L5. Interception and throughflow Flashcards
What is interception loss?
Proportion of precipitation that may be intercepted by a vegetation canopy and lost to the atmosphere via evaporation without reaching the ground
What is the definition of interception?
Fraction of the gross precipitation input which does not reach the ground. Typically wets and adheres to above ground objects until it is returned to the atmosphere through evaporation.
Define gross precipitation (P)
Precipitation that is measured above the canopy or in a clearing
Define through-fall (T)
Precipitation reaching the ground directly or via canopy drip
Define stemflow (S)
Water reaching the ground by flowing along tree trunks and plant steams
Define total interception loss
Sum of all canopy interception and losses
Define net precipitation (N)
Gross precipitation minus total interception loss
Why is interception hard to measure directly during rainfall events?
Lots of spatial variability (vegetation density/type, wind, etc.). Lots of temporal variability since interception increase exponentially during a storm, until the interception capacity is achieved, and the weight of more rain overcomes the surface tension holding the water on the plants.
What is canopy storage for conifers
1-2 mm per square meter
What is canopy storage for deciduous trees?
less than 1mm per square meter
What is canopy storage for tropical trees?
1-5mm per square meter
What is canopy storage for grasses?
1-1.5mm per square meter
Why is interception a critical hydrological process?
- Can be a significant water source for evapotranspiration
- has a strong influence on runoff
- canopy drip can increase local erosion
What are 3 methods of interception measurements?
- above and below canopy (works in small areas but hard to get enough samples)
- plastic sheets (effective but doesn’t work over large areas and with snow)
- cantilever effect (accurate but would take way to long)
How does precipitation intensity influence interception?
High intensity rainfall events can lead to water being delivered too quickly for the plants to accommodate whereas low intensity rain events can allow for more precipitation to be intercepted (new storage capacity is continuously created by ongoing drippage and stemflow)