Chapter 4 Flashcards
Water budget
A quantitative estimate of the amounts of water in storages and flows of the water cycle
What drives the water cycle
Energy from solar radiation and the force of gravity
Water: renewable and non-renewable
Depending on where it is stored, can easily slide from being renewable to non-renewable if poorly managed
Renewable: atmospheres, rivers
Middle ground: groundwater aquifers
Non-renewable: oceans and icecaps
Aquifer
A layer of porous rock, sand or gravel underground that holds water. In aquifers, it takes longer than a human lifetime to replenish the water extracted
Water cycle - transfers
Stays in the same state: advection (wind-blown movement), flooding, surface run-off, infiltration and percolation (when water runs into and through soil or rocks), stream flow and current
Water cycle - transformations
Evapotranspiration (liquid to water vapour), condensation (water vapour to liquid), freezing (into solid snow and ice)
Water cycle - storages
Oceans, soil, groundwater (aquifers), lakes, rivers and streams, atmosphere, glaciers and ice caps
Human impact on water cycle
Withdrawals (domestic use, irrigation in agriculture/industry)
Discharges (adding pollutants to water, chemicals, fertilisers, sewage)
Changing speed at which water can flow/where it flows (building roads, channelling rivers, canalizing, dams, barrages and dykes, reservoirs)
Diverting rivers or sections of rivers (to avoid flood damage, to improve storage)
Canalizing
Straightening large sections of rivers in concrete channels to facilitate more rapid flow through sensitive areas
Flash floods
Occur when rainfall or snowmelt cannot infiltrate the soil and runs off on the surface
Due to land being hard-baked in hot, dry areas, but due to the CITY-based surface (urbanization!!!)
Ocean currents
Movements of water both vertically and horizontally. They move in specific directions and are found on the surface and in deep water
Ocean currents importance
Global distribution of energy
Without them, we could not understand the global atmospheric energy changes
Surface currents
Upper 400m of ocean, are moved by the wind
Earth’s rotation deflects them and increases their circular movement
Deep water currents (thermohaline currents)
Make up 90% of ocean currents and cause the oceanic conveyor belt
Deep water currents key ideas
Due to differences in water density caused by salt and temperature
Warm water can hold less salt than cold water so is less dense and rises - cold water holds more, sinks
Upwellings
When warm water rises, cold has to come up from depth to replace it
Downdwellings
When cold water rises, it has to be replaced by warm water
Cold ocean currents
Runs from the poles to the equator (e.g. Humboldt Current and Benguela Current)
Warm ocean currents
Flow from the equator to the poles (e.g. Gulf Stream and Angola Current)
Water and its effect on temperature
Water has a higher specific heat capacity than land
Water masses heat up and cool down more slowly than landmasses
Land CLOSE to seas and oceans has a mild climate with moderate winters and cool summers
How ocean currents affect local climate
Gulf Stream moderates the climate of Northwestern Europe, which otherwise would have a sub-arctic climate
(Cold) Benguela Current moderates the climate of the Namibian desert
Humboldt Current impacts the climate in Peru
El Niño Southern Oscillation (ENSO)
A phenomenon in the Pacific Ocean - pressure differences across the ocean is reversed (called the Southern Oscillation)
These pressure differences alter both the directions of the wind and the warm surface current
El Niño Southern Oscillation (ENSO) effects
Local effects - collapse of anchovy fish stocks, massive death of sea birds and storms and flooding in the coastal plain of Peru
Humans use fresh water for…
Domestic purposes (drinking, washing, cleaning), agriculture (irrigation, for animals to drink), industry (manufacturing, mining), hydroelectric power generation, transportation (ships), marking the boundaries between nation states (rivers and lakes)