indicate how much water stored in a drainage basin
shows balance between inputs and outputs
UK example-temperature zone
river regimes vary with physical influence
seasons and climate- eg meltwater or more evaporation- eg indus river(south and central asia) meltwater from himiliyas in spring
geology and soil structure- indus river basin made from impermeable igneous and metamorphic rock- swells quickly- overland saturated flow- highly porous can percolate
factors affecting storm hydrograph
size of drainage basin- larger catch more water but further to travel
shape of drainage basin-circular more likely to have flashy
permeability of rocks and soil- surface run off
vegetation- interception, slow surface run off
land use- ploughed arable farm land(flashier) soil more compact and less vegetation, urbanisation, dams