Heating The Earth Flashcards
(22 cards)
Atmosphere
Mixture of gases
Layers of atmosphere
From bottom up Troposphere - contains most gases and water vapour Stratosphere Mesosphere Thermosphere
Gas percentages
Nitrogen - 78%
Oxygen - 21%
Water vapour, carbon dioxide - 1%
How does atmosphere influence the world
We breathe the air. It absorbs heat from the sun. It retains heat at night. It protects us from the Suns rays In the troposphere the weather is formed
How is the atmosphere heated
- The Suns Ray’s heat the earth.
- The earth heats the air around it.
(Diagram)
What causes uneven heating of the atmosphere
Latitude and tilt of the earth
Latitude (across)
Near the equator :
The sun heats a small area.
The Rays don’t travel through much atmosphere so they don’t lose much heat.
Equator is hotter.
Away from the equator :
The rays are spread out and heat a wider area.
Travel through more atmosphere so they lose heat.
Further away from the equator is colder.
(Diagram)
Tilt of the earth
Northern summer : northern hemisphere is tilted towards the sun.
- more heat
- longer days
- winter in the Southern Hemisphere
Northern winter : northern hemisphere is tilted away from the sun
- less heat
- longer nights
- summer in the Southern Hemisphere
(Diagram)
Greenhouse gas percentages
Carbon dioxide : 72%
Methane : 10%
CFC’s : 13%
Nitrous oxide : 5%
The greenhouse effect and global warming
Greenhouse effect is when the earth holds onto some of the heat.
Greenhouse gases cause global warming because they are being retained so more heat is.
Causes of global warming
Fossil fuels : more oil, coal and gas are being burned with increases carbon dioxide in the air.
CFC’s : more plastic, aerosols and fridges are being used which increase CFC’s
Tree’s : more trees are being cut down so there are less trees to absorb carbon dioxide.
Effects of global warming
Water shortages : crop failure and famines
Polar ice caps melting : causes sea levels to ride, creating risk of flooding in low lying areas such as the Netherlands and east England.
Tropical diseases like malaria may spread to warmer places. The desert will spread and ruin some African countries.
(Diagram)
Effects of global warming on Ireland
Rising temperatures : country will be drier (especially in the south), will improve some crop growth, reduce growth of potato, water shortages.
More rain : winter will be wetter,increased flooding, bog bursts, erosion of coastal areas and more flood protection.
Sea levels will rise
Solutions to global warming
Renewable energy : wind, water, sea power
Reduce deforestation : tress will hold more carbon dioxide
Increase energy conservation : energy efficient appliances, better insulation
What is wind and what causes it
Wind is air moving from high pressure to low pressure.
Atmospheric pressure (weight of air pressing down on earth)
Low pressure (air is warmer and lighter so it rises)
High pressure (air cools and is heavier so it’s sinks)
Winds blow from high pressure areas to low pressure areas
(Diagram)
Global wind patterns
Influenced by :
Uneven heating of the earth (creates high and low pressure areas)
Coriolis effect (deflects the wind to the right in the northern hemisphere and to the left in the Southern Hemisphere)
(Diagram)
Uneven heating of the earth global wind pattern
- Low pressure at the equator as the warm air rises. It moves away from the equator and cools. At 30*N latitude the air is heavy and presses down, creating a high pressure area.
- High pressure at North Pole. Air presses down. At 60*N latitude the air warms up and rises, creating a low pressure area.
(Diagram)
How is the global wind system influenced by the Coriolis effect
On a non spinning earth : winds would blow from a high pressure area to a low pressure area.
On a spinning earth : caused by the spinning of the earth. Wind is deflected to the right in
(Diagram)
Ocean currents
Warm currents : equator to north or south poles
Cold currents : north or south poles to equator
What causes ocean currents
Unequal heating of the oceans : cold water sinks and flows. Warm water rises
Prevailing winds : winds drag along the water to form the current
(Diagram)
Currents in the North Atlantic
Currents in the North Atlantic : the Labrador current freezes harbours along Canadian coat and brings icebergs and fog
The North Atlantic Drift : warm, begins at Gulf Stream, gives Ireland mild summer and keeps harbours ice free
The Canaries Current : cold, keeps African coast dry and prevent rain in the Sahara
Effects of ocean currents
Warm currents raise land and sea temperatures by rising the temperature of the air above sea level.
Cold currents lower land and sea temperatures