water during the drought. A network of 36 monitoring wells at 11 sites was installed around the island to measure the amount of water depleted from the aquifer. By the end of the drought in June 1998, the maximum thickness of the freshwater lens was about 45 feet in some wells, while one site measured a thickness as low as 18 feet. Following the resumption of the rainy season, the thickness of the lens increased by up to 8 feet in some areas, indicating that the recharge rate of freshwater lenses on atolls and small islands responds rapidly to changes in precipitation and groundwater pumping rate. Effects of sea level rise Many of the atolls that support freshwater lenses are only a few meters above sea level and as such they are at risk of inundation due to sea level rise. However, an arguably more pressing issue facing these small islands is the intrusion of saltwater on the freshwater aquifer. As more and more of the potable groundwater is salinized, the populations of these islands may see a substantial reduction in available water resources. Smaller islands are at a far greater risk of extensive saltwater intrusion due to a non-linear relationship between island width and thickness of the freshwater lens. A 40 cm rise in sea level can have a drastic effect on the shape and thickness of the freshwater lens, reducing its size by up to 50% and encouraging the formation of brackish zones. Saline plumes can form at the bottom of the freshwater aquifer when the lens thickness is compromised by drought and saltwater intrusion. Even after a full year of groundwater recharge, the saline plume may not completely dissipate. Sea level rise will likely lead to sustained and possibly irreparable damage to freshwater lenses due to an increase in cyclone-generated wave washover, rendering many islands uninhabitable with the loss of potable water. References Hydrogeology