AMAZON RAINFOREST Flashcards
LOCATION
- In South America
- occupies area of more than 6 million km2
- 70% of rainforest in BRAZIL, but also extends into parts of Peru, Ecuador, Venezuela, Colombia, Bolivia, Guyana
- Amazonia is world’s largest rainforest
- Dominated by tall, evergreen, hardwood trees
WATER CYCLE: CLIMATE/CLIMATIC FEATURES
- high average annual temperatures between 25 °C + 30°C
- small seasonal variation in temperature
- high average annual rainfall (>2000 mm) with no dry season
High average temperatures are response to…
intense insolation throughout year
~ But, significant cloud cover ensures maximum temperatures do not reach extremes of subtropical desert climates.
Seasonal differences in temperature are…
small + convectional rain falls all year round, though most areas experience at least 1 drier period.
How much precipitation recycled by evapotranspiration in Amazonia
- Between 50 + 60%
Water losses from Amazon Basin result from
river flow + export of atmospheric vapour to other regions.
~ this loss made good by inward flux of moisture from Atlantic ocean
flows + stores in Water cycle in Amazon rainforest
Precipitation
Evapotranspiration
Run-off
Atmosphere
Soil/groundwater
Vegetation
- Precipitation
High average annual rainfall (>2000 mm)
Rainfall fairly evenly distributed throughout year though short drier season occurs in some places.
High-intensity, convectional rainfall
Interception by forest trees is high (around 10% of precipitation). Intercepted rainfall accounts for 20-25% of all evaporation
- Evapotranspiration
- High rates of evaporation + transpiration due to high temperatures, abundant moisture + dense vegetation
- Strong evapotranspiration-precipitation feedback loops sustain high rainfall totals
- Around half of incoming rainfall returned to atmosphere by evapotranspiration
- Most evaporation from intercepted moisture from leaf surfaces
- Moisture lost in transpiration is derived from soil via tree roots
Run-off
Rapid run-off related to high rainfall, intensive rainfall events and well-drained soils. Depending on seasonal distribution of rainfall, river discharge may peak in one or two months of the year.
atmosphere
High temperatures allow atmosphere to store large amounts of moisture (i.e. absolute humidity is high). Relative humidity is also high.
soil/groundwater etc
Abundant rainfall and deep tropical soils lead to significant water storage in soils and aquifers.
vegetation
Rainforest trees play crucial role in water cycle, absorbing + storing water from soil + releasing it through transpiration.
rainforest carbon cycle
Amazonia’s humid equatorial climate creates ideal conditions for plant growth.
Amazon rainforest is major global reservoir of stored carbon, absorbing 2.4 billion tonnes a year.
Compared to other forest ecosystems, RAPID exchanges of carbon between atmosphere, biosphere + soil
Warm, humid conditions ensure speedy decomposition of dead organic matter + quick release of CO2
Meanwhile, HIGH rates of carbon fixation through photosynthesis
Amazonia’s leached + acidic soils contain only limited carbon + nutrient stores.
fact that such poor soils support biome with highest NPP + biomass of all terrestrial ecosystems, emphasises speed with which organic matter is broken down, mineralised + recycled.
NPP, biomass, storage of carbon from large trees + soil
Net primary productivity (NPP) is high, averaging 2500 grams/m3/year
biomass is between 400 and 700 tonnes/ha.
Large forest trees typically store around 180 tonnes C/ha above ground, + further 40 tonnes C/ha in their roots.
Soil carbon stores average between 90 + 200 tonnes/ha.
Physical factors such as…affect flows + stores of water in Amazon rainforest + other environments.
geology, relief + temperature
Geology + effect on flood hydrograph
Impermeable catchments (e.g. large parts of Amazon Basin are ancient shield area comprising impermeable, crystalline rocks) have minimal water storage capacity resulting in rapid run-off
Permeable + porous rocks (e.g limestone + sandstone) store rainwater + slow run-off
Relief (slopes)
Most of Amazon Basin comprises extensive lowlands. In areas of gentle relief, water moves across surface (overland flow) or horizontally through soil (throughflow) to streams + rivers.
In the west the Andes create steep catchments with rapid run-off. Widespread inundation across extensive floodplains (e.g. Pantanal) occurs annually, storing water for several months + slowing its movement into rivers.
temperature
High temperatures throughout year generate high rates of evapotranspiration
Convection is strong, leading to high atmospheric humidity, development of thunderstorm clouds + intense precipitation.
Water cycled continually between land surface, forest trees + atmosphere by evaporation, transpiration + precipitation.
Physical factors affecting stores and flows of carbon
Forest trees dominate the biomass of Amazon Basin + are principal carbon store. In total approximately 100 billion tonnes of carbon locked up in Amazon rainforest.
Absorbing around 2,4 billion tonnes of CO, a year + releasing 1.7 billion tonnes through decomposition, rainforest is a carbon sink of global importance.
Carbon CYCLES between forest + other living organisms, soil + atmosphere.
Photosynthesis connects rainforest to atmosphere carbon stores.
% of rainforest carbon stored in above ground biomass of tree stems, branches and leaves.
60%
remainder is below ground, mainly as roots and soil organic matter.
High temperatures, high rainfall and intense sunlight stimulate…
primary production.
NPP averages about 2500 grams/m2/year. Amazonia alone accounts for
15-25 per cent of all NPP in terrestrial ecosystems.
Leaf litter + other dead organic matter accumulates temporarily at soil surface + within rainforest soils.
High temperatures + humid conditions promote
rapid decomposition of organic litter by bacteria, fungi + other soil organisms.
Decomposition releases nutrients to soil for immediate take-up by tree root systems, + emits CO2 which is returned to atmosphere.
geology of Amazon Basin is dominated by
ancient igneous and metamorphic rocks. Carbonates are largely absent from the mineral composition of these rocks.
However, in western parts of basin, close to Andes, outcrops of limestone occur. In context of slow carbon cycle they are significant regional carbon stores.