Indonesia Rainforest Case Study Flashcards
(36 cards)
Country profile
Largest economy in SE Asia
Industries- petroleum,natural gas, textiles
GDP per capita- $13,900
Current issues
Poverty, improving education, preventing terrorism
Location
South east Asia, South east of Malaysia, south west of Philippines
Sumatra is west Indonesia, Central Kalimantan is central Indonesia
Climate of Kalimantan
High rainfall from November to April
Temperature stays constant through the year, peak of 28degrees
Climate of Sumatra
Lowest rainfall in June/july
More rain fluctuation, 300mm in November
Consistent temperature
What happens to most rainfall on tropical rainforests
Canopy intercepts up to 70%
About 25% evaporates
Of remaining 75%, half used by plants, other half infiltrated
What flow is minimal in tropical rainforests
Ground water- base flow
Transfers in the rainforest
Evapotranspiration
Precipitation
Drip flow
Stem flow
Evaporation
Stores in the rainforest
Atmospheric moisture
Interception storage
Water in plant tissue
Surface storage
Soil water
What is the Climate of the rainforest
Warm and wet climate, helps promote photosynthesis
Rainforests release a lot of oxygen
Why are rainforests carbon sinks
Wood is about 50% carbon so rainforests are good carbon sinks
Releasing co2 from rainforests
Decomposers thrive in warm wet conditions
This released co2 to the atmosphere
Key stores and transfers
Carbon is lost through respiration, and decomposition
Some carbon is internally transferred from above ground to below ground
Palm oil usage in Indonesia
Caused 22.8% of deforestation in 2001-16
Large amounts of palm oil exports, and used in goods
Timber usage in Indonesia
Used for construction and exported
13.9% of deforestation in 2001-16
Growth of palm oil
Production has grown significantly in the past 10 years
Multi purpose crop, used in foods and shampoos.
85% of all palm oil is produced in Malaysia and Indonesia
Impact on interception storage after localised deforestation
Size decrease due to cut down trees
Impact on evapotranspiration after localised deforestation
Increase, higher amounts of rainfall hitting the ground, more surface water
Impact on throughflow after localised deforestation
Decrease, smaller amounts of trees intercepting water
Impact on overland flow after localised deforestation
Increase, higher amounts of water hitting soil, not infiltrating
Impact on channel flow after localised deforestation
Increase, due to higher quantities of water over the ground
Changes to water balance through extensive deforestation
Less through flow and overland flow due to less precipitation
Evaporation and precipitation become equal
Rainfall reduced due to lack of evapotranspiration, less water in the atmosphere
Predicted forest loss in south east Asia
Loss of 20% between 2000-2100
Precipitation per month loss of 7mm