2.A - the carbon and water cycle in the Amazon basin Flashcards
where is deforestation happening?
- deforestation and degredation occurs in southern brazil/closer to major cities and centres of economy
- most accessible part
what happens to surface run off without trees
surface run off increases by 27% without trees
why is the forest degraded?
- selective logging
- replacing w/ monoculture plantations and grazing land
- not as good at storing carbon
- 80% used for cattle
- NO interception, surface run off, speed up lag time, gullying, soil erosion = ↓ capactiy of river
how much deforested land is used for cattle?
80%
what causes the rainforest’s huge input of rainfall?
- equator = suns rays most concentrated
- so there’s an excess of energy and it has to be re-distributed (tri-cellular model)
- ITCZ shifts N and S with the seasons.
- January = ITCZ south = bands of low pressure = rain
how will the climate in the amazon impact the stores and flows of the carbon/water cycle?
- humid so atmosphere is a big store of water
- biosphere, atmosphere and rivers = big stores
- heat drives flows
- lots of precipitation, evaporation and evapotranspiration
what happens in the ITCZ?
- where air rises the most = more rain
- moves between tropic of cancer and capricorn throughout the year
what is flux?
movement of CO2 from 1 part of the carbon cycle to another
how is the rainforest structured?
- STRATIFIED STRUCTURE
1. shrub layer (0-10m)
2. lower tree canopy (20m)
3. main canopy (20-40m)
4. emergents (50m+)
what % of light reaches the ground floor?
less than 3%
what is GPP?
the amount of carbon taken out of the air/carbon that trees fix is known as the gross primary productivty (GPP)
what do tropical rainforests have all year round?
a positive carbon balance
what % of human emitted CO2 do tropical rainforests absorb?
25%
how much carbon is taken in per hectare?
200-300 carbon tonnes
why is transpiration such a crucial part of the water cycle?
- clouds of water vapour forms above the rainforest canopy
- these are carried away by wind in aerial rivers to drier parts of Brazil and falls as rain
what are the inputs in the rainforest water cycle?
- precipitation is high in most months
- the dense canopy intercepts up to 75% of the rainfall.
- some of this water will be evaporated
what are the stores in the rainforest water cycle?
- atmospheric moisture
- interception storage
- water in plant tissue
- surface storage water in puddles
- soil water
what are the flows in the rainforest water cycle?
- evapotranspiration
- precipitation
- drip flow
- stem flow
- rainwater is transferred to the forest floor by a combination of drip flow and stem flow. drip tips help the tree to shed water from each leaf, and the rest trickles down branches and stems
- most rainforest plants have very shallow roots that take rainwater and dissolved nutrients directly from decomposing leaf litter
what are the outputs in the rainforest water cycle?
- water is lost by transpiration from pores in the leaves
- evaporation from the soil
how does precipitation vary seasonally in the rainforest?
- convectional rain falls all year round, though most areas experience at least one drier period
- rainfall is highest in March (310 mm) and lowest in August (60mm)
- high average annual rainfall (>2000mm) with no dry season
what % of precipitation is recycled?
- between 50-60% of precipitation is recycled by evapotranspiration
- water losses from the Amazon Basin result from river flow and export of atmospheric vapour to other regions
- this loss is made up by an inward flux of moisture from the Atlantic Ocean
what is precipitation like in the rainforest? case study details
- high avg annual rainfall (>2000 mm)
- rainfall is 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 75% of precipitation)
- intercepted rainfall accounts for 25% of all evaporation
what are rates of evapotranspiration like and why?
- high rates due to temperatures, abundant moisture and dense vegetation
- strong evapotranspiration–precipitation feedback loops sustain high rainfall totals
- around 50% of incoming rainfall is returned to the atmosphere by evapotranspiration
- most evaporation is from intercepted moisture from leaf surfaces
- moisture loss in transpiration is derived from the soil via the roots
what sustains rainfall?
strong evapotranspiration–precipitation feedback loops sustain high rainfall totals