Freshwater Change and the Hydrologic Cycle (module 3) Flashcards
Give the % of Earth’s water that is freshwater and the % of freshwater that is easily accessible for human use
- 3% of Earth’s surface water is freshwater
- 0.009% of Earth’s surface water is usable and available
Explain where most accessible water comes from globally, and where Vancouver’s water supply comes from
Vancouver - Capilano, Seymour, Coquitlam watershed
Globally - surface water sources such as rivers, lakes, and reservoirs, snow and land ice, glaciers, ice sheets, ice caps, ponds, streams
Label the natural hydrologic cycle with respect to the stores/pools of Earth’s water and the main processes/fluxes that move water through the cycle
Stores- oceans, ice and snow, groundwater, surface water, lakes, atmosphere
Main fluxes - evaporation, transpiration, sublimation, condensation, precipitation, infiltration, runoff, surface flow
Give at least 2 examples of ways in which human actions can alter the natural hydrologic cycle
- Urbanization (less infiltration, increased surface runoff)
- Dams ( altered flow dynamics)
- Deforestation (less infiltration)
- Accelerating ice discharge
Identify and give an example of the three causes of major regional trends in freshwater storage
- Climate Change ex. changes in precipitation patterns, temperature, and evaporation can impact freshwater storage in a region
- Human activities ex. dam construction impacts downstream water availability
- Land use changes ex. urbanization, reduces infiltration
Distinguish between “blue water” and “green water” and explain why the freshwater planetary boundary was updated in 2022 to include green water
Blue water - Freshwater available for human use (rivers, lakes, reservoirs)
Green water - Freshwater available for ecological functions (terrestrial precipitation, evaporation, and soil moisture)
- approach to water resource management that considers the connections of terrestrial ecosystems, land use practices, and freshwater availability
Identify the control variables and planetary boundaries for global freshwater use as suggested in 2015 and for green water as suggested in 2022
2015 - Global (max amount of consumption freshwater) - 4000 km3/yr
- Basin (freshwater withdrawal as % of mean monthly river flow) - low flow (25%), intermediate (30%), high-flow (55%)
- 2600 km3/yr
2022 - root-zone soil moisture (<10% of ice-free land area on which root-zone soil moisture is wetter or drier than normal variability in any month of the year)
- 18%
List the steps of the scientific method
- observation
- question
- hypothesis
- experiment
- control/experimental setup
- analysis
- conclusion
Where is Groundwater stored
Aquifers
- only accessible by drilling or pumping from wells