hydrology runoff and erosion Flashcards
what is effective rainfall and when does it happen
precipitation - interception (held by vegetation leaf storage and then evaporated). losses can be between 6-80%. this is mainly when there is a low rainfall event
how do you measure effective rainfall
mm through fall (non intercepted open rainfall) - mm stem flow (intercepted on base of tree/vegetation)
what is runoff
effective rainfall - infiltration
what is groundwater
deep soil layer that is saturated with water in all pores
what is a runoff ratio
it measures the fraction of P that becomes runoff
it is a function of soil and cover (curve number)
does Australia have a high runoff ratio
low ratio (8%) compared to global average 35%
what is hortonian runoff
infiltration limited runoff occurs when there is quick high-intensity rainfall that exceeds the hydraulic conductivity of the soil. this is more likely to occur on a hill slope
what is dunne runoff
saturated/storage limited runoff occurs when there is steady high rainfall that completely saturates soil and water can no longer infiltrate. this is more likely to occur on the lower part of the landscape
what is a curve number
range (1-100 less to more runoff) parameter to predict the amount of runoff from the amount of precipitation.
refers to hydraulic condition (amount of cover) and hydrological conductivity number (soil group)
limitations of CN and how it is overcome
good first estimate however limitations include unclear data source, not good for short term averages, variation due to moisture and can be adjusted for these variations
what is the hydrograph
a plot of discharge/runoff/flow over time
what is a quick flow
surface flow runoff can be hortonian dunne runoff, determines peaks in hydrograph heavily influenced by precipitation
what is slow flow
water that infiltrates into soil and passes through groundwater runoff into the stream
how does a well work
well inserted into an aquifer that is under a confining layer and a lot of fo pressure it releases water by releasing pressure.
how does groundwater streamflow input vary with climate (eg humid vs arid)
input can vary from 0-70%.
in humid systems, it is a gaining system meaning the rain is higher than ET therefore continuous draining of groundwater
in arid systems it is a losing system meaning ET is higher than rainfall input therefore groundwater does not flow into the river and can actually be recharged by stream inflows