Carbon EQ1 Flashcards
carbon cycle
exchange of carbon between its four main reservoirs
atmophere
CO2/Methane (CH4) - gaseous carbon
hydrosphere
dissolved CO2 - can be gaseous, inorganic or organic
lithosphere
fossil fuels and limestones/ calcium carbonates - inorganic carbon
biosphere
living and dead organisms - organic carbon
flux
connect reservoirs together to create cycles and feedbacks
closed system
nothing can leave or enter the cycle, total amount in the cycle stays the same
biogeochemical cycle
a system of natural processes that recycle nutrients in various forms from the environment to the organisms and then back to the environment
quantifying stores and fluxes
scientists measure amount of carbon on earth in gigatons or petagrams
CO2 fluxes are higher in the northern hemisphere
greater landmass
spring/summer - smaller concentration, absorbed
autumn/winter - larger concentration, released when leaves decay
sequester
act of removing, separating, or seizing something
oceanic biological pump
phytoplankton are responsible for most of transfers of carbon from the atmosphere to the ocean
thermohaline circulation
1 - main current begins in polar oceans where the water gets cold, sea ice forms, surrounding seawater gets saltier, increases in density and sinks
2 - current is recharged as it passes Antarctica by extra cold salty, dense water
3 - division of main current northward into the indian ocean and into the western pacific
4 - two branches warm and rise as they travel northward, then loop back southward and westward
5 - now warmed surface waters continue circulating around the globe, on their eventual return to the north atlantic they cool and the cycle begins again
when can carbon fluxes happen
diurnally - during the day fluxes are positive, at night the fluxes are negative (loss from ecosystem to atmosphere)
seasonally - northern hemisphere winter atmospheric CO2 concentration rise and during the spring atmospheric concentrations drop
terrestial store - mangroves and soil
where in the world - along tropical and sub tropical tidal coasts in Africa, Australia, Asia and America
how do they store carbon - biological carbon stored in form of dead organic matter
what will happen if store damaged - mangroves cleared for tourism and agriculture, carbon released back into the atmosphere