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Climate change results in the intensification, acceleration or enhancement of the hydrological cycle
Inputs and outputs | |
---|---|
Precipitation (Input) | ● Warmer atmosphere holds more water vapour = more precipitation ● Rainfall is also likely to have a greater intensity ● High latitude areas more likely to have precipitation as rain rather than snow ● Some current dry areas may have less rainfall as heat waves intensify |
EVT (Output) | ● Warmer temperatures lead to higher rates of evaporation ● They also ↑ rates of vegetation growth, & ∴ transpiration |
Stores and flows | |
Snow and glacier melt | ● Periods of snowfall likely to ↓ in length ● Spring snowmelt will begin earlier ● Glaciers will ↓ in size and their snouts retreat due to less accumulation and more melting (disappearing faster than forming) |
Reservoirs and lakes | ● Storage amounts may ↓ w/ more evaporation ● Conversely, if precipitation ↑ then storage may ↑ |
Permafrost | ● More thawing will release more groundwater as the thickness of permafrost ↓ ● Methane release will add to global carbon stores and ↑ rates of climate warming |
Soil moisture | ● Likely to be unchanged as changes to precipitation and evaporation rates cancel each other out |
Runoff and streamflow | ● Greater variability of flows • more floods and more periods of low flow |
Although the world's population increase rate is slowing down, there is going to be 1 bn + more people to find water for by the middle of the century Climate change will occur over both short and long term periods, creating uncertainty regarding the security of water supplies:
Variations in the amounts of water held by reservoirs during a year
Impact of reduced water amounts on forested areas
Lower reliability of monsoon rains
↑ glacier melting may impact mountain communities
Lower amounts of snowfall may impact tourist activities skiing
↓ stores in aquifers will affect water supplies in dry areas
Droughts and associated heat waves may ↑ the incidence of wild fires
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