climate and vegetation chapter 3. the sun and the earth

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Climate and Vegetation CHAPTER 3

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Page 1: Climate and Vegetation CHAPTER 3. THE SUN AND THE EARTH

Climate and Vegetation

CHAPTER 3

Page 2: Climate and Vegetation CHAPTER 3. THE SUN AND THE EARTH

THE SUN AND THE EARTH

Page 3: Climate and Vegetation CHAPTER 3. THE SUN AND THE EARTH

ROTATION AND REVOLUTION

HOW OFTEN DOES THE EARTH ROTATE?

EVERY 24 HOURSHOW OFTEN DOES THE EARTH REVOLVE AROUND THE SUN?

EVERY 365 AND ¼ DAYS

Page 4: Climate and Vegetation CHAPTER 3. THE SUN AND THE EARTH

Because the earth is tilted on its axis, different parts of the globe receive different direct

rays of the sun during different times of the year.

Page 5: Climate and Vegetation CHAPTER 3. THE SUN AND THE EARTH

EARTH’S REVOLUTION AND EARTH’S REVOLUTION AND SEASONSSEASONS

Page 6: Climate and Vegetation CHAPTER 3. THE SUN AND THE EARTH

http://streaming.factsonfile.com/play/PYT7H5

Page 7: Climate and Vegetation CHAPTER 3. THE SUN AND THE EARTH

The Solstice and the Equinox

TURN TO PAGE 49 IN YOUR TEXTBOOKS.

When are the winter and summer solstices?

What happens on these days?

When are the spring and fall equinoxes?

What happens on these days?

Page 8: Climate and Vegetation CHAPTER 3. THE SUN AND THE EARTH

Solstice and Equinox Importance

Ancient calendars were

set by calculating the

solstice and equinox.

Planting, harvesting,

and storing for the

winter were planned

by using the calculations.

Page 9: Climate and Vegetation CHAPTER 3. THE SUN AND THE EARTH

What is the difference between climate and weather?

Weather is the temperature and precipitation of a

certain place at a certain time---a snapshot!

Page 10: Climate and Vegetation CHAPTER 3. THE SUN AND THE EARTH

Climate includes weather conditions (temperature and

precipitation over a long period of time)—like a movie!

Page 11: Climate and Vegetation CHAPTER 3. THE SUN AND THE EARTH

TYPES OF PRECIPITATION

CONVECTIONAL

OROGRAPHIC

FRONTAL

Page 12: Climate and Vegetation CHAPTER 3. THE SUN AND THE EARTH

CONVECTIONALPRECIPITATION

CONVECTIONAL HEATINGOCCURS IN THE TROPICSAND THE RAIN FOREST WHERE THE HUMIDITY IS HIGH

Page 13: Climate and Vegetation CHAPTER 3. THE SUN AND THE EARTH

OROGRAPHIC PRECIPITATION

OROGRAPHIC PRECIPITATIONOCCURS WHERE THEREARE MOUNTAINS THAT BLOCKTHE RAIN SHOWERS

Page 14: Climate and Vegetation CHAPTER 3. THE SUN AND THE EARTH

FRONTAL PRECIPITATION

FRONTAL PRECIPITATIONOCCURS WHEN

TWO LARGEAIR MASSES

(COLD AND WARM FRONTS) COLLIDE

Page 15: Climate and Vegetation CHAPTER 3. THE SUN AND THE EARTH

WEATHER EXTREMES

Define the following in your notes:

hurricanes

typhoons

tornados

blizzards

drought

Where is “Tornado Alley?”

Page 16: Climate and Vegetation CHAPTER 3. THE SUN AND THE EARTH

CLIMATE FACTORSTemperature and Precipitation depend upon the following

factors:

1. ELEVATION2. LATITUDE3. LOCATION TO LANDFORMS4. NEARNESS TO BODIES OF

WATER5. WINDS

Page 17: Climate and Vegetation CHAPTER 3. THE SUN AND THE EARTH
Page 18: Climate and Vegetation CHAPTER 3. THE SUN AND THE EARTH

As the elevation increases,

TEMPERATURE DECREASES

ANDPRECIPITATION

DECREASES

Page 19: Climate and Vegetation CHAPTER 3. THE SUN AND THE EARTH

LATITUDE

THE FARTHER WE MOVE AWAY FROM THE EQUATOR,

THE MORE THE TEMPERATURE AND

PRECIPITATION DECREASE.

Page 20: Climate and Vegetation CHAPTER 3. THE SUN AND THE EARTH

CLIMATE ZONES

Polar zone

Temperate zone

Tropical zone

Temperate zone

Polar zone

Page 21: Climate and Vegetation CHAPTER 3. THE SUN AND THE EARTH

LATITUDESTROPICAL ZONES

LOW LATITUDES 0- 23 DEGREES

TEMPERATE ZONESMID LATITUDES

24-66 DEGREES

POLAR ZONES HIGH LATITUDES

67-90 DEGREES

Page 22: Climate and Vegetation CHAPTER 3. THE SUN AND THE EARTH

LOCATION TO LANDFORMSMOUNTAINS CAN AFFECT CLIMATE, BECAUSE

PRECIPITATION IS SCARCE AS ELEVATION INCREASES. AREAS ON THE DRY SIDE OF THE MOUNTAIN ARE IN THE RAIN SHADOW.

Page 23: Climate and Vegetation CHAPTER 3. THE SUN AND THE EARTH

DRAW A DIAGRAM OF A MOUNTAIN AND LABEL THE

FOLLOWING:

WINDWARD

LEEWARD

RAIN SHADOW

Page 24: Climate and Vegetation CHAPTER 3. THE SUN AND THE EARTH

WIND CURRENTS

The transfer of heat around the globe happens because of

CONVECTION.

Ocean currents and wind currents move the heat from place to place.

Page 25: Climate and Vegetation CHAPTER 3. THE SUN AND THE EARTH

NOTICEHOW WARM

WATER FLOWS

FROM THETROPICS TO THE

COLDEROCEAN AREAS

Page 26: Climate and Vegetation CHAPTER 3. THE SUN AND THE EARTH
Page 27: Climate and Vegetation CHAPTER 3. THE SUN AND THE EARTH

Look on page 54. What is the CORIOLIS EFFECT?

IF YOU ARE BLINDFOLDED AND TRY TO WALK IN A STRAIGHT LINE….

IN THE NORTHERN HEMISPHERE, YOURSTRAIGHT LINE WILL BEGIN TO CURVEIN A CLOCKWISE CIRCLE.

IN THE SOUTHERN HEMISPHERE, YOURSTRAIGHT LINE WILL BEGIN TO CURVE IN A COUNTER-CLOCKWISE CIRCLE.

Page 28: Climate and Vegetation CHAPTER 3. THE SUN AND THE EARTH

And now, a word from “El Nino::

Page 29: Climate and Vegetation CHAPTER 3. THE SUN AND THE EARTH
Page 30: Climate and Vegetation CHAPTER 3. THE SUN AND THE EARTH

CHANGES IN CLIMATE

What is El Nino, really?

What is the Greenhouse Effect?

What is global Warming?

Page 31: Climate and Vegetation CHAPTER 3. THE SUN AND THE EARTH

THE GREENHOUSE EFFECT