1.c. the water cycles have distinctive processes and pathways that operate within them Flashcards
evaporation
When water changes state from a liquid to gas (usually due to heating)
- Latent heat is taken in
Factors that affect the rates:
Temperature -> warmer it is -> more evaporation
Humidity -> more humid it is -> air is already saturated -> no concentration gradient > less evaporation
Wind -> winds can blow saturated air out of an environment -> and bring in unsaturated air -> increasing evaporation
transpiration
When water changes state from a liquid to gas via vegetation
Factors that affect rates:
Same as evaporation-
Temperature -> warmer it is -> more transpiration
Humidity -> more humid it is -> air is already saturated -> no concentration gradient -> less transpiration
Wind -> winds can blow saturated air out of an environment -> and bring in unsaturated air -> increasing transpiration
Others-
SA of vegetation -> more exposure to air -> more transpiration
Amount of vegetation -> more transpiration
Type of vegetation -> evergreen trees vs deciduous trees -> yearly transpiration in evergreen vs none in winter months in deciduous
condensation (including cloud formation)
When water changes state from a gas to liquid (usually due to cooling)
- Latent heat is given off
- Adiabatic lapse rates (DALR and SALR)
- Types of clouds (Cumuliform, Stratiform, Cirrus, Advection fog)
- Cloud formation
Air rises -> air cools with altitude -> air CONDENSES when DEW POINT is reached -> clouds form
precipitation (including causes of precipitation)
Convectional rainfall
Sun heats earths surface -> air is heated and rises -> clouds form
Spatial variation- mostly in warmer places near the topics
Temporal variation- in summer seasons
Relief rainfall
Air is forced to rise over a mountain -> clouds form-> often dry conditions on the other side
Frontal rainfall
Where a warm and cold air mass meet -> hot air rises above -> clouds form
Spatial variation- found in mid-latitudes e.g. England
interception
The process by which vegetation catches + stores rainfall before reaching the surface
Factors that affect rates- (same as others)
SA of vegetation -> more surface to intercept rainfall
Amount of vegetation -> thicker + denser vegetation e.g. forests intercept more effectively than grass -> more throughfall including stem flow + leaf drip
Type of vegetation -> evergreen trees vs deciduous trees -> yearly interception in evergreen vs none in winter months in deciduous trees
ablation
snow melt
runoff (including overland flow and saturated overland flow)
Surface runoff-
Water travelling across the earth’s surface -> and into the river
Factors that affect rates-
- Soil/ rock permeability
catchment hydrology (including infiltration, percolation, through flow, groundwater flow and cryospheric processes)
Infiltration
The process by which water moves from the surface down into the soil by gravity
Factors that affect rates-
Type/ permeability of soil
-> clay -> fewer air spaces -> more compact when wet -> less infiltration
-> sandy -> more air spaces -> more infiltration
Antecedent conditions -> if soil is
-> saturated from last rainfall event
-> frozen solid from low temps
-> baked dry by hot, dry temps
-> less infiltration
Soil depth
-> deep soils -> greater capacity -> more infiltration
-> shallow thin soils -> less capacity -> less infiltration
Percolation-
The process by which water moves from the soil down into the ground rock by gravity
Factors that affect rates-
- Rock permeability
Throughflow-
The horizontal movement of water through the soil
Factors that affect rates-
- Soil permeability
Groundwater flow-
The horizontal movement of water through the ground rock
Factors that affect rates-
- Rock permeability
Cyospheric processess-
Ablation -> snow melt
Accumulation -> the growth of ice
Sublimation -> water changing straight from a solid to gas