1.1 Hydrology and fluvial geomorphology: the drainage basin system Flashcards
What is a drainage basin
A drainage basin is the area drained by a river and its tributaries.
What are inputs to a drainage basin
Inputs are the addition of water to a drainage basin in the form of precipitation. It can occur in a number of forms (rain, snow, hail, etc.)
What are stores in a drainage basin
Stores are where water is held in some part of the drainage basin for any length of time.
What are flows in a drainage basin
Flows refer to the movement/transfer of moisture in a drainage basin
What are outputs in a drainage basin
Outputs are the losses of water from a drainage basin
Define precipitation
Precipitation is any liquid or frozen water that forms in the atmosphere and falls back to the Earth.
Define evapotranspiration
Evapotranspiration refers to the combined loss from both evaporation and transpiration.
Define evaporation
Evaporation is the loss of water from the land surface and bodies of water as it transfers from a liquid to a gaseous sate (water vapour) by application of heat.
Define transpiration
Transpiration is the loss of water vapour from the stomata in the leaves of plants and trees.
Define river discharge
River discharge is the volume of water being discharged by a river.
Normally expressed as the volume of water passing a point in the river channel in a given unit of time. This is commonly the number of cubic metres per second – “cumecs”
Define interception
Interception is the precipitation which is intercepted on its way to the land surface by leaves, plants, and trees
Define soil water
Soil water is water retained within the gaps and pore spaces in the soil.
Define antecedent moisture
Antecedent moisture is the moisture retained in the soil before a rainfall event
Define surface water
Surface water is water that is stored on the surface in the form of puddles, streams, and lakes – often above impermeable surface or saturated ground
Define groundwater stores
Groundwater stores is water that has percolated downwards and is held in gaps such as cracks, joints, bedding planes, fault lines, and pore spaces in rocks in the underground aquifer.