Catchment hydrology - processes of the water cycle Flashcards
What is evaporation
The phase change of liquid to water vapour
Main pathway by which water enters the atmosphere
Latent heat
The energy input of evaporation does not lead to an increase in temperature
Instead the energy is absorbed as latent heat and released later in condensation
Interception
Vegetation intercepts a proportion of precipitation, storing it temporarily on branches, leaves and stems
This water will either evaporate or fall to the ground
Throughfall - rainwater which is briefly intercepted before dripping on to the ground
Stemflow - during prolonged or intense periods or rainfall, intercepted rainwater may flow to the ground along branches and stems
What is infiltration
By gravity into the soil and lateral movement or throughflow to stream and river channels
What is overland flow
Across the ground surface either as a sheet or as trickles and rivulets to stream and river channels
explain flow paths
Overland flow is related to the soils infiltration capacity
When rainfall exceeds the soils infiltration capacity overland flow occur.
Rainfall, regardless of its intensity, always infiltrates the soil, overland flow only occurs when soil becomes saturated and the water table rises to the surface
Saturated overland flow
Geology
Where soils are underlain by permeable rocks, water percolates deep underground
This water then migrates slowly through the rock pores and joints as groundwater flow
This eventually emerges at the surface as springs or seepages
Cryospheric processes
Ablation is the loss of ice from snow, ice sheets and glaciers
Melting, evaporation and sublimation
Meltwater
An important component of river flow in high latitudes and mountain catchments in spring and summer