The Amazon Flashcards
Location & key characteristics
- located in South America
- 60% of the 6,7 million square km rainforest is in Brazil, the other 40% is shared between 8 other nations: Bolivia, Columbia, Guyana, Peru, Suriname, Venezuela and french guinana
- it has 300 billion trees and stores 1/5th of all carbon in the planet’s biomass, also accounting for 30-50% of global photosynthesis
- wide range of plants: myrtle, laurel, palm and acacia
- rainforests hold most of their nutrients in their live vegetation, not in the soil. Their soils do maintain nutrients very well which means that exiting nutrients leech out being carried away as it percolates through the soil
What happen to the water
- the average rainfall in the amazon basin is 3000mm per year, wit the greatest rainfall coming between December-May and temperatures average 28oc, resulting in a very humid climate.
- high humidity and unstable weather results in heavy rainfall most days with 25% of the rainfall being evaporated due to humidity, a lot of water vapour is from transpiration from the trees
- 75% of this total rainfall is intercepted by the trees and then to the ground through stem flow -> of the 75% half is used by plants and eventually returned to the atmosphere through evapotranspiration -> other half infiltrates the soil
- stored temporarily on the ground surface or flowing overland to river channels (runoff)
What are the main drivers of change to the Amazon water cycle
- the amazon rainforest has lost approximately 17% of its primary rainforest in the last 50 years
- 80% due to cattle ranching mainly for economic growth as they export a lot of meat across the world (mainly SA&NA)
- other reasons include logging, mining and for housing to keep up with population growth
- between 200 and 2007, 19386km squared was being destroyed per year
- in Brazil, 2022 was the greatest amount of deforestation ever as a result of shortages in the economy of things like paper as a result of Covid; compared to 2023 where deforestation was down by 50% as a result of greater environmental awareness and concern.
- several factors contributed to change, both human&physical: Deforestation, climate change, land use changes, forest degradation, river damming, agricultural practices, feedback mechanisms, extreme events and global atmospheric circulation
Processes contributing to the change in the rainforest water cycle: deforestation
- clearing large areas of the rainforest for agriculture, logging, and other purposes reduces the forests transpiration and evaporation, affecting local and regional precipitation patterns
- reduced vegetation cover can lead to decreased moisture recycling within the ecosystem
Processes contributing to the change in the rainforest water cycle: climate change
- altered global climate patterns, including rising temperatures and changing precipitation regimes, can influence the intensity and frequency of rainfall in the Amazon
- changes in climate may lead to more prolonged dry seasons and altered storm patterns
Processes contributing to the change in the rainforest water cycle: land use changes
- conversion of natural vegetation to urban areas, agricultural, or pastureland can disrupt the natural water cycle and reduce the forests ability to absorb and release water
- changes i land use can impact the overall balance of evapotranspiration and precipitation
Processes contributing to the change in the rainforest water cycle: forest degradation
- selective logging, wildfires, and other forms of rest degradation can disrupt the integrity of the rainforest, impacting its ability to maintain a healthy water cycle
- degradation reduces the forests resilience to environmental changes
Processes contributing to the change in the rainforest water cycle: river damming
- construction of dams for hydroelectric projects alters the flow of rivers, affecting sediment transport, nutrient cycling, and the overall hydrological balance of the region
- dam construction can lead to changes in river dynamic and influence local weather patterns
Processes contributing to the change in the rainforest water cycle: agricultural practices
- agricultural activities, such as large-scale farming and cattle ranching, can lead to changes in land cover and runoff patterns, impacting the natural flow of water within the ecosystem
- house of irrigation can also modify local hydrological conditions
Processes contributing to the change in the rainforest water cycle: feedback mechanisms
- changes in the water cycle may trigger feedback mechanisms, creating self-reinforcing cycles of environmental change. For example, increased temperatures can lead to more evaporation, further influencing precipitation patterns
Processes contributing to the change in the rainforest water cycle: extreme events
- increasing frequency and intensity of extreme weather events such as droughts and intense storms, ca have significant impacts on the Amazon water cycle, affecting river levels, groundwater recharge, and overall ecosystem health
Processes contributing to the change in the rainforest water cycle: global atmospheric changes
- alterations in global atmospheric circulation patterns, such as El Niño and La Niña events, can influence regional climate conditions, impacting the Amazons water cycle
Why do topical rainforests play a vital part in the carbon cycle
- tropical rainforests play a crucial role in the carbon cycle because they act as significant carbon sinks (wood is about 50% carbon). The dense vegetation in these forests absorbs and stores large amounts of carbon dioxide through photosynthesis. This stored carbon is then released during respiration, but a substantial portion remains sequestered in the trees and soil. The preservation of these rainforests helps mitigate the effects of climate change by reducing atmospheric carbon dioxide levels
- the amazon is estimated to store between 80 and 120 billion tonnes
- rainforests around the globe act as carbon sinks of around 1-3gtC/year
- biomass of these rainforests have been increasing due to increase sequestration of CO2 concentrations - this acts as an Edgar I’ve feedback loop
- it is assured that increased CO2 levels encourages biomass growth. However, although rainforests are growing quicker, they are dying much sooner
Physical impacts on the carbon cycle
- the arm and wet tropical climate is ideal for plant growth. This promotes the process of photosynthesis. This absorbs huge quantities of carbon dioxide from the atmosphere. In return, the rainforest emit oxygen. Wood is about 50% carbon, so rainforests themselves are a huge store as well as a sink in mitigating the effects of global warming
- respiration by plants, trees and the many animals return CO2 back to the atmosphere. Decomposition is an active process. Bacteria and fungi thrive in the warm, wet conditions. This then releases CO2 back into the atmosphere. Some carbon may be stored within the soil or dissolved and then removed by streams as an output from the rainforest system
Human impacts on the carbon cycle
- slash&burn -> cheap, quick and effective. The blackened stumps and ground surface is carbonised wood. Apart from what is stored in this burnt debris, the rest of the carbon has been emitted into the atmosphere as CO2; when burnt for land clearance between 30-60% of carbon is immediately released into the atmosphere. In a typical year the Amazon absorbs 2.2bn tonnes, by 2015 this had decreased to just 1bn tonnes
- photosynthesis ceases until new plant growth begins. This is by far the most significant impact of deforestation on the carbon cycle. Plant and animal respiration drop to almost zero. Rain washes ash into the ground. This increases the carbon content in the soil. In heavy rainfall, carbon in runoff may increase too. Decomposes will be largely absent from this environment
- HOWEVER: replacing rainforest with alternate uses, such as crops and pasture, reintroduces stores and flows, although operating at much less effective levels