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ATMOSPHERE

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INTENSITY OF INSOLATION VARIES WITH TIME OF DAY, ... HIGH ALTITUDES, LOWER ANGLES, LESS INSOLATION ... CLOUDS REFLECT A SIGNIFICANT AMOUNT OF INSOLATION ... – PowerPoint PPT presentation

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Title: ATMOSPHERE


1
ATMOSPHERE
  • CHAPTER 17

2
COMPOSITION OF THE ATMOSPHERE
  • VOLCANIC ERUPTIONS PLAYED A ROLE FORMING EARTHS
    EARLY ATMOSPHERE
  • GASES RELEASED INCLUDED CO2 SO2 WATER VAPOR, AND
    N2

3
ATMOSPHERE
  • TODAY THE LOWER ATMOSPHERE IS A MIXTURE OF MANY
    GASES CALLED AIR!
  • THE PERCENTAGES OF THESES GASES ARE FAIRLY
    CONSTANT TO AN ALTITUDE OF 80KM (50 miles)

4
ATMOSPHERE
  • THE AMOUNTS OF N AND O ARE FAIRLY CONSTANT
  • WATER VAPOR VARIES WITH SEASON, LOCATION, AND
    TIME OF DAY
  • CARBON DIOXIDE VARIES WITH THE TIME OF YEAR
    LOWEST IN SUMMER AND HIGHEST IN WINTER
  • PLUS LOTS OF DUST, POLLEN, SALT

5
RECYCLE!!
  • THE ATMOSPHERE HAS REMAINED STABLE BECAUSE OF THE
    RECYCLING OF MATERIALS IN AND OUT OF THE
    GEOSPHERE, HYDROSPHERE, AND BIOSPHERE

O2, H2O
CO2 H2O
6
DELICATE BALANCE
  • AN INCONVIENENT TRUTH??????
  • THE AMOUNT OF CARBON DIOXIDE LEVELS HAVE
    INCREASED
  • NATURAL INCREASE OR MAN MADE??

7
HEAT TRANSFER
  • HEAT ENERGY MOVES BY
  • ______________
  • ______________
  • ______________
  • IN THE ATMOSPHERE

8
STRUCTURE OF THE ATMOSPHERE
  • __________________________________________________
    _
  • __________________________________
  • __________________________________
  • __________________________________

9
TROPOSPHERE
  • ______________________________________
  • MOST DENSE
  • TEMPS DECREASE WITH ALTITUDE
  • MOST OF THE SUNS RADIATION IS ABSORBED BY THE
    SURFACE OF THE EARTH AND TRANSFERRED TO THIS
    LAYER
  • CONTAINS 80 OF THE TOTAL MASS OF THE ATMOSPHERE
  • CONTAINS MOST OF THE WATER VAPOR
  • MOST OF THE WEATHER OCCURS IN THIS LAYER

10
TROPOPAUSE
  • LAYER BETWEEN THE TROPOSPHERE AND STRATOSPHERE
  • TEMPS INCREASE HERE
  • __________________________________________________
    __________________

11
STRATOSPHERE
  • __________________________________________________
    __________________________________________________
    __
  • OZONE LAYER IS LOCATED HERE
  • TEMP INCREASE IS CAUSED BY THE OZONE LAYER WHICH
    ABSORBS UV RAYS FROM THE SUN AND RELEASES HEAT

12
STRATOPAUSE
  • LAYER BETWEEN THE STRATOSPHERE AND THE MESOSPHERE
  • __________________________________________________
    __________

13
MESOSPHERE
  • ________________________________________________

14
THERMOSPHERE
  • ATMOSPHERE IS EXTREMELY THIN
  • MOLECULES AND ATOMS RECEIVE SUCH INTENSE SOLAR
    RADIATION THAT TEMPS CAN RISE TO ABOVE
    _____________
  • HEAVIER GASES IN THE LOWER LAYERS MOSTLY
    ______________
  • LAYER OF _________ REACHES TO 1,000KM
  • ABOVE THAT A LAYER OF ______ REACHES TO 2,400KM
  • ABOVE THAT A LAYER OF ______________ THINS OUT TO
    SPACE

15
IONOSPHERE
  • LOCATED IN THE THERMOSPHERE
  • BETWEEN 90 AND 500 KM ABOVE THE EARTH
  • __________________________________________________
    __________________________________________________
    ____________________________________
  • AFFECTED BY SOLAR EVENTS
  • REFLECTS RADIO WAVES

16
AURORAS
  • HUGE ERUPTIONS FROM SUNSPOTS SEND OUT LARGE
    AMOUNTS OF RADIATION THAT DISRUPTS RADIO
    COMMUNICATIONS
  • ALSO SENDS OUT IONIZED PARTICLES THAT ARE
    ELECTRICALLY CHARGED
  • THEY ARE DEFLECTED BY THE MAGNETIC FIELD AROUND
    THE EARTH TO THE NORTH AND SOUTH POLES
  • THE IONIZED PARTICLES INTERACT WITH THE AIR
    MOLECULES TO FORM AURORAS, THE COLORFUL PATTERNS
    OF LIGHT IN THE NIGHT SKY
  • EACH POLE DISPLAYS THE SAME PATTERN AT THE SAME
    TIME MIRROR IMAGES

17
EARTHS ATMOSPHERE
  • __________________________________________________
    __________________________________________________
    __
  • HALF OF THAT IS WITHIN 5.5 KM (3.4miles) OF THE
    EARTHS SURFACE

18
OZONE
  • A FORM OF OXYGEN GAS
  • O3 MOLECULE
  • FORMS WHEN UV RAYS HIT OXYGEN IN THE UPPER
    ATMOSPHERE
  • __________________________________
  • THINING OF THE OZONE IS CAUSED BY THE RELEASE OF
    CFCS AND BY THE TEMPERATURE OF THE EARTHS
    SURFACE

19
OZONE
  • THE OZONE LAYER IS NATURALLY THINNER ABOVE THE
    POLES
  • THE THICKNESS OF THE OZONE LAYER CHANGES WITH THE
    SEASONS

20
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21
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22
INSOLATION
  • ________________________
  • ________________________
  • ________________________
  • EARTH RECEIVES ONLY 1/ 2 BILLIONTH OF THE SUNS
    INCOMING RAYS
  • BALANCE INCOMING AND OUTGOING RADIATION IS
    ABOUT EQUAL
  • JUST AS MUCH ENERGY ENTERS THE EARTH AS LEAVES IT

23
GREENHOUSE EFFECT
  • CREATED BY GREENHOUSE GASES
  • ___________________ IS THE BIGGEST GREENHOUSE GAS
    IN THE ATMOSPHERE
  • ______________________ IS ANOTHER GREENHOUSE GAS

24
TEMPERATURE VARIATIONS
  • INTENSITY OF INSOLATION VARIES WITH TIME OF DAY,
    LATITUDE, AND TIME OF YEAR
  • GROUND COVERS AFFECTS THE ABSORBTION OF RADIATION

25
ANGLE OF INSOLATION
  • DEPENDS ON THE ANGLE OF THE SUNS RAYS ON THE
    EARTH
  • AT 90 DEGREES GREATEST AMOUNTS OF ABSORBTION OF
    RADIATION
  • AS THE ANGLE DECREASES THE AMOUNT OF ENERGY
    ABSORBED DECREASES
  • THE SUNS ENERGY IS SPREAD OVER A LARGER AREA
    THUS THE DECREASE IN INTENSITY OF ABSORBTION

26
ANGLE OF INSOLATION
  • SEASONAL
  • THROUGH OUT THE SEASONS THE ANGLE OF THE SUN
    CHANGES THUS THE INTENSITY OF THE INSOLATION
    CHANGES
  • HOTTEST MONTH FOR THE NORTHERN LATITUDES
    AUGUST, A COUPLE OF MONTHS AFTER THE SUN IS AT
    ITS HIGHEST POINT
  • 24 HOUR PERIOD
  • THROUGHOUT THE DAY THE ANGLE OF THE SUN CHANGES
    AND THUS CHANGES THE INTENSITY OF THE INSOLATION
  • HOTTEST TIME OF DAY A FEW HOURS AFTER THE SUN
    IS AT ITS HIGHEST POINT IN THE SKY

27
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28
LATITUDE AND TIME OF YEAR
  • HIGH ALTITUDES, LOWER ANGLES, LESS INSOLATION
  • TILT OF THE EARTH RELATIVE TO THE SUN EFFECTS
    INSOLATION
  • __________________________________________________
    ______________________
  • __________________________________________________
    ______________________

29
CLOUD COVER
  • THE AMOUNT OF ENERGY THAT REACHES THE EARTH ALSO
    DEPENDS ON THE CLOUD COVER
  • CLOUDS REFLECT A SIGNIFICANT AMOUNT OF INSOLATION
  • THEY ALSO HOLD IN A SIGNIFICANT AMOUNT OF
    INSOLATION
  • THE YEAR WITHOUT A SUMMER? CAUSED BY?????

30
HEATING OF LAND AND WATER
  • LAND HEATS FASTER THAN WATER
  • LAND COOLS FASTER THAN WATER
  • CONTINENTS ARE WARMER THAN NEARBY OCEANS IN
    SUMMER
  • CONTINENTS ARE COOLER THATN NEARBY OCEANS IN THE
    WINTER
  • WATER NEEDS MORE ENERGY TO RAISE ITS TEMP
  • SPECIFIC HEAT OF WATER IS 3 TIMES THE SPECIFIC
    HEAT OF LAND

31
ISOTHERMS
  • __________________________________________________
    __________________________________________________
    __
  • TEMPS ARE ADJUSTED TO ELIMINATE THE EFFECT OF
    ALTITUDE
  • ACTIVITY A ISOTHERMS
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