The decrease in conductivity was especially large in the Bayou, likely because freshwater diluted the seawater at that site. Conductivity changes in the stream are more difficult to understand. Different sources of waters within the stream, such as groundwater or surface run-off may have different amounts of dissolved minerals, and therefore different conductivities. We hypothesize that on the day not following a rain event, the stream had more groundwater inputs, which appear to have higher conductivity than the stormwater. We can also infer from the temperature data that the water had been in the stream channel long enough to warm up. Water temperature was lower following rain, because rainfall was relatively cold, and there was little sun to warm the land and