CASE STUDY - TROPICAL RAINFOREST Flashcards

(8 cards)

1
Q

the water cycle in the amazon rainforest

A
  • 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
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2
Q

the carbon cycle in the amazon rainforest

A
  • 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
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3
Q

Physical factors affecting the flows and stores in the water cycle

A
  1. TEMP
    - high all year round –> high evapotranspiration –> high humidity –> intense precipitation –> drives cloud formation and convection
  2. RELIEF
    - most of amazon = flat lowlands –> slow run-off
    - western areas = steeper slopes –> faster run-off and flooding
  3. GEOLOGY
    - ancient permeable shield rock –> limited percolation –> rapid surface run off.
    - some western areas made of limestone –> allow infiltration
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4
Q

Physical factors affecting the flows and stores in the carbon cycle

A
  1. TEMP
    - high temps –> fast decomposition and high NPP.
    - warm wet climate boosts co2 uptake and organic matter breakdown
  2. VEG
    - trees intercept rain and return water to atmo via transpiration.
    - large biomass = key carbon store above and below ground
  3. SOIL
    - thin and leached
    rapid nutrient cycling
    - decomposition = fast carbon release + nutrients recycling
  4. GEOLOGY
    - lack of carbonate rocks = low geological carbon store
    - mainly igneous rocks in basin
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5
Q

CHANGES to flows and stores in the WATER cycle - Madeira river basin - largest tributary of amazon - HUMAN factors

A
  • 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
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6
Q

CHANGES to flows and stores in the water cycle - Madeira river WATER - largest tributary of amazon - NATURAL factors

A
  • seasonal rainfall variations –> affect river discharge (dry vs wet season)
  • Andes slopes naturally produce high run-off rates
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7
Q

Impact of human activity (deforestation, farming) on carbon flows, soil, and nutrient stores

A

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

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8
Q

Strategies to manage the tropical rainforest – positive effects on water and carbon cycles

A

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

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