The catchment area from which a river
system obtains its water. An imaginary
line called the WATERSHED delimits one
drainage basin from another.
Storm hydrographs
FLASHY
Short lag time
steeper drainage basin
lots of surface runoff
underlying rock
less percolation
urban areas
less trees
less interception
ploughing fields
downhill
more tributaries
SUBDUED
Labelling
lag time
the time delay
between maximum
rainfall amount and
peak discharge.
rising limb
As the water enters the drainage basin
the discharge rises- there's a delay due
to overland flow and interception
base flow
the starting and finishing level
receding limb
shows the fall in the discharge back to the base level
peak discharge
indicates the highest flow in the channel
type of hydrograph is determined by relief, rock and soil
type, vegetation, land use, weather, urbanisation,
drainage basin density, drainage basin shape and size
Long profile
River rejuvenation
significant breaks in slopes (knick
points) along a river's long profile- may
be due to rejuvenation
illustrates the changes in the altitude of the course of the river from
its source, along the entire length of its channel to the river mouth.