D4.3 Climate change Flashcards
(26 cards)
Greenhouse gases
Natural process where certain gases trap heat and warms the planet
Enhanced greenhouse effect
Warming of earth’s surface due to increase in concentration of greenhouse gases
Steps of greenhouse effect
- Short wave radiation (UV) passes through atmosphere, warms the surface
- Heat energy is radiated into atmosphere, most heat lost to space
- Some heat energy absorbed by molecules of greenhouse gases in atmosphere, then re-emitted
- Re-emitted heat energy warms the atmosphere and surface
Positive feedback cycle
A cycle where the product of a reaction leads to increase in that reaction
Release of CO2 from deep ocean
Marine organisms die -> sink to benthic zone -> broken down by decomposers -> release of CO2
Ocean surface warms -> more phytoplankton -> more food -> up biomass -> more dead matter
Increase in absorption of solar radiation
Increasing temp -> melting snow -> more dark surface -> higher absorption of light -> increasing temp
Albedo
Ability of surface to reflect light
Accelerating rates of decomposition in permafrost
Higher temp -> higher rates of decomposition -> higher CO2
Peat bog
Stores of partially decomposed organic material
Release of methane from melting permafrost
Higher temp -> permafrost melt -> decomposition -> higher methane
Permafrost
Ground that remains frozen year round
Increase in droughts and fires
Higher temp -> lower rainfall -> drier areas, more fires -> release of CO2 -> loss of vegetation -> lower photosynthesis -> higher CO2
Boreal forest net carbon accumulation to net loss
Higher temp -> shorter winter -> lower snowfall -> less snowmelt -> less water available -> conifers turn brown and fall off -> fuel for fires
Legacy carbon combustion
Large amounts of ancient carbon burns and releases CO2 into atmosphere
Carbon sink
More carbon absorbed than released
Carbon source
More carbon released than absorbed
Land fast sea ice
Ice fastened to the shore and does not move
Nutrient upwelling
Natural process where current bring deep water to surface
Range migration
Higher global temperatures and shorter winters allowing tree population to spread towards the poles
Carbon sequestration
Capture and storage of carbon
Coral reef feedback cycle
Higher CO2 -> ocean acidification -> suppression of calcification in corals
Higher water temp -> coral bleaching
Forest regeneration
Replanting trees
Afforestation
Planting trees where no forests previously were
Phenology
Study of timing of periodical events in biology