Lec 6 Flashcards
Permafrost is dependent on
Climate
Surface characteristics
Thermal properties of the ground
Bogs active layer
Shallow active layers due to insulating properties of peat which dries in the summer
Fens are wet which
Enhances the depth of the summer thaw
Ice wedge formation
Frozen winter grown below -10 degrees begins to crack
Cracks fill with water in spring expanding the ice wedge
This pushes up soil
Ice-wedge polygons go from what to what over time
High centered to low centered over time
Thermokarst lakes (Thaw lakes)
Body of freshwater, usually shallow, that is formed in a depression by melt water from thawing permafrost
Depressions often produced by collapse of ground levels associated with permafrost thaw
Ebullition
Bubbling of methane from decomposition
Coastal erosion
Sea level rise
Longer open water periods
Climate change implications of peatlands
Greater quantities of methane are emitted which offset atmospheric CO2
Enhanced warming at high latitudes could result in a positive feedback as increasing rates of anaerobic microbes yield a higher quantity of methane