CASE STUDY - TROPICAL RAINFOREST Flashcards
(8 cards)
the water cycle in the amazon rainforest
- high rainfall (2000mm) evenly distributed - high-intensity and convectional
- high evapotranspiration bc dense veg and heat. 50-60% rainfall is recycled bc evapotranspiration
- rapid run off bc intense rainfall and steep slopes. low-lands - floodplains store water for months
- 25% rainfall intercepted - mainly from canopy trees
the carbon cycle in the amazon rainforest
- high NPP (net primary productivity) of 2500g/m2/yr
- the dense biomass stores larger carbon: above ground 180 tonnes // below ground (roots) 40 tonnes
- stores 80-120 bill tonnes of carbon and sequesters 2.4bill tonnes/yr
- rapid decomposition due to heat and humidity releases carbon to soil and atmosphere
- soils thin and nutrient poor
Physical factors affecting the flows and stores in the water cycle
- TEMP
- high all year round –> high evapotranspiration –> high humidity –> intense precipitation –> drives cloud formation and convection - RELIEF
- most of amazon = flat lowlands –> slow run-off
- western areas = steeper slopes –> faster run-off and flooding - GEOLOGY
- ancient permeable shield rock –> limited percolation –> rapid surface run off.
- some western areas made of limestone –> allow infiltration
Physical factors affecting the flows and stores in the carbon cycle
- TEMP
- high temps –> fast decomposition and high NPP.
- warm wet climate boosts co2 uptake and organic matter breakdown - VEG
- trees intercept rain and return water to atmo via transpiration.
- large biomass = key carbon store above and below ground - SOIL
- thin and leached
rapid nutrient cycling
- decomposition = fast carbon release + nutrients recycling - GEOLOGY
- lack of carbonate rocks = low geological carbon store
- mainly igneous rocks in basin
CHANGES to flows and stores in the WATER cycle - Madeira river basin - largest tributary of amazon - HUMAN factors
- deforestation –> reduced interception + transpiration –> less recycled rainfall
- increased surface run-off –> higher floor risk (eg Porto Velho flood 2014)
- less evapotranspiration –> less could formation –> less rainfall –> drying feedback loop
- deforestation reduces soil water storage and increases peak flow + shorter lag times
- previous floods during 2000-2012 mean Bolivian rainforest lost - more runoff - more floods
CHANGES to flows and stores in the water cycle - Madeira river WATER - largest tributary of amazon - NATURAL factors
- seasonal rainfall variations –> affect river discharge (dry vs wet season)
- Andes slopes naturally produce high run-off rates
Impact of human activity (deforestation, farming) on carbon flows, soil, and nutrient stores
DEFORESTATION
- reduces carbon absorption by 50-60% in degraded forest
- emissions rise due to burning
- above-ground carbon store drops 180 → 43 tC/ha, below-ground 64 → 12 tC/ha.
- Soil carbon falls due to erosion and reduced organic input
- loss of decomposer activity - reduces nutrients cycling
AGRICULTURE
- crops and pasture store less carbon
- burning and erosion degrade the soil carbon even more
Strategies to manage the tropical rainforest – positive effects on water and carbon cycles
SCHEMES
- legislation to preserve primary forest (Amazon Regional Protected Areas)
- afforestation - Parica project (planting 20 million tropical hardwoods)
- agroforestry - ppl trained to crop rotate
- dark soils - enriched with charcoal + waste - improves fertility –> 5X more productive
IMPACTS
- reduces flooding, run off and loss of nutrients
- Sequesters CO2 in trees and soil
- restores water cycle - interception, transpiration etc