The water cycle and water insecurity Flashcards
Water stress
the demand for water exceeds the available amount during a certain period. If renewable water resources are between 1,000-1,700 m3 per capita per year. Restrictions for usage as well as conflict for water supplies
Water scarcity
between 500-1,000m3 (renewable) per capita per year, usually open tension, and conflict
Absolute water scarcity
renewable water sources are very low (less than 500m3 per capita), resulting in widespread restriction on use
Economic water scarcity
when access to water is limited by capital, technology, and governance
Physical water scarcity
more than 75% of a countries or regions population water is being used
Saltwater encroachment
when salt water contaminates freshwater
Transboundary
water crossing political borders
Stores
these are the stores of water, places where the water is held. For example, the oceans
Fluxes
this is the flow of water between the stores (and the rate/speed of flow)
Processes
the physical factors which drive the fluxes of water between the stores
The Hydrological Cycle
- Example of a closed system. No water is added to the global water budget, and none is removed
- The system is driver by solar energy and gravitational potential energy
- The water is held in different states (solid, liquid, gas) and stores which vary for both human and physical factors
Residence times
these are the average times a water molecule will spend in a reservoir or store
Fossil water
nonrenewable and reachable water for human use (e.g., deep groundwater found in the Sahara Desert
Drainage basin cycle
- subsystem within the global hydrological cycle
- It is an open system with eternal inputs and outputs that cause the amount of water in the basin to vary over time
Antecedent
a thing or event that existed before or logically proceeds another
Water budgets
- annul balance between inputs (precipitation) and outputs (the channel flow and evaporation)
- More outputs than inputs = deficit (then causes droughts)
- More inputs than outputs = surplus (causing flooding)
- more than enough water (this is called a positive water balance)
- not enough water (this is called negative water balance)
River Regimes
average annual pattern of discharge of a river, measured at a particular point
Storm Hydrograph
a graph that shows how a river changes as a result of rainfall, it shows rainfall and discharge
Discharge
the amount of water in a river at particular point
Meteorological drought
This happens when long-term precipitation is lower than. It changes for different regions as it is affected by the atmospheric (Brazil)
Agricultural drought
a situation where lack of rainfall or dry soil significantly impacts farming and crop growth (Brazil)
Hydrological drought
situation where there’s a reduction in the water supply, specifically impacting water levels in rivers, lakes, reservoirs, and groundwater sources (Egypt)
Socio-economic drought
the impact of water scarcity on human activities and livelihoods (London, California)
Ecosystem functioning
the biological, chemical, and physical processes that take place within an ecosystem