2.4 Flashcards
5 biomes
aquatic - freshwater and marine forest - tropical, temperate, boreal grassland - tropical or savanna and temperate desert - hot and cold tundra - arctic and alpine
biome
a collection of of ecosystems sharing similar climatic conditions
biosphere
part of the Earth inhabited by organisms
biomes are where they are because
of climate
temperature, precipitation, geography/terrain - latitude. altitude
factors that affect the global distribution of temperature
- hotter near the equator cooler towards the poles (increased latitude) This is because sun rays hit the earth at a more acute angle and so spread over a greater surface area
- colder with increasing latitude/altitude
- ocean currents and winds distribute surplus heat energy at the equator towards the poles - latent heat - El Nino
temperate forests
rainfall sufficient to establish a forest
temperatures and light intensity vary between season
deciduous/coniferous trees
less complex structure than rainforest and often dominated by one species
some layering, although trees no taller than 30metres
lower and less dense canopy than rainforest means more light so rich shrub layer
tropical rainforest
high rainfall, sunlight and temperature
no seasons, consistent light and temperature
complex structure trees up to 50m
dense canopy, only 1% sunlight reaches the floor, sparse shrub layer
soils are thin and nutrient poor
desert
low rainfall (under 250mm a tear0
Hisgh sunlisht,; bery hot in the day cold at night
scarce vegetation
plants - cacti animals - adapted to desert conditons
soil has a low-water holding capacity, erodes easily in the wind
tundra
high latitudes
low temperatures, low precipitation, seasonal sunlight; short-day length
simple structure, vegetation is low scrub and grasses it forms a single layer
permafrost and soil limit productivity
temperate grasslands
flat areas dominated by grasses and herbaceous plants
temperature range high, low rainfall
tricellular model of atmospheric circulation components
explains the distribution of biomes
polar cell
Ferrel cell
Hadley cell
TRICELLULR MODEL CELLS
0 degrees the equator recieves the most insolation
hot air rises, as it cools the water vapour condenses as rain
air moves away from the equator north and south
30 degrees from the equator dry air sinks
some air returns to form the Hadley Cell
some is blown further north collecting water vapour from the sea
they meet cold polar air and rise (as they are less dense) at 60 degrees
this leads to low pressure areas associated with heavy rainfall
some air flows towards the poles and some back towards lower latitudes (Ferrel Cell)
the air at the poles then descends as it gets cooler forming a high pressure area at the poles (Polar Cell)
deep ocean biome
the ocean and seafloor beyond continental shelves
pressure increases with depth
temperature variation decreases to a constant -2 degrees at depth
light limiting below 1000m there is none
nutrients - lower level and low primary productivity but some dead organic matter falls to deep ocean floors
3xample. arctic, Atlantic, pacific oceans
succession
is how an ecosystem changes in time
zonation
is how an ecosystem is changing along an environmental gradient,e g. altitude