2.4 Biomes, Zonation and Succession Flashcards
Define biome
collections of ecosystems sharing similar climatic conditions that can be grouped into five major classes
Explain the distributions, structure, biodiversity, and relative productivity of deserts
distribution:
- covers 20-30 percent of the land surface
- dry air
- high temperatures (45-49 C in day)
- low precipitation (250 mm yr-1)
structure:
- vegetation scarce (absence of trees).
- soil has low water holding capacity, low fertility
relative productivity:
- low rates of photosynthesis
- low NPP rates
5 major classes of biomes
aquatic, forest, grassland, desert and tundra
Explain the distributions, structure, biodiversity, and relative productivity of a tundra
distributions:
- high alt
- high temps
- seasonal sunlight
- short day length
structure:
- simple
- vegetation = low, single layer
- abscence of tall trees
- frozen permafrost = soil limit productivity
relative productivity:
- low mean NPP
- 0.14 kgm-2yr-1
Explain the distributions, structure, biodiversity, and relative productivity of a tropical rainforest
distribution:
- found between tropics of cancer and capricorn
- high rainfall
- high sunlight
- high temperatures
- no seasons = consistent light keeps temperatures
structure:
- complex structure
- emergent trees (up to 50m)
- dense canopy
- only 1% of light reaches floor
- soil = thin -> nutrients = poor
relative productivity:
- low mean NPP
- 2.2 kgm-2yr-1
Explain the distributions, structure, biodiversity, and relative productivity of a temperate forest
distribution:
- seasonal weather (hot summers/cold winters)
- mild climate, lower average temperature / lower rainfall
structure:
- 2 types of tree types in forests; Evergreen + deciduous could be in one forest or contain both trees
- rainfall average between 500-1500 mm yr-1
relative productivity:
- lower than rainforest
define insolation
the amount of solar radiation that reaches the Earth’s surface and affects temperature.
define precipitation
when rain, snow, sleet or hail falls from the sky.
what shows how insolation, precipitation and temperature determine the distribution of the biomes
Tri Cellular model of Atmospheric Circulation
Intro how the tricellular model contributes to the distribution of biomes
The tricellular model explains the distribution of precipitation and temperature and how they influence structure and relative productivity of different terrestrial biomes. The tricellular model is made up of three different air masses, these control atmospheric movements and the redistribution of heat energy. The three air masses, starting from the equator, are called the Hadley cell, Ferrel cell and the polar cell.
Discuss how climate change is impacting biomes and causing them to shift.
- increases in co2 + other greenhouse gases lead to an increase in global temperatures -> affect rainfall patterns
- these changes in climate affect the distribution of biomes
Convection Currents
Warm air rises as it heats and becomes less dense, cools at higher altitudes, increases in density, and descends, driving atmospheric and oceanic circulation patterns that influence global climate and biome distribution.
define zonation
refers to changes in community along an environmental gradient due to factors such as changes in altitude, latitude, tidal level or distance from shore (coverage by water).
define succession
the long term change in the composition of a community
difference zonation versus succession
zonation is a spacial phenomenon whereas succession is a temporal phenomenon
example zonation
rocky seashore:
The distinct vertical layers experience particular abiotic conditions. This is particularly clear in the distribution of plants and animals on a rocky seashore, where different species inhabit a series of horizontal strips or belts of the shore, approximately parallel to the water’s edge. In many places the strips (zones) are sharply bounded by the differently coloured seaweeds that populate them.
primary succession
- Begins with no life
- No soil present
- New area (e.g., volcanic island)
- Lichen and moss come first
- Biomass is low
secondary succession
- begins after removal of existing life
- soil present
- old area
- biomass is higher