the atmosphere
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The Atmosphere. Earth’s Atmosphere and Distribution of Earth’s Heat on Land and Water. EQ: How do air pressure and temperature vary in the atmosphere?. Standards S6E3b ; S6E4a,b; S6E5j; S6E6a. The Air Around You. Atmosphere Chapter 12 Section One. The Air Around You. - PowerPoint PPT PresentationTRANSCRIPT
EQ: How do air pressure and temperature vary in the
atmosphere?
StandardsS6E3b; S6E4a,b; S6E5j; S6E6a
The Air Around YouWeather is the condition of Earth’s
atmosphere at a particular time.Atmosphere: the layer of gases that surrounds
EarthEarth’s atmosphere is composed of nitrogen,
oxygen, carbon dioxide, water vapor, and other gases.
Earth’s atmosphere contains oxygen and other gases that living things need to survive.
Composition of the AtmosphereNitrogen
Makes up ¾ of the air we breathe.Oxygen
2nd most abundant gas in the atmospherePlant and animals take oxygen from their
surroundings and use it to release energy from food in a cellular process.
Is needed for fire to burnOzone
Form of oxygen that has three oxygen atoms in each molecule
Composition of the AtmosphereCarbon dioxide
Is present in small amounts in the atmosphereEssential to lifeAnimals produce carbon dioxideBurning fossil fuels increases the amount of
carbon dioxide in the atmosphere.Water Vapor
Water in the form of a gasProduces clouds
Importance of the AtmosphereEarth’s atmosphere makes conditions on
Earth suitable for living things.Traps energy from the sun which keeps most
of the Earth’s surface warm.Water exist in liquid form.
Air PressureProperties of air:
Consists of atoms and molecules that have mass
MassDensityPressure
Pressure is the force pushing on an area or surface.
Air pressure is the result of the weight of a column of air pushing down on an area.
Air PressureHow are mass and air pressure related?
The weight of air in the atmosphere causes air pressure.
So why doesn’t air pressure crush objects?The reason is that the molecules of air push in
all directions. The air pushing down on an object is balanced by the air pushing up on the object.
How does the density of air affect air pressure?Denser air exerts more pressure than less
dense air.
Measuring Air PressureAn instrument used to measure air pressure is
a barometer. Two kinds of barometers
Aneroid Mercury
Unit of Air Pressure2 different units of measurement
Inches of mercury millibars
How does altitude affect air pressure?Altitude, or elevation,
is the distance above seal level.
Air pressure decreases as altitude increases.Less oxygen
molecules to breathe at higher altitudes.
As air pressure decreases, so does density.
Altitude Affects Air PressureSea level air has the weight of the whole
atmosphere pressing on it.So air pressure is greater at sea level.The air near the top of the atmosphere has
less weight pressing on it , and thus has lower air pressure.
Altitude Also Affects DensityAs you go through the atmosphere, the
density of the air decreases.This means the gas molecules that make up
the atmosphere are farther apart at high altitudes than they are at sea level.
The air contains 21% oxygen.There are fewer oxygen molecules at high
altitudes.
Layers of the AtmosphereKey Concepts
What are the four main layers of the atmosphere?
What are the characteristics of each layer?
What are the layers of the atmosphere?Scientists divide Earth’s atmosphere into four
main layers classified according to changes in temperature. TroposphereStratosphere (Ozone layer)MesosphereThermosphere
Ionosphere Exosphere
TroposphereWe live in the
troposphere.All weather and
water vapor are in this layer.
Gets colder as you go up.
Clouds0-18 km
Stratosphere2nd layer of the atmosphereTemperature s get warmer are you go up.12 – 50 kmContains the Ozone layer.
Absorbs ultraviolet radiation
MesosphereProtects Earth’s surface from being hit by
meteoroids.Coldest region of atmosphere50 – 80 km
ThermosphereOutermost layer of Earth’s atmosphereAbove 80 kmAir is thin, it is very hot because the sun
strikes this layer firstDivided into 2 layers:
Ionosphere, lower layer of thermosphere 80 – 400 km Radio waves bounce back to Earth’s surface
Exosphere, outer layer of thermosphere 400 – 1000 km Artificial satellites orbit here
Energy from the SunKinds of energy from the sun
Visible lightInfrared radiationUltraviolet radiation
Can cause sunburns, skin cancer, and eye damageWhen Earth’s surface is heated, it radiates most
of the energy back into the atmosphere as infrared radiation.
Greenhouse effect Process by which a blanket of gases around the
Earth that hold heat in the atmosphere.
Heat TransferThree forms of heat transfer:
Radiation Direct transfer of energy by electromagnetic waves
Ex. – heat from the sun travels by radiation Conduction
Direct transfer of heat from one substance to another substance by direct contact. Ex. – pot on a stove
Convection The transfer of heat by the movement of fluid
Ex. – Upward movement of warm air and the downward movement of cool air form convection currents.
WindsA wind is the horizontal movement of air from an
area of high pressure to an area of low pressure.Winds are
Caused by the unequal heating of the earth.Cool, dense air flows under warm, less dense air.
Measuring windSpeed (anemometer)Direction (wind vane)
Wind-chill factor – the increased cooling a wind can cause.
Local WindsWinds that blow over short distances.Caused by the unequal heating of Earth’s
surface within a small area.During the day, land warms up faster than
water.At night, the land cools faster than water.
Global WindsWinds that blow steadily from specific
directions over long distancesCreated by unequal heating of Earth’s
surface.Occur over a large areaGlobal convection currents
Produced by temperature differences between the equator and the poles
Coriolis EffectEarth’s rotation makes winds curve