“…First, the 1982 spike, with EC levels reaching over 10,000 (dS/m), can be attributed to a storm surge in the same year, which caused heavy loss of life (Dube 2012). Similarly, the 2007 to 2011 spikes can be attributed to storms Sidr in 2007 (Pal et al, 2016) and Ayla in 2009 (Rasheed et al, 2014;Haldar et al, 2017) that resulted in saltwater intrusion into the river system. Similarly, during 2008, (Fritz et al, 2009) storm Nargis primarily affected the Myanmar deltaic region, but also the coast of Bangladesh, which can be considered as a link between the two spikes in 2007 and 2009 in Figures 5-7.…”