4 Flashcards
Stores in the Hydrological Cycle
Soil, Organisms, Groundwater (aquifers), Lakes, Rivers, Atmosphere, Glaciers, Ice Caps.
Transfers in the Hydrological Cycle
Flooding, Surface Runoff, Infiltration, Percolation, Stream-flow, Currents, Advection.
Transformations in the Hydrological Cycle
Sublimation, Evaporation, Precipitation, Evapotranspiration, Condensation, Melting/Freezing.
Distribution of Earth’s Water
97% Saltwater. 3% Freshwater.
Ocean Circulatory Systems
Due to differences in water density. Warm water holds less salt so rises, and is less dense. Cold water holds more salt so sinks, and is more dense. As warm water rises it is replaced by cold water, as cold water rises, it is replaced by warm water.
Human Impact on the Hydrological Cycle
Withdrawals for domestic use.
Discharges, adding pollutants.
Changing the speed of which water flows and where it flows, dams etc.
Diverting rivers or sections of rivers.
Impermeable surface reduces infiltration and increases surface-run-off, urbanisation.
Ocean Currents and Climates
Water has higher specific heat capacity than land so cools down and warms up more slowly. Coastal locations have more mild climates.
Warm currents allow more northen places to be warmer, NW Europe with warm gulf stream.
Cold currents allow hotter places to be more mild, Benguela current moderates climate of Namibian desert
Cold Currents
Poles to Equator
Humboldt - off the coast of Peru
Benguela - off the oust of Namibia, Southern Africa.
Warm Currents
Equator to Poles
Gulf Stream - Northern Atlantic Ocean
Angola - off the coast of Angola.
Water Stress
The demand for water exceed the available amount during a certain period or when poor quality restricts its use.
Water Scarcity
The lack or deficiency of safe water supplies.
Irrigation
Water used to water crops.
Ways to Enhance Water Supplies
Reservoirs
Redistribution
Desalination Plants
Artificial recharge of aquifers
Rain water harvesting.
Sharing Water Supplies and Conflict
Phytoplankton