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CLIMATES OF THE EARTH CHAPTER 3
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CLIMATES OF THE EARTH CHAPTER 3. CHAPTER 3, SECTION 1: EARTH-SUN RELATIONSHIPS CLIMATE AND WEATHER EARTH’S TILT AND ROTATION EARTH’S REVOLUTION THE GREENHOUSE.

Dec 29, 2015

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Page 1: CLIMATES OF THE EARTH CHAPTER 3. CHAPTER 3, SECTION 1: EARTH-SUN RELATIONSHIPS CLIMATE AND WEATHER EARTH’S TILT AND ROTATION EARTH’S REVOLUTION THE GREENHOUSE.

CLIMATES OF THE EARTHCHAPTER 3

Page 2: CLIMATES OF THE EARTH CHAPTER 3. CHAPTER 3, SECTION 1: EARTH-SUN RELATIONSHIPS CLIMATE AND WEATHER EARTH’S TILT AND ROTATION EARTH’S REVOLUTION THE GREENHOUSE.

CHAPTER 3, SECTION 1: EARTH-SUN RELATIONSHIPS

• CLIMATE AND WEATHER

• EARTH’S TILT AND ROTATION

• EARTH’S REVOLUTION

• THE GREENHOUSE EFFECT

Page 3: CLIMATES OF THE EARTH CHAPTER 3. CHAPTER 3, SECTION 1: EARTH-SUN RELATIONSHIPS CLIMATE AND WEATHER EARTH’S TILT AND ROTATION EARTH’S REVOLUTION THE GREENHOUSE.

CLIMATE AND WEATHER

• WEATHER = THE CONDITION OF THE ATMOSPHERE IN ONE PLACE DURING A LIMITED PERIOD OF TIME

• CLIMATE = THE TERM FOR THE WEATHER PATTERNS THAT AN AREA TYPICALLY OVER A LONG PERIOD OF TIME

• SEATTLE HAS A RAINY, WET CLIMATE. THE WEATHER IN SEATTLE IS DAY-BY-DAY. TODAY THERE IS A 70% CHANCE OF RAIN WITH A HIGH TEMPERATURE OF 72 DEGREES FAHRENHEIT

Page 4: CLIMATES OF THE EARTH CHAPTER 3. CHAPTER 3, SECTION 1: EARTH-SUN RELATIONSHIPS CLIMATE AND WEATHER EARTH’S TILT AND ROTATION EARTH’S REVOLUTION THE GREENHOUSE.

EARTH’S TILT AND ROTATION

• EARTH’S AXIS = AN IMAGINARY LINE RUNNING FROM THE NORTH POLE TO THE SOUTH POLE THROUGH THE PLANET’S CENTER.

• EARTH’S AXIS IS CURRENTLY TILTED AT AN ANGLE OF ABOUT 23.5 DEGREES

THIS AFFECTS TEMPERATURE, THE MEASURE OF HOW HOT OR COLD A PLACE IS.

Page 5: CLIMATES OF THE EARTH CHAPTER 3. CHAPTER 3, SECTION 1: EARTH-SUN RELATIONSHIPS CLIMATE AND WEATHER EARTH’S TILT AND ROTATION EARTH’S REVOLUTION THE GREENHOUSE.

TROPICS OF CANCER AND CAPRICORN

Page 6: CLIMATES OF THE EARTH CHAPTER 3. CHAPTER 3, SECTION 1: EARTH-SUN RELATIONSHIPS CLIMATE AND WEATHER EARTH’S TILT AND ROTATION EARTH’S REVOLUTION THE GREENHOUSE.

EARTH’S ROTATION

SPACESHIP EARTH• EARTH’S TILT ALWAYS STAYS THE SAME. THIS IS WHY WE HAVE SEASONS (SUMMER AND

WINTER)

• SEASONS ARE MOST DRAMATIC AT THE POLES

• REVOLUTION: ONE TRIP AROUND THE SUN (365 DAYS)

• EQUINOX = WHEN THE SUN’S RAYS FALL DIRECTLY ON THE EQUATOR

• ~MARCH 20

• ~SEPTEMBER 22

• SOLSTICE = WHEN THE SUN’S RAYS FALL ON EITHER THE TROPIC OF CANCER OF THE TROPIC OF CAPRICORN

• ~DECEMBER 21

• ~JUNE 21

Page 7: CLIMATES OF THE EARTH CHAPTER 3. CHAPTER 3, SECTION 1: EARTH-SUN RELATIONSHIPS CLIMATE AND WEATHER EARTH’S TILT AND ROTATION EARTH’S REVOLUTION THE GREENHOUSE.

THE GREENHOUSE EFFECT

Page 8: CLIMATES OF THE EARTH CHAPTER 3. CHAPTER 3, SECTION 1: EARTH-SUN RELATIONSHIPS CLIMATE AND WEATHER EARTH’S TILT AND ROTATION EARTH’S REVOLUTION THE GREENHOUSE.

CHAPTER 3, SECTION 2: FACTORS AFFECTING CLIMATE

• LOW/MID/HIGH LATITUDES

• ELEVATION

• WINDS AND OCEAN CURRENTS

• WIND PATTERNS

• OCEAN LATITUDES

• OCEAN CURRENTS

• EL NIÑO

• LANDFORMS AND CLIMATE

Page 9: CLIMATES OF THE EARTH CHAPTER 3. CHAPTER 3, SECTION 1: EARTH-SUN RELATIONSHIPS CLIMATE AND WEATHER EARTH’S TILT AND ROTATION EARTH’S REVOLUTION THE GREENHOUSE.

LOW/MID/HIGH LATITUDES

High Latitude

Mid Latitude

Low Latitude

Mid Latitude

High Latitude

Page 10: CLIMATES OF THE EARTH CHAPTER 3. CHAPTER 3, SECTION 1: EARTH-SUN RELATIONSHIPS CLIMATE AND WEATHER EARTH’S TILT AND ROTATION EARTH’S REVOLUTION THE GREENHOUSE.

ELEVATION

• ELEVATION = THE HEIGHT ABOVE THE LEVEL OF THE SEA

• THE HIGHER THE ELEVATION, THE THINNER THE AIR (MORE OXYGEN IS PRESENT AT SEA LEVEL).

• THINNER AIR RETAINS LESS HEAT. THAT IS WHY AIRPLANE WINDOWS ARE COLD DURING FLIGHT.

Page 11: CLIMATES OF THE EARTH CHAPTER 3. CHAPTER 3, SECTION 1: EARTH-SUN RELATIONSHIPS CLIMATE AND WEATHER EARTH’S TILT AND ROTATION EARTH’S REVOLUTION THE GREENHOUSE.

WIND PATTERNS

• GLOBAL WINDS BLOW IN FAIRLY CONSTANT PATTERNS CALLED PREVAILING WINDS

• DOLDRUMS ARE THE GENERALLY WINDLESS BANDS, ALSO CALLED HORSE LATITUDES

Doldrums

Page 12: CLIMATES OF THE EARTH CHAPTER 3. CHAPTER 3, SECTION 1: EARTH-SUN RELATIONSHIPS CLIMATE AND WEATHER EARTH’S TILT AND ROTATION EARTH’S REVOLUTION THE GREENHOUSE.

OCEAN CURRENTS• JUST AS WINDS MOVE IN PATTERNS, SO DO COLD AND WARM STREAMS OF

WATER. THESE ARE CALLED CURRENTS

• JUST LIKE THE WINDS, CURRENTS ARE CAUSED BY EARTH’S ROTATION, AIR PRESSURE, AND WATER TEMPERATURE

• EAST AUSTRALIAN CURRENT

Page 13: CLIMATES OF THE EARTH CHAPTER 3. CHAPTER 3, SECTION 1: EARTH-SUN RELATIONSHIPS CLIMATE AND WEATHER EARTH’S TILT AND ROTATION EARTH’S REVOLUTION THE GREENHOUSE.

EL NIÑO• EL NIÑO = THE PERIODIC CHANGE IN THE PATTERN OF OCEAN CURRENTS, WATER

TEMPERATURES, AND WEATHER IN THE MID-PACIFIC REGION

• IT DOESN’T HAPPEN EVERY YEAR, BUT HAS BEEN HAPPENING MORE FREQUENTLY SINCE THE 70’S

• WARM WATER FROM AUSTRALIA TO NORTH/SOUTH AMERICA

• MORE RAIN THROUGH NORTH/SOUTH AMERICA

• SCIENTISTS ARE NOT SURE WHY THIS HAPPENS, OR WHY IT IS HAPPENING MORE FREQUENTLY

Page 14: CLIMATES OF THE EARTH CHAPTER 3. CHAPTER 3, SECTION 1: EARTH-SUN RELATIONSHIPS CLIMATE AND WEATHER EARTH’S TILT AND ROTATION EARTH’S REVOLUTION THE GREENHOUSE.

LANDFORMS AND CLIMATE: THE RAIN SHADOW EFFECT

Windward side = side of the mountainfacing the wind Leeward side = warmer, drier side

of the mountain

Page 15: CLIMATES OF THE EARTH CHAPTER 3. CHAPTER 3, SECTION 1: EARTH-SUN RELATIONSHIPS CLIMATE AND WEATHER EARTH’S TILT AND ROTATION EARTH’S REVOLUTION THE GREENHOUSE.

CHAPTER 3, SECTION 3: WORLD CLIMATE PATTERS

• CLIMATE REGIONS

• TROPICAL CLIMATES

• DRY CLIMATES

• MIDLATITUDE CLIMATES

• HIGH-LATITUDE CLIMATES

• HIGHLAND CLIMATES

• CLIMATE CHANGES

Page 16: CLIMATES OF THE EARTH CHAPTER 3. CHAPTER 3, SECTION 1: EARTH-SUN RELATIONSHIPS CLIMATE AND WEATHER EARTH’S TILT AND ROTATION EARTH’S REVOLUTION THE GREENHOUSE.

TROPICAL CLIMATES

• FOUND IN OR NEAR THE TROPICS (LOW LATITUDES)

• HOW AND WET THROUGHOUT THE YEAR (VERY HUMID)

• TROPICAL RAINFORESTS

Page 17: CLIMATES OF THE EARTH CHAPTER 3. CHAPTER 3, SECTION 1: EARTH-SUN RELATIONSHIPS CLIMATE AND WEATHER EARTH’S TILT AND ROTATION EARTH’S REVOLUTION THE GREENHOUSE.

DRY CLIMATES

• DRY AREAS WITH SPARSE PLANT LIFE

• SCRUBS AND CACTUS

• HOT BY DAY, COLD BY NIGHT

• DESSERTS

Page 18: CLIMATES OF THE EARTH CHAPTER 3. CHAPTER 3, SECTION 1: EARTH-SUN RELATIONSHIPS CLIMATE AND WEATHER EARTH’S TILT AND ROTATION EARTH’S REVOLUTION THE GREENHOUSE.

MIDLATITUDE CLIMATES

• EXPERIENCE VARIABLE WEATHER PATTERNS AND SEASONAL CHANGES

• USUALLY AN ABUNDANCE OF RAINFALL WITH A VARIETY OF NATURAL VEGETATION

• THINK OF THE DIFFERENT CLIMATES FOUND ACROSS THE UNITED STATES

Page 19: CLIMATES OF THE EARTH CHAPTER 3. CHAPTER 3, SECTION 1: EARTH-SUN RELATIONSHIPS CLIMATE AND WEATHER EARTH’S TILT AND ROTATION EARTH’S REVOLUTION THE GREENHOUSE.

HIGH-LATITUDE CLIMATES

• FREEZING TEMPERATURES ARE COMMON THROUGHOUT THE YEAR

• IN THE WINTERS, SUN LIGHT IS MINIMAL TO NON-EXISTENT

• PERMAFROST = PERMANENTLY FROZEN SUBSOIL

Page 20: CLIMATES OF THE EARTH CHAPTER 3. CHAPTER 3, SECTION 1: EARTH-SUN RELATIONSHIPS CLIMATE AND WEATHER EARTH’S TILT AND ROTATION EARTH’S REVOLUTION THE GREENHOUSE.

HIGHLAND CLIMATES

• HIGH MOUNTAIN AREAS, EVEN ALONG THE EQUATOR

• COOLER TEMPERATURES, THINNER AIR

• THE HIGHER THE ELEVATION, THE LESS VEGETATION

Page 21: CLIMATES OF THE EARTH CHAPTER 3. CHAPTER 3, SECTION 1: EARTH-SUN RELATIONSHIPS CLIMATE AND WEATHER EARTH’S TILT AND ROTATION EARTH’S REVOLUTION THE GREENHOUSE.

CLIMATE CHANGES

• CLIMATES GRADUALLY CHANGE OVER TIME, THOUGH THE CAUSES ARE UNCLEAR

• DURING THE LAST 1 TO 2 MILLION YEARS, EARTH HAS EXPERIENCED 4 ICE AGES

• HUMAN INTERACTION WITH THE ENVIRONMENT ALSO AFFECTS CLIMATE

• BURNING FOSSIL FUELS AND POLLUTION HAVE A NEGATIVE IMPACT ON THE PLANET