POSITIVE FEEDBACKS
- more snow: increased albedo, cooler atm.
- lower sea level: exposed continental shelf, incr. albedo, aerosols
- sea ice: fresh water freezes easily, air colder, high albedo
- fresh surface water turns off thermohaline circulation
no production of Atlantic deep water
no Gulf Current to warm North Atlantic
slow circulation increases oceanic CO2 (decr. atm. CO2)
|
NEGATIVE FEEDBACKS
- cold ocean - water vapor 20% - 33% less
lower biol. productivity, + CO2 in atm
reduced precipitation on glaciers
- ice sheet growth
|