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Atmosphere The surrounding air of the Earth Layers of the atmosphere • There are 4 layers in the atmosphere • They are the troposphere, mesosphere, thermosphere, and stratosphere Troposphere • This is the layer that is closest to the surface of the earth • It’s elevation ranges from 0 to 10 km Stratosphere • This 2nd layer sits on top of the troposphere • It’s elevation ranges from 10 km to around 25 km • This layer contains the ozone layer, which protects us from harmful sunlight Mesosphere • This 3rd layer is above the stratosphere • It’s elevation ranges from 25 to 100 km Thermosphere • This is the highest layer of the atmosphere • It’s height ranges from 100 to 400 km • This is where most small meteorites burn up and is also the location in the atmosphere that the northern lights occur (aurora borealis) Composition of Air • There are many different types of gasses in the atmosphere • They include nitrogen, oxygen, argon, carbon dioxide and other noble gasses • The gas that is most abundant is nitrogen This powerpoint was kindly donated to www.worldofteaching.com http://www.worldofteaching.com is home to over a thousand powerpoints submitted by teachers. This is a completely free site and requires no registration. Please visit and I hope it will help in your teaching. Air Pressure • The measure of the force that the air molecules push on a surface • Air pressure “pushes” an object in all directions • As altitude increase, air pressure decreases Altitude • The height of an object above Earth’s surface • The greater the altitude, the less amount of air pressure Ozone • Located in the stratosphere, is a molecule made up of 3 oxygen atoms that absorb solar energy in the form of ultra-violet (UV) radiation warming the surrounding air • Radiation- the transfer of energy through empty space – Energy from the Sun heating the Earth’s surface – Takes place when there is NO direct contact between surfaces • Conduction- heat transfer by direct contact of particles of matter – Example: a metal spoon sitting in a hot bowl of soup – Heat will ALWAYS travel from the warmest object to the coolest object! • Convection- heat transfer involving the movement of fluids-liquids & gases from one particle to another • Caused by different temperatures & densities within the fluid • Heat rises & cold sinks • Greenhouse effect- a heating process on Earth where the gases in the atmosphere (ozone layer) trap thermal energy keeping the troposphere at a livable temperature. – 50% of the radiation that enters the Earth’s atmosphere is absorbed by the Earth’s surface • Global warming- the gradual warming up of Earth’s atmosphere – Contributes to the depletion of the ozone layer – Caused by human activity mostly • Burning of fossil fuels, deforestation, CFC’s, ect. • Wind- A flow or current of directionally moving air – Due to the Earth’s counterclockwise rotation, the Northern Hemispheres wind patterns typically blow from the west to the east – Can be either a warm or cold wind pattern – Ocean current mimic wind patterns • Coriolis Effect- The curved path that the rotation of the Earth causes the wind to travel in – Winds in the Northern Hemisphere travel to the right & in the Southern Hemisphere they travel to the left • Trade winds- Winds that blow from 30 degrees latitude to the equator – They are in both hemispheres – Have been used by sailors for hundreds of years – Doldrums • Where the northern & southern hemisphere trade winds meet in an area of low pressure • Very little wind; means “foolish” in Latin – Horse Latitudes • Area of weak winds at 30 degrees north & 30 degrees south latitude • Legend states that sailors would throw horses over the sides of their boats to make the boat lighter to sail • Westerlies- wind belts found in both the Northern & the Southern hemispheres between 30 degrees and 60 degrees latitude – Flow toward the poles in the opposite direction of the trade winds – Helped early traders return to Europe • Polar easterlies- wind belts that extend from the poles to 60 degrees latitude in both hemispheres; Form from cold sinking air • Jet streams- narrow belt of high-speed winds that blow in the upper troposphere and lower stratosphere; do NOT follow a regular path around Earth – changes speeds often and can exceed 500 km/hr – Wind that blows the weather systems across the land