The areal characteristics of a rain storm are represented by a-
(i )Depth area duration (DAD) relationship
Depth of rainfall at a rain gauge station is called point rainfall.
A depth area duration curve expresses graphically the relation between progressively decreasing average depth of rainfall and progressively increasing area from the centre of the storm outward to its edge for a given duration of rainfall.
For a rainfall of a given duration, the average depth decreases with the area is an exponential function given by
¯P=P0e−KA"
¯P=Average depth in catchment over area A (km2)
P0=Highest amount of rainfall in catchment at the storm curve.
k,n=Constant.
(ii) Double mass curve:
Inconsistency of record is corrected by using double mass curve technique.
Thus after correction, the previous record becomes consistent with present day environmental and land use condition.
Double mass curve plots between accumulated precipitation of the station (i.e. ∑Px) on y axis v/s the accumulated values of the average of the group of base stations (i.e. ∑Pavg)
Some of the common cause for inconsistency of the records are
Shifting of rain gauge station to a new location.
Neighbourhood of the station undergoing a marked change.
Replacement of old instrument by new one.
Change in the ecosystem due to climate such as forest fires, landslides etc.
Occurrence of observational error from a certain data.