1 water cycle Flashcards
systems approach
systems approaches study hydrological phenomena by looking at
the balance of inputs and outputs
how water is moved between stores by flows
stores
reservoirs where water is held
eg ocean
fluxes
the rate of flow between the stores
processes
physical mechanism that drives the fluxes of water between the stores
cryosphere
areas of the earth where water is frozen into snow or ice
blue water
water stores in rivers, streams, lakes and groundwater in liquid form
(the visible part of the hydrological cycle)
green water
water stored in soil and vegetation
precipitation
the movement of water from the atmosphere to the ground
evaporation
change in state of water from a liquid to a gas
residence time
the average time a water molecule will spend in a reservoir or store
fossil water
ancient groundwater from former pluvial periods
transpiration
diffusion of water from vegetation into the atmosphere, involving change from gas to liquid
groundwater flow
the slow transfer of percolated water underground through porous rocks
catchment
area of land drained by a river
watershed
the highland which divides and separated waters flowing to different rivers
condensation
the change from a gas to a liquid
eg water vapour into water droplets
dew point
temperature at which dew forms
it is a measure of atmospheric moisture
convectional rainfall
the earths hot surface heats the air above it
often associated with intense thunderstorms which occur widely in areas with ground heating such as the Tropics
cyclonic rainfall
warm air is forced to rise when it is undercut by colder air
a period of sustained rain which is associated with the passage of depressions
orographic rainfall
when air is forced to rise over a barrier such as a mountain, it cools and condensation takes place
through fall
rainfall persists or is relatively intense and the water drops from leaves/neadles etc
stem flow
when water tickles down along twigs and branches and then down the trunk
infiltration
the movement of water from the ground surface into the soil
infiltration capacity
maximum rate at which rain can be absorbed by soil