The water cycle and water insecurity Flashcards

1
Q

Water stress

A

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

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2
Q

Water scarcity

A

between 500-1,000m3 (renewable) per capita per year, usually open tension, and conflict

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3
Q

Absolute water scarcity

A

renewable water sources are very low (less than 500m3 per capita), resulting in widespread restriction on use

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4
Q

Economic water scarcity

A

when access to water is limited by capital, technology, and governance

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5
Q

Physical water scarcity

A

more than 75% of a countries or regions population water is being used

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6
Q

Saltwater encroachment

A

when salt water contaminates freshwater

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7
Q

Transboundary

A

water crossing political borders

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8
Q

Stores

A

these are the stores of water, places where the water is held. For example, the oceans

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9
Q

Fluxes

A

this is the flow of water between the stores (and the rate/speed of flow)

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10
Q

Processes

A

the physical factors which drive the fluxes of water between the stores

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11
Q

The Hydrological Cycle

A
  • 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
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12
Q

Residence times

A

these are the average times a water molecule will spend in a reservoir or store

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13
Q

Fossil water

A

nonrenewable and reachable water for human use (e.g., deep groundwater found in the Sahara Desert

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14
Q

Drainage basin cycle

A
  • 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
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15
Q

Antecedent

A

a thing or event that existed before or logically proceeds another

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16
Q

Water budgets

A
  • 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)
17
Q

River Regimes

A

average annual pattern of discharge of a river, measured at a particular point

18
Q

Storm Hydrograph

A

a graph that shows how a river changes as a result of rainfall, it shows rainfall and discharge

19
Q

Discharge

A

the amount of water in a river at particular point

20
Q

Meteorological drought

A

This happens when long-term precipitation is lower than. It changes for different regions as it is affected by the atmospheric (Brazil)

21
Q

Agricultural drought

A

a situation where lack of rainfall or dry soil significantly impacts farming and crop growth (Brazil)

22
Q

Hydrological drought

A

situation where there’s a reduction in the water supply, specifically impacting water levels in rivers, lakes, reservoirs, and groundwater sources (Egypt)

23
Q

Socio-economic drought

A

the impact of water scarcity on human activities and livelihoods (London, California)

24
Q

Ecosystem functioning

A

the biological, chemical, and physical processes that take place within an ecosystem

25
Ecosystem resilience
refers to the capacity of an ecosystem to recover from disturbance or withstand ongoing pressures. Levels vary, however desert and semi-arid ecosystems tend to be the most resilient
26
Flash floods
- Occurs quickly and unexpectedly after heavy rainfall, often with little infiltration and rapid runoff. - Very dangerous due to their sudden onset and potential for significant damage. - Example: 2013 Sardinia floods caused by thunderstorms resulted in 18 deaths and $1.14 billion in damage.
27
Monsoons
- Cause: Seasonal change in wind direction. - Impact: Heavy rainfall in India and Southeast Asia between April and September. - Rainfall Distribution: 70% of average rainfall occurs in 100 days.
28
Snowmelt
* Impact: Snowmelt in high latitudes and mountain areas can increase river capacity. * Melting Pattern: Melting snow in late spring primarily affects Asia and America. * Glacial Outbursts: Glacial outbursts, known as jokulhlaups, can occur in regions like the Himalayas and Iceland, releasing large volumes of meltwater.