whats on the x and y axis on the storm hydrograph
x axis = time
y axis= river discharge
what is discharge
the volume of water flowing through a cross section of river during a time period
what is lag time
the time period between peak rainfall and peak discharge
effect of direct channel input
very small amount of rainfall falls on river itself
what are the two types of overland flow
-infiltration excess overland flow
-saturation excess overland flow
what is infiltration excess overland flow
when the rain is falling more quickly than the infiltration rate
what is saturation excess overland flow
when soil spaces are so full of water that no more rain can be absorbed
what is the level of discharge before the storm called
the antecedent discharge
different types of a storm hydrograph
-peak rainfall
-lag time
-peak discharge
-falling and rising limb
-normal flow
how does the graph vary between a storm hydrograph and a river regime
river regime usually graphed over a year
storm hydrograph show discharge changes over short period of time
what does the storm hydrograph shape depend on
-shape
-size
-drainage density
-rock type
-soil and vegetation
-relief
what are hydro graphs with very steep limb, especially rising limb, high peak discharge and short lag time called
flashy
what are gently inclined limbs with low peak discharge and long lag time hydro graphs called
delayed or flat
what key concept links with storm hydrographs
planners in managing land use
what is measured in a bar graph
rainfall
what is measured in a line graph
-discharge