“…The past decade has seen a preponderance of research on the link between interannual and interdecadal climate oscillations such as ENSO and PDO, respectively, and a wide variety of hydrological processes. These studies range from an examination of the correlation between these signals and the magnitude and timing of snowmelt runoff in Oregon [ Beebee and Manga , 2004] and assessment of the correlation between rainfall erosivity and ENSO [ D'Odorico et al , 2001] to direct examination of interannual climate oscillation‐precipitation relationships [ Rajagopalan and Lall , 1998; Kwon et al , 2006], interdecadal climate oscillation‐precipitation relationships [ Lucero and Rodríquez , 1999], and interdecadal climate oscillation‐streamflow relationships [ Gutiérrez and Dracup , 2001]. Little research, however, investigates the relationship between climate oscillations and groundwater resources hypothesized by Rodell and Famiglietti [2001].…”