Water Stewardship Information Sources

Citation Fleming, SW and Quilty, EJ. 2006. Aquifer responses to El Nino-Southern Oscillation, southwest British Columbia. Ground Water 44:595-599.
Organization Environment Canada
URL https://info.ngwa.org/GWOL/pdf/060181491.pdf
Abstract/Description or Keywords We used climatological composite analysis to investigate El Nin˜o–Southern Oscillation (ENSO) signals in
long-term shallow ground water level observations from four wells in the lower Fraser Valley of British Columbia.
Significance of differences between warm-phase, cold-phase, and neutral climate states was assessed with a Monte
Carlo bootstrap technique. We also considered time series of local precipitation and streamflow for comparison.
Composite annual hyetographs suggest that ENSO precipitation impacts are largely limited to winter and spring,
with higher and lower rainfall occurring, respectively, under cold-phase and warm-phase episodes. This is consistent
with prior work in the region and is found to be directly reflected in both streamflow and ground water level
data. The mean magnitude of ENSO terrestrial hydrologic anomalies can be up to ~50% of the average seasonal
cycle amplitude. ENSO does not appear to systematically affect annual hydrometeorological cycle timing in this
study area. However, relative to the surface hydrologic systems considered, aquifers are observed to retain a stronger
memory of seasonal ENSO-related precipitation anomalies, with changes potentially extending through the
following summer, presumably reflecting storage effects. Most responses appear to be somewhat nonlinear.
Information Type article
Regional Watershed Lower Fraser
Sub-watershed if known
Aquifer #
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