1.0 - Perception Of Water Flashcards
Storage
Where water is held
Processes
The physical mechanisms that drive fluxes
Fluxes
The ways that water changes state i.e. moves around the world.
Open Water System
Both inputs and outputs e.g. drainage basin
Closed Water System
Water has no exit e.g. hydrological cycle water goes (solid ice, water vapour, liquid flow, back to ice).
Water Budgets
Show the balance between water storage and water fluxes. Most water is inaccessible, and some stores can be replenished whilst others can’t
Causes Of Change To Water Budget
Human Activity - Extraction, Reservoirs, Drinking
Climate Change - Evaporation, Precipitation, Melting
Rainfall In The Mid-Latitude
Cold polar air meets warm tropical air from the south, the warm air rises and it cools and condenses to clouds which causes rain e.g. frontal rainfall/mid-latitude depressions.
Rainfall At The Equator
The sun is directly overhead the equator, heating the land and the water/air, creating lower density, causing air to rise, then cool, cloud and condense i.e. convectional rainfall.
Rainfall At The Tropics
Hadley cell causes the air to sink at the tropics, making air pressure high and less clouds form meaning there’s less rain making the ground temperature high, and then no rainfall to cool it down.
Hadley Cell
Warm, moist air rises, to 30 deg N and S of the equator, where air becomes cool and dry and begins to sink as it becomes more dense. It sinks back towards the equator where the air will get warm again and the cycle repeats. The circular motion of these clouds are called trade winds.