“…1) are highly seasonal as a result of intensive precipitation during the annual monsoon (Klump et al, 2006;Mukherjee et al, 2007;Larsen et al, 2008;Norrman et al, 2008;Berg et al, 2008). Seasonal fluctuations vary considerably both at spatial and temporal scales and range from 2-8 m in the Ganges-Brahmaputra-Meghna (GBM) Delta (BGS and DPHE, 2001), 2-5 m in the Red River Basin (Norrman et al, 2008), 2-8 m in the Mekong Basin (Benner et al, 2008;Berg et al, 2008), and 1-5 m in the Chao Phraya Basin (Suwanlert, 2004). Groundwater abstraction for dry-season irrigation which has taken place since 1970s in the GBM Delta (WARPO, 2000) and more recently in the Irrawaddy Basin and Mekong Delta (Dawe, 2005;FAO, 2006), serves to increase seasonality in shallow groundwater levels.…”