Lecture 9: Water Cycle
Water cycle
Continuous movement of water on, above, and below earth’s surface
while on the move, water is changing states between liquid, vapor, and solid
happening in the blink of an eye and over millions of years
closed system
amount of water is constant
no water is created or destroyed
only transforms/moves between different resivors/environments
Benefits of closed system
accounting of fluxes
mass balance (water budget)
climate change evalutation
Fluxes of the hydrologic cycle
evaporation
precipitation
runoff
infiltration
What energy drives the movement of these fluxes
sun = heat energy
evaporation
earths revolution, rotation, and tilt
temp and pressure gradients
wind energy
temp and pressure gradients
earths revolution, rotation, and tilt
colling with altitude
condensation/precipitation/rainfall/snow
gravity
precipiation falls on surface
gradient in temp and gradient in pressure drives the flow
Reservoirs of water cycles
temp storage locations
three main Reservoirs of water cycle
atmosphere (clouds)
evaporation brings water to atmosphere through vapor, which then condenses
clouds then move and transports water
water comes down as precipitation
surface (rivers, lakes, oceans, glaciers, wetlands)
evaporation takes away
precipitation brings water back
runoff carries water to a different surface
subsurface (soils and aquifers)
soils:
water seeps as infiltration, precolates
recharges aquifers
Aquifers:
can recharge surface water through base flow
which then is recharged by more surface water
discharged into ocean