by
rescaling a dimensionless regional flood frequency distribution or growth curve, qR(
D;T ),
com-
mon to all sites of the homogeneous region, with the so-called index flood, µi(
D), of the target
site:
bQi(
D;T ) = µi(
D)qR(
D;T ); (1)
where bQi(
D;T ) is the estimated flood quantile, i.e. the T -year flood peak discharge averaged
over duration
D, at site i. The regional growth curve, qR(
D;T
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf