For the RMI as a whole, the supply of natural freshwater is severely limited. The primary source of freshwater is rain which (due to the low elevation of the atolls and islands) soaks directly into the soil and disperses into saltwater which permeates atoll subsoils. In some favourable locations some of the freshwater may accumulate in a Ghyben-Herzberg lens which floats on the saltwater below and can be accessed with wells (SOPAC 1996).
There is a rainfall gradient, with heavier rainfall in the southern atolls and islands (typically in excess of 100 inches per annum) and less rainfall in the northern atolls and islands (typically less than 100 inches per annum).