Water cycle and insecurity Flashcards
stores
reservoirs where water is held
fluxes
the rate of flow between 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
isolated systems
systems that don’t interact with anything outside the system boundary with no input or output of energy
closed systems
systems that have energy transfers into and beyond the systems boundary but with no transfer of matter
open systems
systems where energy and matter can be transferred into and beyond the system boundary
dynamic equilibrium
state where the inputs and outputs of a system are the same, managed by feedback
positive feedback
the effects of a change are amplified and can have multiplied or knock-on effects
negative feedback
the effects of a change are nullified by its knock-on effects
blue water
water stored in rivers, streams, lakes and groundwater in liquid form (visible part of the hydrological cycle)
green water
water stored in soil and vegetation (invisible part of the hydrological cycle)
residence time
the average time a water molecule will spend in a reservoir or store
precipitation
the movement of water in any form from the atmosphere to the ground
evaporation
the transformation of water droplets into water vapour by heating
interception
the prevention of rain from reaching the Earth’s surface by trees and plants
condensation
the process by which water vapour is converted to water
transpiration
the loss of water into the atmosphere from the leaves of plants
vegetation storage
the storage of water in the roots and stems of plants
stemflow
the movement of water through plants into the soil
surface storage
the total volume of water held on the Earth’s surface in takes, ponds and puddles
infiltration
the downward movement of water into the soil surface
soil water storage
the storage of water in the soil
percolation
the gravity flow of water within the soil
groundwater storage
the storage of water underground in permeable rock strata
overland flow
the movement of water over the surface of the land, usually when the ground is saturated, frozen or precipitation is too intense for infiltration to occur
throughflow
the movement of water downslope within the soil layer
groundwater flow
the slow transfer of percolated water through permeable or porous rocks
channel storage
the storage of water in river channels
channel flow
the movement of water within a river channel
river runoff
the discharge of a river through the drainage basin
river runoff
the discharge of a river through the drainage basin
fossil water
ancient, deep groundwater from former pluvial (wetter) periods
drainage basin/ river catchment
the area of land drained by a river and its tributaries that is an open system
watershed
the highland which divides and separates waters flowing to different rivers determining the boundary of a drainage basin