Top Banner
Atmosphere Atmosphere Properties Properties and Weather and Weather Notes Chapter 11-13 Notes Chapter 11-13
48

Atmosphere Properties and Weather Notes Chapter 11-13.

Dec 26, 2015

Download

Documents

Dale Holland
Welcome message from author
This document is posted to help you gain knowledge. Please leave a comment to let me know what you think about it! Share it to your friends and learn new things together.
Transcript
Page 1: Atmosphere Properties and Weather Notes Chapter 11-13.

Atmosphere PropertiesAtmosphere Properties and Weather and Weather

Notes Chapter 11-13Notes Chapter 11-13

Page 2: Atmosphere Properties and Weather Notes Chapter 11-13.

Atmosphere

ClimateWeatherThin envelope of gases that surrounds the planet.

The state of the atmosphere at a given place and time

Weather conditions at a locality averaged over a specified time period

Meteorology Study of weather and climate

Page 3: Atmosphere Properties and Weather Notes Chapter 11-13.

LayersLayers of Atmosphere of Atmosphere

Exosphere (outer space)Exosphere (outer space)

Ozone Layer

Weather occursWeather occurs

Page 4: Atmosphere Properties and Weather Notes Chapter 11-13.

TroposphereTroposphere

Layer closest to our earthLayer closest to our earth Extends to a height of 8-15 kilometers (5-9 Extends to a height of 8-15 kilometers (5-9

miles)miles) Temperature ranges from Temperature ranges from (63° to -62°F) Weather occurs hereWeather occurs here A very large thunderstorm could extend into the A very large thunderstorm could extend into the

next layer of the atmospherenext layer of the atmosphere The air that we breathThe air that we breath Can contain air pollution, bad ozone, smogCan contain air pollution, bad ozone, smog

Page 5: Atmosphere Properties and Weather Notes Chapter 11-13.

StratosphereStratosphere

22ndnd layer of the atmopshere layer of the atmopshere Ozone layer (good ozone) that shields us Ozone layer (good ozone) that shields us

from harmful radiation from the sunfrom harmful radiation from the sun Temperature increase as you go up Temperature increase as you go up

through the atmospherethrough the atmosphere Temperature is (Temperature is (27°F).

Page 6: Atmosphere Properties and Weather Notes Chapter 11-13.

MesosphereMesosphere

33rdrd layer of the atmosphere layer of the atmosphere Meteorites burn up in this sectionMeteorites burn up in this section Coldest layerColdest layer

Page 7: Atmosphere Properties and Weather Notes Chapter 11-13.

ThermosphereThermosphere

44thth Layer of the atmopshere Layer of the atmopshere UV radiation is absorbedUV radiation is absorbed Shooting starsShooting stars Hottest layerHottest layer

Page 8: Atmosphere Properties and Weather Notes Chapter 11-13.

Natural Atmosphere ProcessesNatural Atmosphere ProcessesOzone Shield in the StratosphereOzone Shield in the Stratosphere

Ozone shield is needed to filter out the sun’s UV Ozone shield is needed to filter out the sun’s UV radiation. 95% filteredradiation. 95% filtered

The ozone shield protects humans from skin The ozone shield protects humans from skin cancer, sun burns, eye cataracts, and damage cancer, sun burns, eye cataracts, and damage to the immune systemto the immune system

Prevents the oxygen in the troposphere from Prevents the oxygen in the troposphere from being converted to photochemical ozonebeing converted to photochemical ozone

Page 9: Atmosphere Properties and Weather Notes Chapter 11-13.

What causes ozone depletion?What causes ozone depletion?CFCCFC

CFC—chlorofluorocarbonsCFC—chlorofluorocarbons CFC-11 trichlorofluormethane, CFC-12 dichlorodifluoromethane CFC-11 trichlorofluormethane, CFC-12 dichlorodifluoromethane

also known as freonsalso known as freons Odorless, colorless, nontoxic, nonreactive, nonflamable, Odorless, colorless, nontoxic, nonreactive, nonflamable,

noncorrosivenoncorrosive CheapCheap Used a coolants for air conditioners, refrigeratorsUsed a coolants for air conditioners, refrigerators Used as propellants in aerosol spray cansUsed as propellants in aerosol spray cans Cleaners for computer chipsCleaners for computer chips FumigantsFumigants

Insoluble to water so they remain in the atmosphereInsoluble to water so they remain in the atmosphere Each molecule can last 65-385 yearsEach molecule can last 65-385 years Each chlorine atom converts ozone to oxygenEach chlorine atom converts ozone to oxygen

Page 10: Atmosphere Properties and Weather Notes Chapter 11-13.

Anthropogenic effects on Anthropogenic effects on biogeochemical cyclesbiogeochemical cycles

Carbon cycleCarbon cycle Adding carbon dioxide by burning Adding carbon dioxide by burning fossil fuels, deforestationfossil fuels, deforestation

Nitrogen cycleNitrogen cycle Adding NOx by burning fossil Adding NOx by burning fossil fuels, fertilizers, acid depositionfuels, fertilizers, acid deposition

Sulfur cycleSulfur cycle Volcanoes, burning fossil fuels, Volcanoes, burning fossil fuels, making acid depositionmaking acid deposition

Toxic metals Toxic metals (arsenic, (arsenic, cadmium lead)cadmium lead)

Injecting those into the Injecting those into the atmosphereatmosphere

Page 11: Atmosphere Properties and Weather Notes Chapter 11-13.

Nitrogen (78%) & Oxygen (21%) Nitrogen (78%) & Oxygen (21%) Carbon dioxide & others (trace amounts)Carbon dioxide & others (trace amounts)

Gases in AtmosphereGases in Atmosphere

Page 12: Atmosphere Properties and Weather Notes Chapter 11-13.

3 methods of energy transfer:3 methods of energy transfer:

1)1) RadiationRadiation= transfer of energy through = transfer of energy through space by visible light, UV light, and space by visible light, UV light, and electromagnetic waves electromagnetic waves EX: sunEX: sun

2)2) ConductionConduction= transfer of energy when = transfer of energy when molecules collide molecules collide EX: metalsEX: metals

3)3) ConvectionConvection= transfer of energy by flow of = transfer of energy by flow of a heated substance a heated substance EX: water, airEX: water, air

Page 13: Atmosphere Properties and Weather Notes Chapter 11-13.

Humidity vs. Relative HumidityHumidity vs. Relative Humidity

Humidity= amount of water vapor in the airHumidity= amount of water vapor in the air

Relative Humidity= ratio of water vapor in Relative Humidity= ratio of water vapor in the air relative to how much water vapor the air relative to how much water vapor the air can holdthe air can hold

0% very dry0% very dry 90% very wet (rain is near)90% very wet (rain is near)

Page 14: Atmosphere Properties and Weather Notes Chapter 11-13.

Relative Humidity• The relative humidity tells us how “full” the air is at the time of measurement.

• For example, 90% relative humidity means that at that moment the air is holding 90% of the maximum amount of water it could.

Page 15: Atmosphere Properties and Weather Notes Chapter 11-13.

Relative HumidityRelative Humidity

Measure of water vapor in the air.Measure of water vapor in the air. Instrument = Instrument = HygrometerHygrometer If air holds all the water vapor it can, it is at If air holds all the water vapor it can, it is at

100% RH and is said to be 100% RH and is said to be saturatedsaturated

Warm air can hold more water vapor.Warm air can hold more water vapor.

Page 16: Atmosphere Properties and Weather Notes Chapter 11-13.

Air MassesThere are two types of air masses:

1. Continental Polar air masses

2. Maritime Tropical air masses

Page 17: Atmosphere Properties and Weather Notes Chapter 11-13.

Coriolis EffectCoriolis Effect

http://www.classzone.com/books/earth_science/terc/content/visualizations/es1904/es1904page01.cfm Animation Animation

Particles are deflected in the Northern Particles are deflected in the Northern Hemisphere to the right and in the Hemisphere to the right and in the Southern Hemisphere to the left.Southern Hemisphere to the left.

Page 18: Atmosphere Properties and Weather Notes Chapter 11-13.

Trade WindsTrade Winds The sun warms the air and it rises to 20 to The sun warms the air and it rises to 20 to

30 degrees to the South and the North, 30 degrees to the South and the North, then is falls back downthen is falls back down

Page 19: Atmosphere Properties and Weather Notes Chapter 11-13.

Jet StreamJet Stream

The current of fast moving airThe current of fast moving air Usually moves from East to WestUsually moves from East to West

Page 20: Atmosphere Properties and Weather Notes Chapter 11-13.

Fronts

A front is the boundary separating air masses of different densities

Fronts extend both vertically and horizontally in the atmosphere

Page 21: Atmosphere Properties and Weather Notes Chapter 11-13.

Fronts: Five Types of Fronts1. Cold Front: The zone where cold air is replacing warmer air

• In U.S., cold fronts usually move from northwest to southeast

• Air gets drier after a cold front moves through

Page 22: Atmosphere Properties and Weather Notes Chapter 11-13.

Fronts: Five Types of Fronts2. Warm Front: The zone where warm air is replacing colder air

• In U.S., warm fronts usually move from southwest to northeast

• Air gets more humid after a warm front moves through

Page 23: Atmosphere Properties and Weather Notes Chapter 11-13.

Fronts: Five Types of Fronts3. Stationary Front: When either a cold or warm front stops moving

• When the front starts moving again it returns to either being a cold or warm front

Page 24: Atmosphere Properties and Weather Notes Chapter 11-13.

High and Low Pressure Areas

• High pressure causes air to sink

• Usually results in several days of clear sunny skies

• Air rises in low pressure areas and forms water droplets

• Usually results in rain and storms

Page 25: Atmosphere Properties and Weather Notes Chapter 11-13.

Temperature and ThermometerTemperature and Thermometer

Measurement of how rapid or slow a Measurement of how rapid or slow a molecule move aroundmolecule move around

Measured by a thermometerMeasured by a thermometer UnitsUnits

Fahrenheit (Fahrenheit (°F)°F) Celsius (Celsius (°C)°C) Kelvin (K)Kelvin (K)

Page 26: Atmosphere Properties and Weather Notes Chapter 11-13.

Wind Direction and SpeedWind Direction and Speed

Direction is measured Direction is measured with a “vane”with a “vane”

Speed is measured with Speed is measured with an “anemometer.”an “anemometer.”

Page 27: Atmosphere Properties and Weather Notes Chapter 11-13.

Pressure and BarometerPressure and Barometer

Air molecules push down Air molecules push down on objects—including us!on objects—including us!

Measured by Measured by BarometersBarometers DemonstrationDemonstration

Page 28: Atmosphere Properties and Weather Notes Chapter 11-13.

Doppler Radar EffectDoppler Radar Effect Doppler Effect is the movement of Doppler Effect is the movement of

frequencies going away or toward you as frequencies going away or toward you as the source movesthe source moves

Radar measures the amount of Radar measures the amount of precipitation in the airprecipitation in the air

Doppler RadarDoppler Radar

Page 29: Atmosphere Properties and Weather Notes Chapter 11-13.

Pressure-Temperature-Density Pressure-Temperature-Density RelationshipsRelationships

As Temperature , PressureAs Temperature , Pressure

As Temperature , PressureAs Temperature , Pressure

As Temperature, DensityAs Temperature, Density

**Temperature and Pressure are directly proportionate **Temperature and Pressure are directly proportionate (goes the same direction)(goes the same direction)

** Temperature and Density are inversely proportionate ** Temperature and Density are inversely proportionate (goes in the opposite direction)(goes in the opposite direction)

Page 30: Atmosphere Properties and Weather Notes Chapter 11-13.

What happens in the atmosphereWhat happens in the atmosphere

Most of the time, the temperature and Most of the time, the temperature and pressure decreases through the pressure decreases through the tropospheretroposphere

Sometimes….the atmosphere does not Sometimes….the atmosphere does not have perfect relationships between have perfect relationships between temperature, density, and pressure.temperature, density, and pressure.

Warm Air rises, cold air sinksWarm Air rises, cold air sinks

Page 31: Atmosphere Properties and Weather Notes Chapter 11-13.

Temperature InversionTemperature Inversion

When the cold air is on When the cold air is on top of the warm air. top of the warm air. The warm air can not The warm air can not rise to release rise to release pollution.pollution.

This can lead to smog This can lead to smog and pollution closer to and pollution closer to the earth’s surfacethe earth’s surface

Page 32: Atmosphere Properties and Weather Notes Chapter 11-13.

Dew Point and CondensationDew Point and Condensation

Temperature at which air must be cooled Temperature at which air must be cooled at constant pressure to reach saturationat constant pressure to reach saturation

Saturation= amount that the atmosphere Saturation= amount that the atmosphere can hold.can hold.

Higher the dew point then condensation Higher the dew point then condensation (changing gas to liquid) can occur and it (changing gas to liquid) can occur and it can rain.can rain.

Page 33: Atmosphere Properties and Weather Notes Chapter 11-13.

HeatHeat

Transfer of energyTransfer of energy

Hot ALWAYS travels into the ColdHot ALWAYS travels into the Cold

Page 34: Atmosphere Properties and Weather Notes Chapter 11-13.

Weather Station ModelWeather Station Model

Directions:

•Read the handout again to understand what each symbol means

•Use the chart to draw your own on in your lab book

Page 35: Atmosphere Properties and Weather Notes Chapter 11-13.

Weather MapsWeather Maps

From the weather maps, you are going to From the weather maps, you are going to answer the questions about the maps in answer the questions about the maps in your comp book.your comp book.

Page 36: Atmosphere Properties and Weather Notes Chapter 11-13.

Clouds Clouds Write this on your own paper for your notesWrite this on your own paper for your notes

Turn in your textbooks to page Turn in your textbooks to page 287287

Draw this chart on the screenDraw this chart on the screen

Using your textbook and table 11-Using your textbook and table 11-3, write what the description and 3, write what the description and draw a picture of the clouddraw a picture of the cloud

When you have finished see me to When you have finished see me to pick up your construction paper pick up your construction paper and cotton balls. You will and cotton balls. You will reconstruct the clouds out of the reconstruct the clouds out of the cotton balls. Please label each cotton balls. Please label each cloud.cloud.

After everyone builds the clouds After everyone builds the clouds we will go outside and observe we will go outside and observe themthem

Cloud NameCloud Name DescriptionDescription PicturePicture

CirrusCirrus

CumulusCumulus

StratusStratus

NimbusNimbus

CumulonimbusCumulonimbus

Page 37: Atmosphere Properties and Weather Notes Chapter 11-13.

Tornadoes vs. HurricanesTornadoes vs. Hurricanes

TornadoTornado Whirlwind of air on Whirlwind of air on

landland Measured by Fujita Measured by Fujita

scalescale F0-F5F0-F5

HurricanesHurricanes Whirlwind of air on Whirlwind of air on

waterwater Measured by Saffir Measured by Saffir

Simpson IndexSimpson Index 1-51-5

Page 38: Atmosphere Properties and Weather Notes Chapter 11-13.

Severe WeatherSevere Weather

ThunderstormsThunderstorms All contain lighting, cumulunimbus cloudsAll contain lighting, cumulunimbus clouds Single CellSingle Cell Multi CellMulti Cell Super Cell Super Cell violent tornados violent tornados

May produce flash floods/hail/tornadosMay produce flash floods/hail/tornados Downdrafts Downdrafts damaging winds near damaging winds near

surfacesurface

Page 39: Atmosphere Properties and Weather Notes Chapter 11-13.

TornadosTornados

Violently rotating column of Violently rotating column of air in contact with the air in contact with the ground ground

Rotating updraftRotating updraft is a key to is a key to the development tornado. the development tornado. Caused by wind shearCaused by wind shear

5mph

25 mph

Page 40: Atmosphere Properties and Weather Notes Chapter 11-13.

MesocycloneMesocyclone

Page 41: Atmosphere Properties and Weather Notes Chapter 11-13.

How does lightening form?How does lightening form? Air friction in the Air friction in the

cloudsclouds Separate + and – Separate + and –

create voltage create voltage channelchannel

Lightning kills Lightning kills more people than more people than tornados, tornados, hurricanes hurricanes

Page 42: Atmosphere Properties and Weather Notes Chapter 11-13.

What causes thunder?What causes thunder?

30,000 30,000 ooC air C air expandsexpands

““Explosion of Air”Explosion of Air” Light waves travel Light waves travel

faster than sound faster than sound waveswaves

Page 43: Atmosphere Properties and Weather Notes Chapter 11-13.

Weak Weak Strong Strong

No greater than 110 mph

110 mph – 200mph 200 mph +

Less than 2%

Page 44: Atmosphere Properties and Weather Notes Chapter 11-13.

Cyclones, Typhoons, Hurricanes???Cyclones, Typhoons, Hurricanes??? All the same thingAll the same thing

All need energy source All need energy source = warm tropical water= warm tropical water

Page 45: Atmosphere Properties and Weather Notes Chapter 11-13.

HurricanesHurricanes Tropical cyclones with winds that exceed Tropical cyclones with winds that exceed

64 knots (74 mi/hr) 64 knots (74 mi/hr) circulate counter-clockwise circulate counter-clockwise

Northern Hemisphere Northern Hemisphere Clockwise in the Clockwise in the

Southern Hemisphere Southern Hemisphere Water must be warmer than 81 FWater must be warmer than 81 F

Page 46: Atmosphere Properties and Weather Notes Chapter 11-13.

Stages of DevelopmentStages of Development

Depression Depression Storm Storm Hurricanes Hurricanes

Page 47: Atmosphere Properties and Weather Notes Chapter 11-13.

Extreme Weather Video ClipsExtreme Weather Video Clips

http://dsc.discovery.com/videos/wonders-of-http://dsc.discovery.com/videos/wonders-of-weather-extreme-weather.html (extreme weather-extreme-weather.html (extreme weather)weather)

http://dsc.discovery.com/videos/wonders-of-http://dsc.discovery.com/videos/wonders-of-weather-lightning-phenomena.html (lightning)weather-lightning-phenomena.html (lightning)

http://dsc.discovery.com/videos/storm-chasers-http://dsc.discovery.com/videos/storm-chasers-science-of-storm-chasing/ (storm chasers)science-of-storm-chasing/ (storm chasers)

Page 48: Atmosphere Properties and Weather Notes Chapter 11-13.

HurricanesHurricanes

http://planetgreen.discovery.com/videos/http://planetgreen.discovery.com/videos/focus-earth-hurricanes-and-climate-focus-earth-hurricanes-and-climate-change.html (climate and hurricanes)change.html (climate and hurricanes)

http://www.pbs.org/wgbh/nova/http://www.pbs.org/wgbh/nova/sciencenow/3204/02.html (hurricanes)--12 sciencenow/3204/02.html (hurricanes)--12 minmin