Carbon Cycle Exam 3 Flashcards
(44 cards)
The ocean is the largest reservoir of carbon
~38,000 pg
Soils are distant second reservoir of carbon
~2,000 pg
Similar amounts of carbon in atmosphere
~897 pg
in living terrestrial plants
~600 pg
ocean surface
900 pg
photosynthesize as much as land plants in a year
Negligible as a reservoir
phytoplankton
changes in CO2 - inputs to atmosphere - Volcanism
0.05 - 0.2 per year
emissions from freshwater
0.1 pg
emissions from ocean
0.1 pg
outputs from atmosphere - weathering of rock
0.3 pg per year
Preindustrial Atmosphere is
~600 pg
Very long-term process (>1 million years)
Geologic factors (volcanism, weathering)
Evolution of plants
Medium term process (Glacial/interglacial ~ 0.1 million years)
Changes in solar radiation (milankovitch cycle)
Ocean/Atmosphere interactions
When earth is warmer…….
Weathering increases
CO2 declines
Each cools
When earth is cooler,,,,,,,,,
Weathering decreases
CO2 increases
Earth warms
the sun has _______ intensity through time
increased
living processes _____ faster than geologic processes
100x
terrestrial respiration
plant primary production
release of CO2 from ocean……
absorption of CO2 from ocean
changes in CO2 could _______ response by increasing surface temperature
amplify
changes would be _______ because CO2 stays in atmosphere for much longer
global
Possible oceanic mechanism
Temperature effect on bicarbonate system
higher export of production to depth
possible terrestrial mechanisms
Temperature effects on plant biomass
Sequestration or release of soil C
Under preindustrial conditions: Amount of CO2 is upwelled water depends on _______ of water and ________ CO2 when water sank
temp, atmospheric