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The atmosphere

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Page 1: The atmosphere
Page 2: The atmosphere

• They include

nitrogen,

oxygen, argon,

carbon dioxide

and other

noble gasses

• The gas that is

most abundant

is nitrogen

Page 3: The atmosphere

•Water vapor

•Aerosols

•Ozone

Page 4: The atmosphere

–Up to about 4% of the air's volume

–Forms clouds and precipitation

–Absorbs heat energy from Earth

Page 5: The atmosphere

–Tiny solid and liquid particles

–Water vapor can condense on solids

–Reflect sunlight

–Help color sunrise and sunset

Page 6: The atmosphere

–Three atom oxygen (O3)

–Distribution not uniform

–Concentrated between 10 to 50 kilometers above the surface

–Absorbs harmful UV radiation

–Human activity is depleting ozone by adding chlorofluorocarbons (CFCs)

Page 7: The atmosphere
Page 8: The atmosphere
Page 9: The atmosphere

•Weather is over a short

period of time

•Constantly changing

Page 10: The atmosphere

•Climate is over a long

period of time

•Generalized,

composite of weather

Page 11: The atmosphere

•Temperature

•Humidity

•Cloudiness

•Precipitation

•Air pressure

•Wind speed and direction

Page 12: The atmosphere

•Temperature is amount of heat in a

substance. Expressed in degrees

Fahrenheit or Centigrade (Celsius)

•Temperature is measure by an

instrument called a thermometer.

Page 13: The atmosphere

• The sun heats up the water on land and causes evaporation.

• The moisture the is in the air is called humidity.

• Saturated is when the air has too much moisture and cannot hold anymore.

Page 14: The atmosphere

• It is the ratio of how much

moisture is in the air and how

much the air can hold.

• 50% humidity means the air is

holding 50% moisture

Page 15: The atmosphere
Page 16: The atmosphere

• Wind is moving air in the atmosphere.

• Air is always moving from high pressure to low pressure.

• The strongest winds are tornadoes, the air pressure is extremely low.

Page 17: The atmosphere

• Wind speed is measure in kilometresper hour (kph). We use a device called an anemometer.

• Wind Direction is always stated in terms of where the wind is coming from.

Page 18: The atmosphere

• Wind Sock

»Weathervane

Page 19: The atmosphere

• When there is too much moisture, the water

will fall as precipitation.

• Precipitation will fall in two main forms: rain or

snow depending on the temperature of the air

through which the moisture will fall.

• Other forms of precipitation are sleet and hail.

Page 20: The atmosphere
Page 21: The atmosphere

• If the air is cooled below the freezing point of water, the condensing moisture is quickly freeze into ice crystals.

• The ice crystals join to make snowflakes

• Snowflakes are always six sided.

Page 22: The atmosphere

• When droplets

of moisture join

together

becoming

heavy enough

to fall to the

ground.

Page 23: The atmosphere

• Formed in

cumulonimbus

(storm) clouds.

They are

frozen droplets

of moisture.

Page 24: The atmosphere

• When falling rain starts off in warmer air, but passes through air below freezing, the rain drops cool and freeze onto surfaces when they hit the ground.

Page 25: The atmosphere

• It takes 10 centimetres of snow to

make one centimeter of rain.

• Dew is moisture in the air cools off

at night. In the morning it is found

on everything. In colder

temperatures, dew is frost.

Page 26: The atmosphere

• The force that is applied on everything on the Earth caused by the weight of the air.

• Air particles are mobile, the exert pressure on objects.

• High air pressure brings warm, dry air. Low air pressure brings rain or moisture

Page 27: The atmosphere

• Air pressure can change quickly, ie-when a storm comes in.

• There are three factors that affect air pressure: altitude, air mass temperature and the amount of moisture in the air.

• A Barometer is used to measure air pressure.