Precipitation intensity effects on groundwater recharge in the southwestern United States

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Abstract

Episodic recharge as a result of infrequent, high intensity precipitation events comprises the bulk of groundwater recharge in arid environments. Climate change and shifts in precipitation intensity will affect groundwater continuity, thus altering groundwater recharge. This study aims to identify changes in the ratio of groundwater recharge and precipitation, the R:P ratio, in the arid southwestern United States to characterize observed changes in groundwater recharge attributed to variations in precipitation intensity. Our precipitation metric, precipitation intensity magnification, was used to investigate the relationship between the R:P ratio and precipitation intensity. Our analysis identified significant changes in the R:P ratio concurrent with decreases in precipitation intensity. The results illustrate the importance of precipitation intensity in relation to groundwater recharge in arid regions and provide further insights for groundwater management in nonrenewable groundwater systems and in a changing climate.

Figures

  • Figure 1. Site map illustrating locations of groundwater observation wells.
  • Figure 2. The cumulative rate of change in groundwater elevations (dh/dt) (in blue) and the timing of the maximum Tc statistic indicating a significant (p < 0.001) change in the behavior of dh/dt (in orange). Panels correspond to wells identified in Table 1 and Figure 1.
  • Table 1. Well information.
  • Table 1. Cont.
  • Figure 3. Monthly ratios of recharge (R) to precipitation (P). It is important to recognize the influence of infiltration lag, which produces high ratios of R/P on a monthly time scale.
  • Figure 4. Double mass curves illustrating sum of precipitation (P) versus sum of recharge (R). The significant change in the R/P ratio is illustrated as a vertical orange line. The step pattern in the DMC is typical of episodic recharge.
  • Figure 5. Intensity-Duration-Frequency curves preceding the change in the R/P ratio (solid line) compared to posterior IDF curves for 3-, 6-, 12-, 24-, 36- and 48-h event durations. In general, the observed intensity for posterior precipitation events were lower than preceding precipitation events.
  • Table 2. Precipitation intensity magnification as estimated using Equation (8).

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CITATION STYLE

APA

Thomas, B. F., Behrangi, A., & Famiglietti, J. S. (2016). Precipitation intensity effects on groundwater recharge in the southwestern United States. Water (Switzerland), 8(3). https://doi.org/10.3390/w8030090

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