Climate Change Flashcards
Residence time for fossil fuel pools
long or short
usually long, but we shorten it up by burning these pools for energy
ice age unit (quantity)
about 4.5 degrees celsius
Turnover rate for biospheric pools
fast or slow
fast
vegetation life is short, so turnover rate is fast
4 components in Long term CO2 and temperature feedback loops
- greenhouse effects/long wave radiation exposure changes
- ocean temps change
- changed oceans absorbs varied CO2 from the atmosphere
- atmospheric CO2 changes
repeat
Precession:
1 of 3 natural causes for variations in earth’s CO2/temperature
changes in the DIRECTION of Earth’s tilt
cycles last 19,000-23,000 years
Snowball Earth
what the earth would be without greenhouse gases to trap heat on the planet
POSITIVE feedback loops
A loop that perpetuates itself but needs outside intervention to stop
Greenhouse Gases (GHGs):
gases in the atmosphere that absorb long-wave radiation reflected off Earth’s surface and then re-radiate that heat back toward Earth
Climate change
= persistent changes in average weather conditions
Fossil fuels
type of carbon pool
fuel sources (such as coal or oil) comprised of remains (organic matter) from organisms that lived in the earth’s geological past.
3 Traits of Weather systems
- chaotic
- unpredictable
- long-term
Atmospheric pool
type of carbon pool
comprised of the atmosphere
Carbon cycle:
describes the movement of carbon through biotic and abiotic components of the Earth system
and/or
movement from pool to pool
The 4 Greenhouse Gases
CO2
methane
nitrous oxide
water vapor
How we measure carbon levels throughout earth history
- glacier core samples
What plants use carbon for
to make cellulose and legnin
Eccentricity:
1 of 3 natural causes for variations in earth’s CO2/temperature
changes in how circular (or ovular) our orbit around the sun is
cycles last ~100,000 years