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Factors affecting the drainage basin and storm hydrographs
Descripción
Mind map of all the factors which affect processes within the drainage basin and affect the shape/nature of storm hydrographs
Sin etiquetas
rivers
drainage basin
storm hydrographs
as geography
as geography
rivers
a levels
Mapa Mental por
strangelyblue
, actualizado hace más de 1 año
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Creado por
strangelyblue
hace más de 10 años
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Resumen del Recurso
Factors affecting the drainage basin and storm hydrographs
Deforestion
Less trees means less of the water is intercepted or absorbed by trees for evapotranspiration
Deforestation can also lead to less rainfall
Agricultural Practises
Poor practises such as compacted soil from livestock can lead to more/quicker runoff
Soil depth, type and condition
Thin impermeable soil means less infiltration. If the soil is already damp from antecedent rainfall there will be even less infiltration
Urbanisation
More urbanisation means more impermeable surfaces in towns and possibly drains that will move water faster into the river
Lithology
Impermeable rocks means there is less percolation
Vegetation type
Deciduous woodland will suffer more moisture loss than moorland vegetation
Season
In the summer months there is more evapotranspiration, meaning more water will be absorbed by plant life
Amount/intensity of rainfall
More rainfall means more water in the drainage basin
Presence of stores (Lakes, swamps)
Climate
A damper climate means more rain, it can also allow more evapotranspiration
Drainage Basin Density
The more streams in the drainage basin, the more water that reaches the river
Snow Melt
Fast snow melt can increase the amount of water reaching the river
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