Onondaga Creek crashes toward drought as an airport's pollution load looms larger
Onondaga Creek has fallen fast over the past two weeks.1 At the Dorwin Avenue gage, flow dropped from 43.6 to 18.8 cubic feet per second and gage height slid from 2.43 to 1.57 feet, tracking a week in which the county's abnormally-dry footprint jumped from a quarter to 85 percent of its land area.1, 2 Syracuse Hancock Airport, eight kilometers off, has logged only 1.5 inches of rain this month against a normal of just over three, with highs running a couple of degrees warm.3 The watershed above the gage covers only 88.5 square miles, small and quick to respond, which is exactly why a rain deficit that a larger river would barely notice can knock this creek down by more than half in fourteen days.1
The timing is unfortunate. The creek's upper and middle reaches are already listed as impaired and are still waiting on a federal pollution budget.4 Less water moving through the same channel means whatever nutrient and organic load it carries has less flow to dilute it, and less turbulence to keep it oxygenated, though the actual dissolved-oxygen and water-quality readings needed to confirm that effect here aren't in hand.
The local insect records can't fill that gap. A handful of mayfly observations came in across Onondaga County this summer, but they sit apart from the story: and its close relatives were all logged on a single day in late June near Cicero, well off Onondaga Creek, while scattered single records of and came from Skaneateles, Oswego, Fabius and Moravia.5 All are community-science sightings still awaiting identification review, and each one marks a species being present at a spot on a date — not abundance, not condition, not a trend. The clean-water reputation mayflies carry as a group doesn't transfer neatly to this particular mix either: Caenis tolerates silt and low oxygen, and Callibaetis is a still-water genus. None of these records fall on the impaired reach, so none of them can speak to what a falling, warming creek is doing to it.
What does change the calculus is the Syracuse Hancock International Airport discharge, which entered this month already flagged for a biochemical oxygen demand violation that has tripled twice in three quarters, a trajectory covered in an earlier report on the airport's oxygen-demand violation.6 Less water in the receiving creek means the same permitted discharge has less flow to dilute into, a concern worth watching even without direct downstream water-quality measurements yet in hand. The airport is also the subject of a SEQR determination notice tied to its 2040 expansion, which puts a facility with an active, worsening water-quality violation at the center of a live development decision on a waterway that is currently running at less than half its normal flow.7
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