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WORLD CLIMATES

World climates

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characteristics of the world climates

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Page 1: World climates

WORLD CLIMATES

Page 2: World climates

WEATHER AND CLIMATE

• Weather is the atmospheric conditions here and now.

• Climate is an average of conditions in a particular place over time

Page 3: World climates

A COUNTRY’S CLIMATE DEPENDS ON FOUR MAIN FACTORS

• Latitude is the distance of a location from the equator. The hottest temperatures are found at the equator. As you move further away from the equator towards the polar regions, less and less sun is received during the year and the climates become colder and colder.

Altitude is the height above sea level or the height above the earth's surface. The higher the altitude, the lower the temperature will be. On average for every 1,000 metres higher you go the temperature will fall about 6.5 °C.

Proximity to the sea affects the temperature of a place because the sea temperature changes slower than land temperature. So the sea will keep coastal areas warmer than inland area during the winter and cooler than inland areas during the summer.

• Currents exist in all the oceans. Currents that move water from tropical areas towards the poles (North Atlantic Drift starts in the Gulf of Mexico) are known as warm currents. Those currents moving from northern (or southern) colder seas, nearer the poles towards the equator are known as cool currents, an example is the Canaries current

Page 4: World climates

CLIMATE ELEMENTS

• Temperature is how hot or cold the atmosphere is - ie, how many degrees Celsius (centigrade) it is above or below freezing (0°C)

• farenheit and celsius scale

Page 5: World climates

• Precipitation is the term given to moisture that falls from the air to the ground

• pluviometer

Page 6: World climates

• Atmospheric pressure (or air pressure) is the weight of air resting on the earth's surface. Pressure is shown on a weather map, often called a synoptic map, with lines called isobars.

• Low pressure occurs when air becomes warmer. The air molecules expand, become lighter and it rises.

• High pressure occurs when air becomes colder. The air molecules contract, become denser, heavier and sink towards the earth.

Page 7: World climates

barometer

Page 8: World climates

• Wind is the movement of air masses from high pressure areas (high) to low pressure areas (low). The effect of this movement of air is to rebalance the pressure in the atmosphere.

Page 9: World climates

MAIN CLIMATIC ZONES

Page 10: World climates

WORLD CLIMATE ZONES AND BIOMES

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World climatesKoeppen’s classification

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TROPICAL ZONE

Page 13: World climates

EQUATORIAL CLIMATE

• Characteristics• Constant high

temperatures. • Lowest annual

temperature range of any climate.

• Evenly distributed, heavy precipitation.

• Lots of cloud cover and high humidity

Page 14: World climates

Rainforest Biome

• Biome: A biome is a large geographical area of distinctive plant and animal groups, which are adapted to that particular environment

Page 15: World climates

Tropical dry-wet

• Characteristics• wet season in

summer,dry periods in winter.

• Rainfall less than equatorial and monsoon.

• Highest temperature ranges of low latitude wet climates

Page 16: World climates

Savanna Biome

Page 17: World climates

Monsoon

• Characteristics • Heavy rain season;

short dry season. • Highest temperature

just before rainy period.

Page 18: World climates

Desert

• Characteristics• Among the driest places on

earth • Low relative humidity • Irregular rainfall • Highest percentage of

sunshine of any climate • Large daytime temperature

range • Highest daytime temperature

of any climate • Annual precipitation less than 250 mm

Page 19: World climates

Desert Biome

Page 20: World climates

TEMPERATE ZONE

Page 21: World climates

Humid subtropical

• Characteristics• High humidity; summers

like humid tropics. • Frost with polar air

masses in winter. • 1000 to 2000 mm of year

precipitation, decreasing inland.

• Monsoon influence in Asia

Page 22: World climates

Mediterranean

• Characteristics

• Mild, moist winters, • Dry summers• High percentage of

sunshine

Page 23: World climates

Chaparral biome

Page 24: World climates

Humid continental• Characteristics• Warm Summer Subtype:• Hot humid summers; occasional

winter cold waves. • Large annual temperature ranges.

Ie. Chicago • Cool Summer Subtype:• Moderate summers; long cold

winters. • Large annual temperature ranges. • Less precipitation than warm

summer subtype• Ie. Winnipeg, Manitoba, Canada

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Deciduous forest biome

Page 26: World climates

Marine west coast

• Characteristics• Mild winters, mild

summers. • Low annual

temperature range. • Heavy cloud cover;

high humidity.

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Biome: deciduous forest

Page 28: World climates

Dry midlatitude climate

• These dry climates are limited to the interiors of North America and Eurasia.

• Cold winters and warm or hot summers. A small amount of rain falls during this season.

• Annual temperatures range widely.

Reno, Nevada, USA

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Grassland biome

Page 30: World climates

POLAR ZONE

Page 31: World climates

Subartic climate

• Characteristics• Brief, cool summers;

long, hard cold winters.

• Largest annual temperature ranges.

• Lowest temperatures outside of Antarctica.

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Biome: Taiga

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Tundra

• Characteristics• At least 9 months

average below freezing.

• Low evaporation; precipitation usually below 300 mm.

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Biome: Tundra

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CLIMATE AND HUMAN ACTIVITIES

Page 37: World climates

POPULATION

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CLIMATE AND FARMING

Page 39: World climates

TROPICAL CLIMATES

BURNING RAINFOREST

TOBACCO PLANTATION

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MONSOON CLIMATE

Page 41: World climates

TEMPERATE CLIMATES

WEST COAST VINEYARDS CALIFORNIA

Page 42: World climates

HUMID CONTINENTAL CLIMATE

GRASSLAND AREA