Abstract:
Protecting and restoring river flow regimes and hence the ecosystems
that they support by providing environmental flows has become a major aspect
of water resource management in river basins. It is difficult to quantify the
amount of flows that could be removed from a river while maintaining desired
ecosystem conditions. This study focused on to determine the optimum flow that
has to be maintained along the Attanagalu Oya and sufficiency of water to
sustain riverine ecosystem and other requirements with future water demands.
Water withdrawal data for drinking and irrigation were collected from
the Water Supply and Drainage Board and Department of Irrigation, respectively.
Daily flows were generated for past 50 years and for next 30 years by calibrating
and validating the HEC-HMS 3.4 model for the Attanagalu Oya catchment.
Simulated stream flows were characterized using 36 different hydrological
parameters separately for the past 50 years and for the next 30 years. The Range
of Variability Approach (RVA) targets and rate of non-attainment of the flows for
the past and the future scenarios were calculated using original flows before
water withdrawals.
According to the RVA approach, environmental flow has not being
maintained at present in the Attanagalu Oya. Mean rate of non-attainment of the
indicators of Hydrologic Alteration (IHA) groups after water withdrawals vary in
between 12% to 80%. If the rainfall pattern of the next thirty years shows the
maximum rainfall of past fifty years, the mean rate of non-attainment would be
45%. Hence, any development project that deal with water withdrawal or any
damming across the Oya needs broad analysis of environmental impacts due to
changes in flow regimes that could have an adverse impact on the ecosystem
and associated functions along the river.