Water Cycle Flashcards
Systems approach
Systems approaches study hydrological phenomena by looking at the balance of inputs and outputs, and how water is moved between stores and flows
Stores
Reservoirs where water is held, such as the oceans
Fluxes
The rate of flow between the stores
Processes
The physical mechanisms that drive the fluxes of water between the stores
Cryosphere
Areas of the Earth where water is frozen into snow or ice
Blue water
Water stored in rivers, streams, lakes and groundwater in liquid form (visible part of the hydrological cycle)
Green water
Water stored in the soil and vegetation (the invisible part of the hydrological cycle)
Precipitation
The movement of water in any form from the atmosphere to the ground
Evaporation
The change in state of water from a liquid to a gas
Residence time
The average times a water molecule will spend in a reservoir or store
Fossil water
Ancient, deep groundwater from former pluvial (wetter) periods
Transpiration
The diffusion of water from vegetation into the atmosphere, involving a change from a gas to a liquid
Groundwater flow
The slow transfer of percolated water underground through pervious or porous rocks
Catchment
The area of land drained by a river and its tributaries
Watershed
The highland which divides and separates waters flowing to different rivers
Condensation
The change from a gas to a liquid, such as when water vapour changes into water droplets
Dew point
The temperature at which dew forms; it is a measure of atmospheric moisture
Convectional rainfall
Often associated with intense thunderstorms, which occur widely in areas with ground heating such as the Tropics and continental interiors
Cyclonic rainfall
A period of sustained, moderately intensive rain; it is associated with the passage of depressions
Orographic rainfall
Concentrated on the windward slopes and summits of mountains
Interception loss
This is water that is retained by plant surfaces and later evaporated or absorbed by the vegetation and transpired. When the rain is light, for example drizzle, or of short duration, much of the water will never reach the ground and will be recycled by this process (it’s the reason you can stand under trees when it’s raining and not get wet).
Throughfall
This is when the rainfall persists or is relatively intense, and the water drops from the leaves, twigs, needles, etc.
Stem flow
This is when water trickles along twigs and branches and then down the trunk
Infiltration
The movement of water from the ground surface into the soil
Infiltration capacity
The maximum rate at which rain can be absorbed by a soil
Surface run-off
The movement of water that is unconfined by a channel across the surface of the ground. Also known as overland flow
Throughflow
The lateral transfer of water down slope through the soil via natural pipes and percolines