Climates of the Earth.

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Presentation transcript:

Climates of the Earth

Key Terms Weather – The condition of the atmosphere in one place for a short period of time. Climate – Weather patterns that an area typically experiences during a long period of time.

The Greenhouse Effect Only a small amount of the sun’s heat reaches the Earth. Most is reflected back into space by atmosphere and the earth’s surface Enough remains to warm the earth’s land and water. Not all places get the same amount of heat and light 1. Location 2. Day and night 3. Seasonal Change

Earth’s Tilt and Rotation Axis – An imaginary line that runs through the center of the Earth between the North and South Pole Earth is tilted at a 23 ½ degree angle rotates on the axis 1. Not every place receives the same amount of sunlight this affects temperature Spins East to West

Earth’s Revolution Earth travels in an orbit around the Sun Revolution – One trip around the Sun 1. Takes 365 ¼ days to complete a revolution

Latitude – Describes climate a general way according to certain climate zones Low latitudes - Area between the tropics 1. Have very warm and hot climates Middle latitudes – area between the tropics and the Arctic / Antarctic Circles 1. Receives warm air from the tropics in the summer and cold air from the high latitudes in the winter. 2. Most places have a temperate climate 3. Weather changes dramatically with the seasons High latitudes – Area between the poles and the Artic /Antarctic circles (66 ½ degrees latitude to 90 degrees latitude) 1. Has a generally cold climate

Elevation Air get thinner as altitude increases Temperature drops 3.5 degrees farenheight for every 1000 feet gained in altitude High mountains stay covered in snow year around (Even on the equator)

Wind Patterns Prevailing winds – Winds that blow in a fairly constant direction Trade Winds – Prevailing wind in the low latitudes 1. They blow toward the equator Westerlies – Generally blow in an West to East direction Doldrums – Windless area near the Equator

Ocean Currents – Cold and warm rivers of sea water Cold water currents flow south from the poles Warm currents blow north from the Equator Currents affect the coastal land they pass.

Landforms Water – Takes longer to heat and cool than air 1. Interior land temperatures change more dramatically than coastal temperatures Mountain Ranges 1. Windward side – Side of a mountain facing the wind 2. Leeward side – Side of a mountain facing away from the rain, doesn’t get rain

Tropical Climates – Found in or near low latitudes Tropical Rain Forest – Near the equator 1. Warm humid rains almost daily 2. Amazon River basin contains the world’s largest tropical rainforest Tropical Savanna – Located in Africa and South America Has a dry season in the winter and a wet season in the summer

Dry Climates Desert Climates – Dry areas with sparse plant life 1. Annual rainfall is less than 10 inches 2. Extremely hot in the day and cold at night 3. Oasis – Area of lush vegetation in the desert (may be supported by under ground springs 4. Deserts cover about 1/5 or 20% of the earth’s land surface Steppe Climate – Dry areas bordering deserts 1. Annual rainfall is between 10 and 20 inches 2. Vegetation consist of short grasses, not many trees

Mid-latitude Climates Marine West Coast Climate – Usually found along the western coastlines between 30 and 60 degrees latitude 1. Ocean currents produce cool summers and mild winters Mediterranean Climate – Usually found between 30 and 40 degrees latitude 1. Mild rainy winters and hot sunny summers Humid Subtropical Climate – Usually found in the southeastern part of continents 1. Rainfall throughout the year, thunderstorms in the summer Humid Continental Climate – Influenced more by landmasses 1. The father north, the longer and more sever the winter gets 2. Only found in the northern hemisphere

High Latitude Climates Sub Arctic Climates – Located just below the Arctic circle Winters are bitterly cold and the summers are cool and short Tundra Climates – Located north of the sub arctic regions in the northern hemisphere Thin soil above permafrost Bitterly cold Winters