“…the potential for extreme storms) is perhaps more important to river (Foster, 2001;Hiscock et al, 2011;Iverson and Major, 1986;Loveless et al, 1996;Macdonald et al, 2012;Schweckendiek et al, 2014;Wols and van Thienen, 2014 (Hemer et al, 2013;Woolf and Wolf, 2010) Moderate Increased storminess (severity, frequency, sequence) (Karunarathna et al, 2014) Low Wave direction (mean) Low Salinity (Holliday et al, 2010) Low Acidity (Turley et al, 2010) Low Temperature, solar radiation and drought Earth embankments and other 'soil' and 'vegetation'-based infrastructure Extremes of temperature (cold, hot, extreme dry periods) (Blenkinsopp and Fowler, 2007;Burke et al, 2010;Karoly and Scott, 2006;Murphy et al, 2009;Rahiz and New, 2013;Tham et al, 2011;Vidal and Wade, 2009) infrastructure than changes in mean flows. This is because changes in the morphology of the catchment is most responsive to individual storm events and any associated increased erosion (including scour around bridges, embankments, bends, etc.)…”