2.a. It is possible to identify the physical and human factors that affect the water and carbon cycles in a tropical rainforest. Flashcards
Where is the Amazon rainforest located?
Located in South America.
How much area does the Amazon rainforest occupy?
More than 6 million km2.
What percentage of the Amazon rainforest is in Brazil?
70% of the rainforest is in Brazil, but extends to six other countries.
Amazonia is dominated by what kind of trees?
(The Rainforest Water Cycle)
Tall, evergreen, hardwood trees.
Outline the 3 climatic features within the Amazon rainforest.
(The Rainforest Water Cycle)
High average annual temperatures between 25°C and 30°C.
Small seasonal variation in temperature.
High average annual rainfall (>2000 mm) with no dry season.
What causes high average temperatures within the Amazon rainforest?
(The Rainforest Water Cycle)
Act as a response to intense insolation throughout the year.
However, significant cloud cover ensures that maximum temperatures do not reach the extremes of sub- tropical desert climates.
Outline seasonal differences in temperature, within the Amazon rainforest.
(The Rainforest Water Cycle)
Differences include small and convectional rain falls all year round, though most areas experience at least one drier period.
What percentage of precipitation in Amazonia is recycled by evapotranspiration?
(The Rainforest Water Cycle)
Between 50-60%.
Water losses from the Amazon Basin are caused by what? How is this loss of water made positive?
(The Rainforest Water Cycle)
Caused by river flow and exports of atmospheric vapour to other regions (evapotranspiration).
This loss is made good by an inward flux of moisture from the Atlantic Ocean.
Outline precipitation in the Amazon rainforest.
(The Rainforest Water Cycle)
High average annual rainfall (>2000 mm).
Rainfall fairly evenly distributed throughout the year though short drier season occurs in some places.
High-intensity, convectional rainfall.
Interception by forest trees is high (around 10 per cent of precipitation).
Intercepted rainfall accounts for 20-25 per cent of all evaporation.
Outline evapotranspiration in the Amazon rainforest.
(The Rainforest Water Cycle)
High rates of evaporation and transpiration due to high temperatures, abundant moisture and dense vegetation.
Strong evapotranspiration-precipitation feedback loops sustain high rainfall totals.
Around a half of incoming rainfall is returned to the atmosphere by evapotranspiration.
Most evaporation is from intercepted moisture from leaf surfaces.
Moisture lost in transpiration is derived from the soil via tree roots.
Outline run-off in the Amazon rainforest.
(The Rainforest Water Cycle)
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.
Outline atmosphere in the Amazon rainforest.
(The Rainforest Water Cycle)
High temperatures allow the atmosphere to store large amounts of moisture (i.e. absolute humidity is high). Relative humidity is also high.
Outline soil/ groundwater in the Amazon rainforest.
(The Rainforest Water Cycle)
Abundant rainfall and deep tropical soils lead to significant water storage in soils and aquifers.
Outline vegetation in the Amazon rainforest.
(The Rainforest Water Cycle)
Rainforest trees play a crucial role in the water cycle, absorbing and storing water from the soil and releasing it through transpiration.
What does NPP stand for?
Net Primary Productivity.
What is ‘Net Primary Productivity’ (NPP)?
The amount of biomass or carbon produced by primary producers per unit area and time
Amazonia’s humid equatorial climate creates ideal conditions for what?
(The Rainforest Carbon Cycle)
Plant growth.
In the Amazon rainforest, is NPP high or low? What is the average values for carbon and biomass?
(The Rainforest Carbon Cycle)
NPP is high.
Carbon: 2500 grams/m2/year.
Biomass: between 400 and 700 tonnes/ha.
How much carbon does a large Amazon rainforest tree typically store?
(The Rainforest Carbon Cycle)
180 tonnes C/ha above ground.
40 tonnes C/ha in their roots.
What is the average carbon capacity for soil stores?
(The Rainforest Carbon Cycle)
Between 90 and 200 tonnes/ha.
The Amazon rainforest is a major global reservoir of stored carbon. How much does it store each year?
(The Rainforest Carbon Cycle)
2.4 billion tonnes a year.
Compared to other forest ecosystems, are carbon exchanges in the Amazon slow?
(The Rainforest Carbon Cycle)
No, in comparison they are quicker - with exchanges of carbon between the atmosphere, biosphere and soil all being rapid.
Why are carbon exchanges in the Amazon rainforest much greater than in other forest ecosystems?
(The Rainforest Carbon Cycle)
Warm, humid conditions ensure speedy decomposition of dead organic matter and the quick release of CO2.
Rates of carbon fixation through photosynthesis are high.
Does Amazonia’s leached and acidic soils have plentiful carbon and nutrient stores? What does this show?
(The Rainforest Carbon Cycle)
No, the stores are limited.
This shows that poor soils support a biome with the highest NPP and biomass of all terrestrial ecosystems, emphasising the speed with which organic matter is broken down, mineralised and recycled.
What 3 factors affect flows and stores of water in the Amazon rainforest and other environments?
(Physical factors and stores and flows of water)
Geology, relief, and temperature.
Outline geology’s effect on the flood hydrograph.
(Physical factors and stores and flows of water)
Impermeable catchments (e.g. large parts of the Amazon Basin are an ancient shield area comprising impermeable, crystalline rocks) have minimal water storage capacity resulting in rapid run-off.
Permeable and porous rocks such as limestone and sandstone store rainwater and slow run-off.
Outline relief’s effect on the flood hydrograph.
(Physical factors and stores and flows of water)
Most of the Amazon Basin comprises extensive lowlands.
In areas of gentle relief, water moves across the surface (overland flow) or horizontally through the soil (throughflow) to streams and rivers.
In the west the Andes create steep catchments with rapid run-off.
Widespread inundation across extensive floodplains (e.g. the Pantanal) occurs annually, storing water for several months and slowing its movement into rivers.
Outline temperature’s effect on the flood hydrograph.
(Physical factors and stores and flows of water)
High temperatures annually generate high rates of evapotranspiration.
Convection is strong, leading to high atmospheric humidity, the development of thunderstorm clouds and intense precipitation.
Water is cycled continually between the land surface, forest trees and the atmosphere by evaporation, transpiration and precipitation.
What dominates the biomass of the Amazon basin?
(Physical factors affecting stores and flows of carbon)
Forest trees.
These are the principal carbon store.
In total, how many tonnes of carbon is locked up in the Amazon rainforest?
(Physical factors affecting stores and flows of carbon)
Approximately 100 billion tonnes.
How much CO2 does the Amazon rainforest absorb each year? How much is released through decomposition?
(Physical factors affecting stores and flows of carbon)
2.4 billion tonnes of CO2 a year
1.7 billion tonnes through decomposition.
What percentage of rainforest carbon is stored in the above ground biomass of tree stems, branches, and leaves? What about the remainder?
(Physical factors affecting stores and flows of carbon)
60%.
The remainder is below ground, mainly as roots and soil organic matter.
What process connects the rainforest to the atmosphere carbon stores?
(Physical factors affecting stores and flows of carbon)
Photosynthesis.
What three things stimulate primary photosynthesis production?
(Physical factors affecting stores and flows of carbon)
High temperatures, high rainfall, and intense sunlight.
How much does Amazonia account for (alone) of all NPP in terrestrial ecosystems?
(Physical factors affecting stores and flows of carbon)
15-25%.
Leaf litter and other dead organic matter accumulates temporarily at the soil surface and within rainforest soils. What promotes the rapid decomposition of of organic litter? What carries out the decomposition?
(Physical factors affecting stores and flows of carbon)
Leaf litter and other dead organic matter accumulates temporarily at the soil surface and within rainforest soils.
High temperatures and humid conditions promote rapid decomposition of organic litter.
This is carried out by bacteria, fungi, and other soil organisms.
What are the products of decomposition within the Amazon rainforest?
(Physical factors affecting stores and flows of carbon)
Releases nutrients to the soil for immediate take-up by tree root systems.
Emits CO2 which is returned to the atmosphere.
Outline the geology of the Amazon Basin.
(Physical factors affecting stores and flows of carbon)
Dominated by ancient igneous and metamorphic rocks.
Carbonates are largely absent from the mineral composition of these rocks.
State 3 reasons for why deforestation is carried out.
(Human factors affecting stores and flows of water)
Crop farming.
Cattle farming.
Road construction.
Settlement.
Mining.
Logging.
Fuel.
What is the average rate of deforestation each year in the Amazon?
(Human factors affecting stores and flows of water)
17,500km²/year.
Since 1970, how much of primary Amazon rainforest has been destroyed or degraded?
(Human factors affecting stores and flows of water)
1/5.
In what year did deforestation rates fall? Why did they go back up?
(Human factors affecting stores and flows of water)
Began to fall from 2009.
They have risen in recent years after the appointment of now former Brazilian president Bolsonaro.
How was deforestation in the Upper Madeira drainage basin affected the water cycle?
(Human factors affecting stores and flows of water)
Reduced water storage in forest trees, soils, permeable rock and the atmosphere.
Fewer trees also means less evapotranspiration and less precipitation.