The Atmosphere Made up of mainly two gases: Nitrogen 78% Oxygen 21% Trace Gases 1%

Transcription

1 The Atmosphere 18.1

2 The Atmosphere Made up of mainly two gases: Nitrogen 78% Oxygen 21% Trace Gases 1%

3 Layers of the Atmosphere made made up of 5 layers: Troposphere Stratosphere Mesosphere Ionosphere Thermosphere

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5 1. Troposphere 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.

6 Troposphere Within the troposphere a temperature inversion may occur. This is a condition where warmer air traps cooler air near the Earth s s surface. This can cause air to get thick with pollution, where it can t escape.

7 Temperature Inversions

8 2. Stratosphere 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

9 Stratosphere

10 3. Mesosphere The coldest of layer of the atmosphere. (-80( 0 C) Temperature decreases with altitude

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12 4. Ionosphere 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. (exited photons)

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14 Aurora Borealis Northern lights

15 5. Thermosphere Most outer layer. Hottest layer (980 0 C) temperatures will increase with increase altitude It absorbs solar radiation

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17 Early Atmosphere Early Early atmosphere was much different during Earth s s early days. Volcanic Volcanic eruptions released H 2, ammonia, methane. CO, CO 2 and N 2. No oxygen was present

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19 Changing Atmosphere 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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21 Present Atmosphere 350 million years later aerobic animals 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.

22 Carbon Dioxide/ Oxygen Cycle

23 Our affect on the atmosphere. #1 Natural Stratosphere Ozone 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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28 #2 Man-made Ozone Ozone while helpful in stratosphere, is very toxic if trapped in the troposphere. Main gas pollutant from cars, trucks, factories that causes smog.

29 Ozone Issues:

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32 Greenhouse effect 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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34 #3 Enhanced Greenhouse Effect 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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37 #4 Enhanced Greenhouse Effect The cause of global warming (climate change) We are experiencing a major shift in the balancing of the Earth s s climate. All species and ecosystems are feeling the affects and there are many signs that it is happening. Still being debated whether man- made

38 Signs of Climate Change: Increasing Land drying up

39 Increasing global temperatures

40 Coral Reef Bleaching due to increasing ocean temperatures

41 Endangering Animal Species

42 Melting Ice Caps

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44 Melting Glaciers

45 Rising Sea levels

46 Increasing Extreme Weather Events

47 Are we not realizing the changes?

48 The Problem of Not Taking Action:

49 Not Much of a Debate:

50 Risk Assessment

51 A Political Satire

52 Water and Wind 18.2

53 The Water Cycle The continuous movement of water from atmosphere to Earth and back. 44 mechanisms of travel

54 The Water Cycle Water enters the atmosphere: 1.Evaporation Evaporation occurs at the lakes, rivers, and oceans. 2.Transpiration evaporation of water through plant s s leaves.

55 Transpiration

56 The Water Cycle 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.

57 Condensation vaporation

58 Water Vapor 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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60 I hope this planet doesn t have any water

61 Dew Point The temperature at which water vapor molecules start to form liquid water. Higher the humidity the higher the dew point.

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63 Clouds Form from the rising of warm water vapor in the troposphere. Made up of tiny condensed droplets of liquid water. 33 main types

64 1. Cirrus Clouds highest altitude clouds appear wispy and light.

65 Cirrus Clouds

66 2. Stratus Clouds layered or sheet like clouds form at lower altitudes.

67 Stratus Clouds

68 3. Cumulus Clouds white and fluffy appear at many levels.

69 Cumulus Clouds

70 Other Clouds 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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72 Nimbostratus

73 Cumulonimbus

74 Air pressure (Barometric Pressure) The The pressure due to the weight of the atmosphere. Measured with an instrument called a barometer. Air pressure decreases with altitude in the troposphere

75 Mercury Barometer

76 Wind 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

77 Cabin Pressure

78 Wind and the Earth Coriolis effect. the change in direction of an object s s path due to Earth s s rotation.

79 Wind and the Earth Winds in the Northern hemisphere curve right. Winds in the southern hemisphere curve left.

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81 coriolis effect

82 Weather and Climate 18.3

83 Weather 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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85 Fronts A 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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87 Front Types Warm front -warm air moves over cooler air forming clouds. -Produces steady rain or snow for a couple of days.

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89 Front Types Cold fronts -Cold air moves under slow moving warm air -Brings high winds, thunderstorms, and possible tornadoes.

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91 warm/cold fronts

92 Weather Events 1. Thunder Storms 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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95 Thunder Storm Safety If you count to 10 or less after seeing lightening before hearing thunder, then the storm is less than two miles away.

96 2. Tornadoes 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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101 3. Hurricanes 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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107 Weather maps Produced by meteorologists to help forecast weather. They They use many variables Precipitation and cloud cover Wind speed -Air pressure (isobars) fronts

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110 Climate Average weather condition over many years for a particular region. It is not measured day by day.

111 Climate Affected By: 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 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) 4. Elevation, amount of water, mountains or flatness