SlideShare uma empresa Scribd logo
1 de 3
Name: ____________________________             Date: ______________        Period: _____

OBJECTIVE: To discover how the atmosphere can be divided into layers based on
temperature changes at different heights, by making a graph.

BACKGROUND:
The atmosphere can be divided into four layers based on temperature variations. The
layer closest to the Earth is called the troposphere. Above this layer is the stratosphere,
followed by the mesosphere, then the thermosphere. The upper boundaries between these
layers are known as the tropopause, the stratopause, and the mesopause, respectively.
Temperature variations in the four layers are due to the way solar energy is absorbed as it
moves downward through the atmosphere. The Earth’s surface is the primary absorber of
solar energy and some of this energy is re-radiated by the Earth as heat, which warms the
overlying troposphere. The global average temperature in the troposphere rapidly
decreases with altitude until the tropopause, the boundary between the troposphere and
the stratosphere. The temperature begins to increase with altitude in the stratosphere.
This warming is caused by a form of oxygen called ozone, (O3). Ozone absorbs
ultraviolet radiation from the sun. Ozone protects us from most of the sun’s ultraviolet
radiation, which can cause cancer, genetic mutations, and sunburn. Scientists are
concerned that human activity is contributing to a decrease in stratospheric ozone. Nitric
oxide, which is the exhaust of high-flying jets, and chlorofluorocarbons (CFCs), which
are used as refrigerants, may contribute to ozone depletion. At the stratopause, the
temperature stops increasing with altitude. The overlying mesosphere does not absorb
solar radiation, so the temperature decreases with altitude. At the mesopause, the
temperature begins to increase with altitude, and this trend continues in the thermosphere.
Here solar radiation first hits the Earth’s atmosphere and heats it. Because the atmosphere
is so thin, a thermometer cannot measure the temperature accurately and special
instruments are needed.

DIRECTIONS:
   1. Table 1 contains the average temperature readings at various altitudes in the
      Earth’s atmosphere. Plot this data on the graph on the worksheet, and connect
      adjacent points with a smooth curve. Be careful to plot the negative temperature
      numbers correctly. This profile provides a general picture of temperature at any
      given time and place; however, the actual temperature may deviate from the
      average values, particularly in the lower atmosphere.
2. Label the different layers of the atmosphere and the separating boundaries between each layer.

3. Mark the general location of the ozone layer. You should place eight words on your graph in the correct
locations: troposphere, tropopause, stratosphere, stratopause, mesosphere, mesopause, thermosphere and
ozone layer.


QUESTIONS:
  1. What is the basis for dividing the atmosphere into four layers?




    2.   Does the temperature increase or decrease with altitude in the:
                 troposphere? _____________ stratosphere? ________________
                 mesosphere? _____________ thermosphere? _______________


    3.   What is the approximate height and temperature of the:

                 tropopause: _______________ _____________
                 stratopause: _______________ _____________
                 mesopause: _______________ _____________


    4.   What causes the temperature to increase with height through the stratosphere, and decrease with
         height through the mesosphere?




    5.
         What causes the temperature to decrease with height in the troposphere?
Atmosphere Activity

Mais conteúdo relacionado

Mais procurados

Air Atmosphere
Air AtmosphereAir Atmosphere
Air AtmosphereOshal Khan
 
layers of atmosphere
layers of atmospherelayers of atmosphere
layers of atmosphereManjeet Verma
 
Layers of the atmosphere
Layers of the atmosphereLayers of the atmosphere
Layers of the atmosphereRam Padigos
 
Atmosphere & Pollution
Atmosphere & PollutionAtmosphere & Pollution
Atmosphere & PollutionStephen Taylor
 
6.4 condensed characteristics atmosphere review
6.4 condensed characteristics atmosphere review6.4 condensed characteristics atmosphere review
6.4 condensed characteristics atmosphere reviewmojavehack
 
Layers of the atmosphere
Layers of the atmosphereLayers of the atmosphere
Layers of the atmosphereJaime Pena
 
Atmosphere environment.envi sci
Atmosphere environment.envi sciAtmosphere environment.envi sci
Atmosphere environment.envi scipydrex
 
Earth’s atmosphere
Earth’s  atmosphereEarth’s  atmosphere
Earth’s atmosphereitutor
 
Weather, Layers of the Atmosphere and Energy Transfer
Weather, Layers of the Atmosphere and Energy TransferWeather, Layers of the Atmosphere and Energy Transfer
Weather, Layers of the Atmosphere and Energy Transferrebelbrindley
 
The Layers of the Atmosphere
The Layers of the AtmosphereThe Layers of the Atmosphere
The Layers of the AtmosphereHayford Adjavor
 
layers of the earths atmosphere.ppt
layers of the earths atmosphere.pptlayers of the earths atmosphere.ppt
layers of the earths atmosphere.pptMarkChristianLapuz1
 
Earth’s atmosphere
Earth’s atmosphereEarth’s atmosphere
Earth’s atmosphereclarisseoria
 
Layers of the earth's atmosphere
Layers of the earth's atmosphereLayers of the earth's atmosphere
Layers of the earth's atmosphereSteven Heath
 

Mais procurados (20)

Air Atmosphere
Air AtmosphereAir Atmosphere
Air Atmosphere
 
layers of atmosphere
layers of atmospherelayers of atmosphere
layers of atmosphere
 
Atmosphere
AtmosphereAtmosphere
Atmosphere
 
Atomosphere
AtomosphereAtomosphere
Atomosphere
 
Layers of the atmosphere
Layers of the atmosphereLayers of the atmosphere
Layers of the atmosphere
 
Earth’s Atmosphere
Earth’s AtmosphereEarth’s Atmosphere
Earth’s Atmosphere
 
Atmosphere & Pollution
Atmosphere & PollutionAtmosphere & Pollution
Atmosphere & Pollution
 
6.4 condensed characteristics atmosphere review
6.4 condensed characteristics atmosphere review6.4 condensed characteristics atmosphere review
6.4 condensed characteristics atmosphere review
 
Layers of the atmosphere
Layers of the atmosphereLayers of the atmosphere
Layers of the atmosphere
 
Atmosphere environment.envi sci
Atmosphere environment.envi sciAtmosphere environment.envi sci
Atmosphere environment.envi sci
 
Earth’s atmosphere
Earth’s  atmosphereEarth’s  atmosphere
Earth’s atmosphere
 
Layers of the atmosphere
Layers of the atmosphereLayers of the atmosphere
Layers of the atmosphere
 
Weather, Layers of the Atmosphere and Energy Transfer
Weather, Layers of the Atmosphere and Energy TransferWeather, Layers of the Atmosphere and Energy Transfer
Weather, Layers of the Atmosphere and Energy Transfer
 
The Layers of the Atmosphere
The Layers of the AtmosphereThe Layers of the Atmosphere
The Layers of the Atmosphere
 
Atomosphere
AtomosphereAtomosphere
Atomosphere
 
layers of the earths atmosphere.ppt
layers of the earths atmosphere.pptlayers of the earths atmosphere.ppt
layers of the earths atmosphere.ppt
 
Earth’s atmosphere
Earth’s atmosphereEarth’s atmosphere
Earth’s atmosphere
 
solar_earth_atm.ppt
solar_earth_atm.pptsolar_earth_atm.ppt
solar_earth_atm.ppt
 
Atmosphere 1
Atmosphere 1Atmosphere 1
Atmosphere 1
 
Layers of the earth's atmosphere
Layers of the earth's atmosphereLayers of the earth's atmosphere
Layers of the earth's atmosphere
 

Semelhante a Atmosphere Activity

Semelhante a Atmosphere Activity (20)

Layers of Atmosphere WS Graph.pdf
Layers of Atmosphere WS Graph.pdfLayers of Atmosphere WS Graph.pdf
Layers of Atmosphere WS Graph.pdf
 
Unit 5
Unit 5Unit 5
Unit 5
 
The layers of the Atmosphere
The layers of the AtmosphereThe layers of the Atmosphere
The layers of the Atmosphere
 
The atmosphere
The atmosphereThe atmosphere
The atmosphere
 
Sim earth's atmosphere
Sim earth's atmosphereSim earth's atmosphere
Sim earth's atmosphere
 
layers of the earths atmosphere.ppt
layers of the earths atmosphere.pptlayers of the earths atmosphere.ppt
layers of the earths atmosphere.ppt
 
layers of the earths atmosphere.ppt slides for grade 9
layers of the earths atmosphere.ppt slides for grade 9layers of the earths atmosphere.ppt slides for grade 9
layers of the earths atmosphere.ppt slides for grade 9
 
layers of the earths atmosphere.ppt
layers of the earths atmosphere.pptlayers of the earths atmosphere.ppt
layers of the earths atmosphere.ppt
 
layers of the earths atmosphere.ppt
layers of the earths atmosphere.pptlayers of the earths atmosphere.ppt
layers of the earths atmosphere.ppt
 
Unit 5
Unit 5Unit 5
Unit 5
 
Atmosphere environment
Atmosphere environmentAtmosphere environment
Atmosphere environment
 
Unit 5. ATMOSPHERE: WEATHER AND CLIMATE
Unit 5. ATMOSPHERE: WEATHER AND CLIMATEUnit 5. ATMOSPHERE: WEATHER AND CLIMATE
Unit 5. ATMOSPHERE: WEATHER AND CLIMATE
 
ATMOSPHERE.ppt
ATMOSPHERE.pptATMOSPHERE.ppt
ATMOSPHERE.ppt
 
Unit 5
Unit 5Unit 5
Unit 5
 
ATMOSPHERE PPT.pptx
ATMOSPHERE PPT.pptxATMOSPHERE PPT.pptx
ATMOSPHERE PPT.pptx
 
composition &structure of atmosphere
composition &structure of atmospherecomposition &structure of atmosphere
composition &structure of atmosphere
 
Weather and Climate
Weather and ClimateWeather and Climate
Weather and Climate
 
Unit 5. Weather and climate
Unit 5. Weather and climateUnit 5. Weather and climate
Unit 5. Weather and climate
 
Module 5-ELS.pptx
Module 5-ELS.pptxModule 5-ELS.pptx
Module 5-ELS.pptx
 
Weather and climate
Weather and climateWeather and climate
Weather and climate
 

Mais de David Genis

Wc rage handbook
Wc rage handbookWc rage handbook
Wc rage handbookDavid Genis
 
Metric conversion house
Metric conversion houseMetric conversion house
Metric conversion houseDavid Genis
 
The everyday metric system
The everyday metric systemThe everyday metric system
The everyday metric systemDavid Genis
 
Experimental Design
Experimental DesignExperimental Design
Experimental DesignDavid Genis
 
Class policies and procedures
Class policies and proceduresClass policies and procedures
Class policies and proceduresDavid Genis
 
Class policies and procedures
Class policies and proceduresClass policies and procedures
Class policies and proceduresDavid Genis
 
Class policies and procedures
Class policies and proceduresClass policies and procedures
Class policies and proceduresDavid Genis
 
Class policies and procedures
Class policies and proceduresClass policies and procedures
Class policies and proceduresDavid Genis
 
Energy forms and_changes
Energy forms and_changesEnergy forms and_changes
Energy forms and_changesDavid Genis
 
0708 types of_energy
0708 types of_energy0708 types of_energy
0708 types of_energyDavid Genis
 
Cub simple lesson01_presentation
Cub simple lesson01_presentationCub simple lesson01_presentation
Cub simple lesson01_presentationDavid Genis
 

Mais de David Genis (20)

WCRage Handbook
WCRage HandbookWCRage Handbook
WCRage Handbook
 
Wc rage handbook
Wc rage handbookWc rage handbook
Wc rage handbook
 
Metric conversion house
Metric conversion houseMetric conversion house
Metric conversion house
 
The everyday metric system
The everyday metric systemThe everyday metric system
The everyday metric system
 
Experimental Design
Experimental DesignExperimental Design
Experimental Design
 
Class policies and procedures
Class policies and proceduresClass policies and procedures
Class policies and procedures
 
Class policies and procedures
Class policies and proceduresClass policies and procedures
Class policies and procedures
 
Class policies and procedures
Class policies and proceduresClass policies and procedures
Class policies and procedures
 
Class policies and procedures
Class policies and proceduresClass policies and procedures
Class policies and procedures
 
Work
WorkWork
Work
 
Electricity
ElectricityElectricity
Electricity
 
Energy forms and_changes
Energy forms and_changesEnergy forms and_changes
Energy forms and_changes
 
0708 types of_energy
0708 types of_energy0708 types of_energy
0708 types of_energy
 
Work
WorkWork
Work
 
Work
WorkWork
Work
 
Cub simple lesson01_presentation
Cub simple lesson01_presentationCub simple lesson01_presentation
Cub simple lesson01_presentation
 
Ttl7 09
Ttl7 09Ttl7 09
Ttl7 09
 
Lightning noaa
Lightning noaaLightning noaa
Lightning noaa
 
Presentation3
Presentation3Presentation3
Presentation3
 
Humidity
HumidityHumidity
Humidity
 

Atmosphere Activity

  • 1. Name: ____________________________ Date: ______________ Period: _____ OBJECTIVE: To discover how the atmosphere can be divided into layers based on temperature changes at different heights, by making a graph. BACKGROUND: The atmosphere can be divided into four layers based on temperature variations. The layer closest to the Earth is called the troposphere. Above this layer is the stratosphere, followed by the mesosphere, then the thermosphere. The upper boundaries between these layers are known as the tropopause, the stratopause, and the mesopause, respectively. Temperature variations in the four layers are due to the way solar energy is absorbed as it moves downward through the atmosphere. The Earth’s surface is the primary absorber of solar energy and some of this energy is re-radiated by the Earth as heat, which warms the overlying troposphere. The global average temperature in the troposphere rapidly decreases with altitude until the tropopause, the boundary between the troposphere and the stratosphere. The temperature begins to increase with altitude in the stratosphere. This warming is caused by a form of oxygen called ozone, (O3). Ozone absorbs ultraviolet radiation from the sun. Ozone protects us from most of the sun’s ultraviolet radiation, which can cause cancer, genetic mutations, and sunburn. Scientists are concerned that human activity is contributing to a decrease in stratospheric ozone. Nitric oxide, which is the exhaust of high-flying jets, and chlorofluorocarbons (CFCs), which are used as refrigerants, may contribute to ozone depletion. At the stratopause, the temperature stops increasing with altitude. The overlying mesosphere does not absorb solar radiation, so the temperature decreases with altitude. At the mesopause, the temperature begins to increase with altitude, and this trend continues in the thermosphere. Here solar radiation first hits the Earth’s atmosphere and heats it. Because the atmosphere is so thin, a thermometer cannot measure the temperature accurately and special instruments are needed. DIRECTIONS: 1. Table 1 contains the average temperature readings at various altitudes in the Earth’s atmosphere. Plot this data on the graph on the worksheet, and connect adjacent points with a smooth curve. Be careful to plot the negative temperature numbers correctly. This profile provides a general picture of temperature at any given time and place; however, the actual temperature may deviate from the average values, particularly in the lower atmosphere.
  • 2. 2. Label the different layers of the atmosphere and the separating boundaries between each layer. 3. Mark the general location of the ozone layer. You should place eight words on your graph in the correct locations: troposphere, tropopause, stratosphere, stratopause, mesosphere, mesopause, thermosphere and ozone layer. QUESTIONS: 1. What is the basis for dividing the atmosphere into four layers? 2. Does the temperature increase or decrease with altitude in the: troposphere? _____________ stratosphere? ________________ mesosphere? _____________ thermosphere? _______________ 3. What is the approximate height and temperature of the: tropopause: _______________ _____________ stratopause: _______________ _____________ mesopause: _______________ _____________ 4. What causes the temperature to increase with height through the stratosphere, and decrease with height through the mesosphere? 5. What causes the temperature to decrease with height in the troposphere?