π elss sg4 Flashcards
(42 cards)
location of arctic tundra
northern hemisphere
north of arctic circle at 66.5N
size of arctic tundra
8 million km squared
average annual temp of AT
-12.2 c
annual temp change
33c
average annual precipitation
137mm
type of seasons
summer: 2-3 months, 2-3c, always light
winter: 8-9 months, -30c, dark for 3 months straight
vegetation characteristics
no trees due to short growing season & low temps
some small shrubs in summer but very low NPP
soil characteristics
active layer: ground that is frozen in winter but melts in summer
permafrost: permanently frozen ground for at least 2 years
talik: unfrozen ground
precipitation in AT
very little and normally snow
evapotranspiration in AT
low temps so little ET as not enough heat to melt ice/snow
run off in AT
in summer more run off because ice melts, in winter stays frozen
infiltration in AT
permafrost is impermeable so water canβt infiltrate
store of water in atmosphere in AT
low temps so little ET
store of water in soil and ground water in AT
permafrost is impermeable so no water can infiltrate into ground (very small store)
store of water in vegetation in AT
not correct climate for vegetation to grow so very little water stored in it
store of water on surface in AT
in summer, impermeable permafrost so puddles etc
in winter none because active layer freezes
how does temperature in AT affect flows and stored in water cycle
very cold = low ET = so little stored in atmosphere
permafrost = impermeable surface = little stored in soil
how does rock permeability and porosity in AT affect flows and stored in water cycle
active layer becomes waterlogged as ground is impermeable so active layer becomes water logged and surface storage and overland flow increases
how does relief in AT affect flows and stored in water cycle
flat land due to weathering and erosion so lots of surface storage as doesnβt run off
photosynthesis in arctic tundra
short growing season as bad climate for vegetation to grow so little photosynthesis
respiration in arctic tundra
little respiration bc little vegetation and wildlife as too cold
decomposition and soil respiration in arctic tundra
too cold for decomposition so very little
ground is frozen so soil organisms canβt respire
carbon in the atmosphere in arctic tundra
small amount bc little respiration and decomposition
carbon in biomass in arctic tundra
small amount due to low temps, little water availability, few nutrients so vegetation doesnβt grow