Projections of future changes to flood risk resulting from the combined effects of natural climate variability and anthropogenic climate change typically have high uncertainty, due to uncertainty in both the atmospheric forcings and the processes by which rainfall is converted to runoff. In this paper we test for non-stationarity of the most extensive annual maximum (AM) streamflow database compiled...
Financed by the National Centre for Research and Development under grant No. SP/I/1/77065/10 by the strategic scientific research and experimental development program:
SYNAT - “Interdisciplinary System for Interactive Scientific and Scientific-Technical Information”.