THE ATMOSPHERE The Atmosphere Air is a MIXTURE

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THE ATMOSPHERE

THE ATMOSPHERE

The Atmosphere �Air is a MIXTURE of gases. �Nitrogen = 78% �Oxygen = 21%

The Atmosphere �Air is a MIXTURE of gases. �Nitrogen = 78% �Oxygen = 21% �Argon = < 1% �CO 2 =. 039%

The Atmosphere �Components of Air 1. Gases 2. Water vapor a. b. Varies 0

The Atmosphere �Components of Air 1. Gases 2. Water vapor a. b. Varies 0 – 4% Depends on location and weather pattern 3. Aerosols (solids and liquids suspended in air) 4. Ozone a. b. 3 atoms of oxygen bonded together. O 3 Ozone layer located at the top of the Stratosphere

Structure of Atmosphere �Air Pressure �Decreases as you rise in altitude �Average = 1013.

Structure of Atmosphere �Air Pressure �Decreases as you rise in altitude �Average = 1013. 2 mb (millibars) �Measured with a barometer

Structure of Atmosphere � 4 layers based on temperature change. �Troposphere � Layer we

Structure of Atmosphere � 4 layers based on temperature change. �Troposphere � Layer we live in � Temp. decrease �Stratosphere � Ozone layer here � Temp. increase �Mesosphere � Coldest �Thermosphere � Space shuttle � Hubble telescope � Temp. increase

Atmospheric Heating �Heating of the Atmosphere from the Sun’s energy. � 3 methods of

Atmospheric Heating �Heating of the Atmosphere from the Sun’s energy. � 3 methods of heat transfer Energy Transfer 1. Conduction a. by contact of molecules 2. Convection a. By different densities of air (hot/cold) 3. Radiation a. By electromagnetic waves Surface

GREEN HOUSE EFFECT � Incoming radiation � Mostly visible light � Gets absorbed by

GREEN HOUSE EFFECT � Incoming radiation � Mostly visible light � Gets absorbed by surface � Changed to Infrared (heat) � Greenhouse gases: � H 2 O � CO 2 � Absorb Infrared heat and keep air near surface warm. � Increase of Greenhouse gases � Causes increase of heat trapped � Called Global Warming

Ozone Layer �O 3 �Absorbs UV rays from sun � Changes it to heat

Ozone Layer �O 3 �Absorbs UV rays from sun � Changes it to heat � Causes increase temperature in stratosphere �Ozone Problem �O 3 layer is getting thinner �Broken up by CFC’s (chlorofluorocarbons) �Causes increase UV rays to reach surface (increase skin cancer)

Atmospheric Energy Budget �What happens to the Energy of the Sun as it hits

Atmospheric Energy Budget �What happens to the Energy of the Sun as it hits the atmosphere? Of the total energy that 100% strikes our atmosphere: • Radiation absorbed by clouds or atmosphere? 20% • Total scattered and reflected back to space? 30% • Absorbed by Earth’s surface? 50%

Affect of Surface Material �Albedo: Reflectivity of the surface �High Albedo = Very reflective,

Affect of Surface Material �Albedo: Reflectivity of the surface �High Albedo = Very reflective, poor absorber �Low Albedo = Good absorber, poor reflector �Color: �Darker color = good absorber = Low Albedo �Light color = good reflector = High Albedo

Effect of Surface Material Land Verses Water �Which heats up the quickest? �Which heats

Effect of Surface Material Land Verses Water �Which heats up the quickest? �Which heats to a higher temperature? �Which will cool down the quickest? �Which will cool to a cooler temperature? �How does this temperature change affect where you live?

Effect of Surface Material How does living near the ocean affect the air temperature?

Effect of Surface Material How does living near the ocean affect the air temperature? �Winter? �Summer? How does living inland affect the air temperature? �Winter? �Summer? Which location would have a greater change of temperature during the year?

Moisture in the Atmosphere �Humidity = Amount of water vapor in the air �

Moisture in the Atmosphere �Humidity = Amount of water vapor in the air � 5 g H 2 O/kg of air �Saturated air = Holding all the water vapor it can hold. �Capacity = The amount of something it can hold �When something is filled to CAPACITY it is SATURATED. Water vapor Capacity or Air Direct Relationship: As air temperature INCREASES, its water vapor capacity INCREASES.

Moisture in the Atmosphere �Relative Humidity = The amount of water vapor in the

Moisture in the Atmosphere �Relative Humidity = The amount of water vapor in the air compared to how much it can hold at that temperature. �Given as a % of fullness. �As the temperature changes throughout the day, so does the Relative Humidity.

Moisture in the Atmosphere �Dew-point Temperature: The temperature the air must cool down to

Moisture in the Atmosphere �Dew-point Temperature: The temperature the air must cool down to for the water-vapor in the air to condense as liquid onto objects. �Usually occurs in the evening as the temperature decreases. �Relative humidity = �Air is % (holding all the water-vapor it can hold) �More humid air = higher dew-point temperature �What do you call it when the dew-point is below freezing?

Moisture in the Atmosphere Clouds �Classified by: 1. Height above ground Low � Middle

Moisture in the Atmosphere Clouds �Classified by: 1. Height above ground Low � Middle � High � 2. Appearance Layered � Puffy � Wispy �

Clouds �Cloud TYPE roots: 1. Cirro = curly 2. Cumulo = puffy(heaped) 3. Strato

Clouds �Cloud TYPE roots: 1. Cirro = curly 2. Cumulo = puffy(heaped) 3. Strato = layered 4. Alto = middle level 5. Nimbo/bus = rain Draw here:

Clouds �Classification of clouds �Cirro = High and wispy �Stratus = cover whole sky

Clouds �Classification of clouds �Cirro = High and wispy �Stratus = cover whole sky �Cumulo = clumpy (puffy) �Examples: �Cirrocumulus = �Altocumulus = �Cirrostratus = �Nimbostratus = �Cumulonimbus = Description:

Name each cloud type:

Name each cloud type:

Cumulonimbus cloud = Thunderstorms Thunderstorm: • Heavy down pour of rain • Thunder and

Cumulonimbus cloud = Thunderstorms Thunderstorm: • Heavy down pour of rain • Thunder and lightning • Gusty winds • Hail • Tornado possible Cumulus clouds Updraft builds vertical Breaks up