Earth's Biomes and Spatial Diversity Flashcards
climate
long term average weather
solar radiation angle and surface temperature
sun hits the equator directly - hotter
at the poles, light hits less directly and is spread further - cooler
earth tilts 23.5 degrees - seasonal variation (more sun/closer in summer). variation is most impactful at poles
topography
- mountains
physical features of the earth
mountains can be glaciated to reflect heat
ocean currents and wind and heat movement
move heat to poles - equator is less hot than expected and the poles are warmer
wind and ocean current mechanisms
- hot air rises from equator and spreads towards poles, cooling as it goes. eventually it is dense enough to return to the surface where it heats and moves towards the equators
- series of cells (heating and cooling cycles)
- when warm air moves up, cool air replaces it (wind)
Coriolis effect
because of the earth’s counterclockwise rotation about its axis, winds and oceanic currents in the Northern Hemisphere deflect to the right and those in the south deflect to the left
earth’s rotation and winds and water
earth rotates clockwise - equator moves furthest and fastest in a spin
- wind push oceans to form currents in surface water
- water carries more heat than air and moves to the poles
- cold water sinks and moves to equator
rainfall
- warm air carries more water vapour than cold air
- rising air cools = rain
- descending air warms, taking more moisture = arid climate
rain shadows
the area on the lee side of mountains, where air masses descend, warming and taking up water vapour; these lands are arid
- takes moisture into mountains where the air cools and it rains
biomes and distributions
distributions of biomes reflect regional climates
evapotranspiration
the sum of evaporation directly from soils and water bodies plus the amount transpired by plants
potential evapotranspiration
the amount of evapotranspiration that temperature, humidity and wind would cause if water supply wasn’t limiting; the demand on water in an ecosystem
potential evapotranspiration ratio
the ratio of water demand to supply - what vegetation can be supported?
plant evolution
evolve to conditions and may look similar but be unrelated
tundra
coldest, short days - grasses, moss, rabbits, wolves
alpine
lacks permanent ice below soil (tundra), cold, windy, small plants
taiga
cool, moist forests, rainy summers, conifers, mosses, shrubs, moose
temperate coniferous forest
lots of rain, enormous conifers, warm