Water Cycle Flashcards
5 Stores of Water
Cryosphere (2/3) Atmosphere (0.04%) Lithosphere (1.7%) Terrestrial (includes biosphere) (30%) Oceanic
Process of Condensation
Air cools, holds less water vapour
Dew point temperature
Water vapour loses energy to surroundings
Condensation nuclei needed
When does condensation occur?
Volume of air increases but no heat is added
Temperature of air reduces below dew point but volume remains constant
Process of Evaporation
Water uses energy from surroundings, latent heat, to become a gas
What does rate of evaporation depend on?
Amount of solar energy
Air temperature
Humidity of air (rate decreases close to saturation)
Availability of water
Cloud Formation
Evaporation Convection Air expands as it rises- lower pressure of atmosphere Saturation- dew point temperature Condensation When too heavy, precipitation occurs
3 way cloud formation begins
Topography- air forced to rise over hills
Sun’s energy heats ground- latent heat
Warm air meets cold air- warm air rises
Input in the Drainage Basin System
Precipitation
Flows/ Transfers in Drainage Basin System
Interception Stem Flow Surface Runoff Infiltration Through Flow Percolation Channel Flow Ground Water Flow
Storage in Drainage Basin System
Surface Storage Soil Water Storage Channel Storage Groundwater Storage Vegetation Storage
Outputs in Drainage Basin System
Transpiration
Evaporation
River Runoff
Water Balance Equation
P = Q + E + ΔS
P= Precipitation Q= Runoff E= Potential Evapotranspiration ΔS= Change in Groundwater Storage
P > Q + E
Positive water balance
ΔS increases
P < Q + E
Negative water balance
ΔS decreases
Natural factors impacting shape of a storm hydrograph
Size of drainage basin
Topography
Rock and soil type