170
D. Wrzesi´ nski
A
B
C
D
E
Fig. 9.2 Monthly flow coefficients – Pardé coefficients (PC), share of groundwater supply (H ground )
and sequences of hydrological periods of selected rivers of particular types of regime: A – nival
poorly formed, B – nival moderately formed, C – nival well-formed, D – nival-pluvial, E – pluvialnival; Types of periods: 1 – deep low-water, 2 – average low-water, 3 – low low-water, 4 – normal
period, 5 – low high-water, 6 – average high-water, 7 – high high-water, 8 – very high high-water
(after [13])
D. Wrzesi´ nski
A
B
C
D
E
Fig. 9.2 Monthly flow coefficients – Pardé coefficients (PC), share of groundwater supply (H ground )
and sequences of hydrological periods of selected rivers of particular types of regime: A – nival
poorly formed, B – nival moderately formed, C – nival well-formed, D – nival-pluvial, E – pluvialnival; Types of periods: 1 – deep low-water, 2 – average low-water, 3 – low low-water, 4 – normal
period, 5 – low high-water, 6 – average high-water, 7 – high high-water, 8 – very high high-water
(after [13])