“…These rises are interpreted as a response to episodic pulses of recharge resulting from substantially above-average precipitation during the 2004-05 winter (Soule, 2006;Mirus and Nimmo, 2013). These rapid rises are consistent with preferential flow paths that allow recharge to reach the water table quickly (Thordarson, 1965;Ebel and Nimmo, 2009). Previous estimates of recharge to the water table on Rainier Mesa range from 5 (Belcher and others, 2004) to 50 millimeters per year (mm/yr) (Russell and Minor, 2002).…”