 kg, at 0⁰C)?
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Energy Heat: energy transfer between molecules in motion
Temperature: a measure of the average heat energy of a substance All molecular motion stops at -273⁰C
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Amount of water vapor in the air
Humidity: Amount of water vapor in the air Relative humidity- amount of water vapor in air compared to what it can hold at that temp. 25% Relative Humidity 100% Relative Humidity
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Dew Point The temperature at which a gas condenses into a liquid.
Depends on temp. & humidity
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If Temperature Then density Increases Decreases Warm Air: rises → cools → its density increases → sinks Cold Air: sinks → warms → its density decreases → rises
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Air masses Large uniform volume of air that is consistent in temp., density & humidity Pushed around globe by winds
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Name Description c Continental Dry m Maritime Humid E Equatorial Hot T
3. Take on the characteristics of area over which it forms: Name Description c Continental Dry m Maritime Humid E Equatorial Hot T Tropical Warm P Polar Cold A Arctic Very cold
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cA mP cP mP mT cT mT
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Bell Work Why does the temperature in the: Troposphere ↓ with height?
Stratosphere ↑ with height? Mesosphere ↓ with height? Thermosphere ↑ with height?
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Movement of Air Masses Travel with global wind patterns In US move from west to east Air masses change as they move FRONT: an area where two air masses meet
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A. Cold Front: Cold air mass runs into a warm air mass
Cold air forces warm mass to rise Rising warm air cools → releases moisture Symbol on a map:
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Cold Front Weather A shift in wind direction Sudden drop in temp.
Increasing clouds Heavy rains & thunder Followed by clearing with colder, drier weather
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B. Warm Front: Warm air mass runs into a cold air mass Warm air mass is pushed up Moisture in warm air cools & condenses → leads to rain Warm air slowly pushes away cold air Symbol on a map:
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Warm Front Weather Winds change slightly
Slow, steady increase in temp. Continuous precipitation along front Hotter weather follows front
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Stationary Front Weather
C. Stationary Front: Two air masses meet and neither advances Symbol on map: Stationary Front Weather Continuous heavy precipitation along front Frequent flooding
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D. Occluded Front: Cold air mass overtakes a warm front Symbol on map:
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Occluded Front Weather
Colder temperatures Continuous heavy precipitation along front Light rain continues after front passes
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Bell Work What is the difference between heat and temperature?
1/27/16 What is the difference between heat and temperature? How does temperature affect the movement of air? Get the air masses and fronts worksheet out to review (do NOT turn in) Get your notebooks out for the notebook quiz
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A B C Bell Work What type of front is shown in A? How do you know?
1/28/16 A Bell Work What type of front is shown in A? How do you know? What type of front is shown in B? How do you know? Identify each of the front symbols shown in C. B C
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Clouds A collection of water droplets or ice crystals formed when water vapor condenses into condensation nuclei.
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Cloud names: Alto-: clouds at middle altitudes Cirro-: clouds that form at high altitudes Nimbo- or -nimbus: clouds likely to produce precipitation Cumulo-: piled up clouds Strato-: layered clouds
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Stratus clouds: Form in layers Cover large areas Nimbostratus clouds: Dark stratus clouds Produce continuous rain
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Cumulus clouds: Puffy, white clouds with flat bottoms When small indicate fair weather When large (Cumulonimbus) produce stormy weather
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Cirrus Clouds: Thin, feathery, white clouds Found at high altitude When they get thicker, a change in weather is coming
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Fog: stratus cloud that formed close to ground
Contrails: clouds formed when water vapor condenses around particles in aircraft exhaust
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Heat: energy transfer between moving molecules Heat energy can be transferred in 3 ways:
Radiation: transfer of energy through electromagnetic waves (e.g. the sun)
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Conduction: transfer of heat energy through a solid object e. g
Conduction: transfer of heat energy through a solid object e.g. a blacksmith heating metal to change its shape
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Convection: transfer of heat energy through movement of a liquid or gas
Water when it boils Magma in Earth’s mantle Ocean currents Air in the atmosphere
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Pressure: Force applied perpendicular to an object Atmospheric Pressure: Force applied against a surface by the weight of the air above
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Atmospheric Pressure Systems
High Pressure System: Cool air moves in and sinks Winds blow out away from high pressure Isobars: Lines of equal pressure
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High Pressure System: Surface winds spiral outward from center – blow clockwise in Northern hemisphere Brings fair, dry weather
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Low Pressure System: Hot air rises leaving a void (empty space) Winds blow in toward center of low pressure
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Low Pressure System Winds blow Counter-clockwise in Northern hemisphere Bring clouds & precipitation
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Cyclones: Occur where a lower pressure area is surrounded by higher pressure areas Air spirals towards center of low pressure Marked by L on weather map Bring clouds and rain or snow
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Anticyclone: A rotation of air around an area of high pressure Air spins clockwise away from center of the high pressure Marked by H on weather map Brings fair weather
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Bell Work 2/1/16 1. Read the article: “Auroras in the Night Sky” 2. Answer the questions on the ½ sheet of paper
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Global Pressure Cells Hadley Cell: Warm air at the equator rises, moves towards the poles, cools, sinks at ~30° north & south of equator then moves back towards equator.
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Polar cell: Cold air at the poles sinks, moves away from pole, warms, rises at about 60°N or south and moves back toward poles
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Ferrel cell: Sinking cold air at convergence with the Hadley cell moves north Warmer air is pushed up at convergence with the air coming from the Polar cell
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Wind: movement of air caused by differences in air pressure
↑ pressure difference → ↑ wind speed Temperature (heat energy) affects air pressure: Warm air rises - ↓ pressure Cold air sinks - ↑ pressure
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Global Wind Systems: caused by
Pressure gradients in Cells Coriolis Effect
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Polar Easterlies: winds blow EAST to WEST from the poles to 60⁰ N. & S. of equator
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Westerlies: Winds blow from 30° latitude WEST to EAST towards polar easterlies in both hemispheres
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Trade Winds: Winds blow from 30° latitude EAST to WEST towards the equator in both hemispheres
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Jet streams Narrow belts of high speed winds (up to 400 km/h) in the upper troposphere and lower stratosphere.
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Doldrums: Located along the equator; no winds blow; rising air & low pressure
Horse Latitudes weak winds at 30 N and 30 S of equator
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Bell Work North Carolina is at latitude 35.5°N of the equator.
1. What wind belt blows over us? 2. From what direction do the winds blow?
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Cold front: Rainfall can be torrential and wind speeds can be high
Cold front: Rainfall can be torrential and wind speeds can be high. Blue lines with triangles on one side represents cold fronts on weather maps. The direction the triangles point is the direction in which the cold front is moving.
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Warm front: Brings a gradual increase in rainfall followed by clearing and warming after the front passes. Can bring prolonged rain. A red line with semi-circles on one side represents warm fronts. The side the semi-circles are on represents the direction the front travels.
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Occluded front: Formed when a cold front overtakes a warm front
Occluded front: Formed when a cold front overtakes a warm front. Weather events depend on whether it is a warm or cold occlusion. An occluded front usually brings heavy precipitation and changing wind directions. A purple line with semi-circles and triangles both on the same side represents occluded fronts and shows the direction of travel
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Stationary front: Indicates a non-moving boundary between two different air masses. These fronts have long continuous rainy periods that linger for extended periods in one area and move in waves. A semi-circle bordering one side and triangles along the opposite side represents that the front is not moving in any direction.
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