Summer upwelling plunges nearshore temperatures ten degrees
July 23, 2026
Nearshore water temperatures have dropped sharply to 16.5°C this week — a plunge of more than ten degrees from the dangerous highs of a month ago, when tributary streams were pushing the thermal limits for cold-water fish. The shift is driven by a classic summer upwelling: persistent southwesterly winds push the warm surface layer offshore, pulling cold, deep water up along the shoreline in its place. The change can be dramatic — sometimes dropping temperatures ten degrees in a single day.
strandings documented from Milwaukee Bay south to Wind Point through June fit this pattern closely. These introduced forage fish are acutely vulnerable to the thermal shock that upwelling delivers—the phenomenon was implicated in the catastrophic beach die-offs of the 1960s that ultimately prompted the stocking of Pacific salmon as a biological check on their population. For stressed by heat in tributary streams all summer, the cold plume offers a brief reprieve — though it is temporary, a seasonal rhythm rather than a rescue.
combined sewer system is currently in significant non-compliance with its Clean Water Act permit, meaning that during heavy rain events, untreated sewage and stormwater are still being discharged directly into receiving waters. The Menomonee River, one of the two main river systems draining into this shoreline stretch, carries an official impairment listing — a formal acknowledgment that it is not meeting basic water quality standards. Giant mayfly nymphs are exquisitely sensitive to low dissolved oxygen and fine-sediment quality; the same conditions that once wiped the species out regionally are, in a less acute form, still being generated by overflow events today.
The giant mayflies have returned to a system that has not yet returned to them.
That asymmetry is the defining ecological tension of this moment on the riverfront. Giant mayflies are recolonizing the margins of a recovery that remains incomplete, and whether these populations persist and expand or contract back will be determined in large part by what happens in the sediment over the next several years — how often anoxic pulses reach the river bottom, how much fine organic waste accumulates, and how reliably cool, oxygenated conditions hold through summer. The species is doing the work of a bioindicator whether we ask it to or not.
The broader ecoregional context matters here too. This riverfront sits within the
Lake Michigan Lacustrine Clay Plain
, a landscape shaped by glacial lake clays that drain slowly, concentrate runoff, and amplify the downstream effects of urban impervious surfaces during storm events. That geology is not incidental: it is why combined sewer overflows here carry such ecological weight, and why summer storm intensification — already a documented trend in the Great Lakes region — poses a compounding threat. As the season's heavier rains arrive, the sightings record here will become a real-time legibility test for how much the system can absorb before the recovery signal at the riverfront dims again. Watch the emergence windows carefully through July.