atmosphere Flashcards
(5 cards)
1
Q
Timeline of change of the atmosphere
A
- During first Billion years there was intense volcanic activity
- Volcanos realsed gasses that formed early atmosphere
- Gasses where water vapour, carbon dioxide, nitrogen
- small amounts Methane and Ammonium
- Earth atmosphere contained little to no oxegen, so very simular to planets like Mars and Venus.
- Earth cooled down and water vapour developed to form the oceans
- Some of carbon dioxide dissolved into oceans forming a weak acid
- This reacted with minearls in the sea to form preciptates
- Over time this formed sediments of carbonate rock on the seabed
- Some of carbon dioxide made coral and shells of organisms
- When they died they formed the sedementry rock limestone, while removing carbon dioxide from atmosphere
- Level of carbon dioxide began to fall
- Around 2.7 billion years ago the first Photosynthetic algae evolved in the oceans
- Proccess of photosynthisis produced oxegen which entered the atmosphere
- Plants evolved increasing amount of oxegen in atmosphere reaching point where animals could evolve
2
Q
Pecentage of gasses in the modern atomsphere
A
- 78% Nitrogen
- 21% Oxegen
- 0.04% Carbon dioxide
- 1 perecent everything else
3
Q
Early atmosphere
A
Lots of
- Carbon di-oxide
- Water vapour
- Nitrogen
Smaller amounts of
- Methane
- Ammonia
4
Q
Why can scientist not be certian about the early compositon of the atomosphere
A
The earth is around 4600 million years old, that means scientist cannot be sure about the early atmosphere
5
Q
How do greenhouse gasses work
A
- Suns heat energy goes down onto earth in form of shortwave radiaton
- Passes through atmosphere and hits surface of earth
- Some of the energy is absorbed and heats up ground
- Most is remmited or reflected into the atmosphere towards space in form of Longwave radiaton
- Some energy makes it back to space
- Most hits particles of Gas in atmosphere, which absorbs energy they then reimmit the energy in random dirrections
- Some energy remmited towards spave and some towards earth
- Most energy collides with other gas particles before leaving the atmosphere
- Proccess repeates keeping heating earth longer than if there was no atmosphere
- Keeps earth at stable temp