Climate and Climate Change
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Transcript Climate and Climate Change
Section 1: Pg. 472
Climate vs. Weather
Weather changes easily…day by day
Climate is different.
It is an average of the year to year temperature and
precipitation in an area.
Climate changes result in a change of climate all over the
world.
Factors that Influence Temperature
Latitude: Climates hear the equator are
warm….farther from the equator are cold
Altitude: The higher elevation it has, the colder it is
Ocean Currents: Warm currents can warm the air
above them, causing the temperature to be warm in a
certain area that would normally be cold.
Zones of Latitude
Tropical Zones: Near equator, direct sunlight year
round, warm climate
Polar Zones: Near the poles, never has direct sunlight,
cold climate
Temperate Zones: Between tropical and polar. In
summer, they have direct sunlight---warm….In winter,
sun hits at an angle, so they are cold.
Climate types
Marine Climates:
Located near oceans
Have little changes in temp…mild summers, cool winters
Happens because water doesn’t change temperature
easily
Continental Climates: Extreme Temperature changes
with very cold winters and warm to hot summers.
Ocean currents don’t affect these climates
Factors the Influence Precipitation
Prevailing Winds: Carry air masses that change
humidity and temperature
Mountain Ranges: Cause air masses to rise and cool as
they travel over high landscape
Windward: Side of the mountain that the wind hits
Leeward: Side of the mountain opposite the wind
Seasonal winds: Bring changes as the seasons change
Changing of the Seasons
Caused by the tilt of the earth on it’s axis.
As the earth rotates, the sun hits it at various angles.
This causes the change of the seasons…
Turn to page 479 in your book……
Classification of Climates
2 factors
Weather
Temperature
6 Regions:
Tropical Rainy
Dry
Temperate Marine
Temperate Continental
Polar
Highlands
Tropical Rainy
2 types
Tropical Wet: Low lying areas near the equator
Most days have rain (many days out of the year)
Rain Forest: Happen in tropical wet climates and have
rainfall year round.
Tropical Wet and Dry: Areas near the equator that
have distinct dry and rainy seasons
Savannas: Tropical grasslands that have scattered
clumps of trees that can survive the dry season.
Dry
2 Types
Arid: Less than 25 cm of rain per year with extreme
temperatures
Deserts: Arid regions that get less than 25 cm of rain a
year. Can be hot and sandy, or cold and rocky.
Semiarid: Found at the edges of deserts. They are dry,
but have enough rainfall to support small plant life.
Steppe: Area that is dry, but gets enough rainfall for
short grasses and low bushes to grow.
Temperate Marine Climates
Found near oceans
All types have humid, mild winters
Marine West Coast: Coolest, mild rainy winters, summer
precipitation varies (Found on west coast of US). Allows for
thick forests and tall trees.
Mediterranean: Drier and warmer (S. Coast of California and
Mediterranean sea). Mild temperatures, winter---rainy,
summer---little rain
Humid Subtropical: Found in the edges along the
tropical/temperate zone. Climates are wet and warn, but not
constantly hot. Found in the southern tips of the US.
Temperate Continental Climates
Only on Continents in N. Hemisphere
Humid Contental: Tropical and polar air masses shift,
changing temperature and precipitation constantly. In
winter, cold weather moves in from the polar, and in
summer, tropical bring heat and humidity. These
areas receive moderate rain in the summer, and small
amounts in the winter.
Subarctic: North of the humid continental. Has
short, cool summers, and Long very cold winters.
Polar Climates
Coldest climate region
Ice Cap: Found on greenland and Antartica
Avg. temps at or below freezing
Covered with ice and snow year round
Very dry air---due to ice
Tundra: Short, cool summers….Long Cold winters
Permafrost: Permanently frozen tundra soil
Highlands
Areas of high elevation within other regions
High elevation makes them colder than the areas
around them
Usually has low temperatures and more precip than
areas around them.
Will have a tree line where areas at a certain elevation
are too cold for trees to grow.