Moody’s and other rating agencies have begun incorporating climate exposure into municipal credit assessments, noting that repeated infrastructure damage and rising insurance costs can weaken local fiscal positions and, in some cases, contribute to negative outlooks or higher borrowing costs over time.¹²
The Pacific shifts. The storm track follows. Water moves differently. The cost shows up somewhere else—in a premium notice, a bond discussion, or a utility bill.
Which brings the story back to policy, and to the one place where the United States still has leverage before damage becomes debt.
The Federal Emergency Management Agency is built to respond to disasters, but just as importantly, to reduce them before they happen. Programs like BRIC—Building Resilient Infrastructure and Communities—fund drainage upgrades, flood protection, electrical hardening, relocations from hazard zones, and the unglamorous work that prevents small failures from becoming larger ones.
In 2025, that program was canceled. In 2026, a federal court forced its reinstatement, restoring roughly $1 billion in mitigation funding after billions in projects had been frozen or delayed.¹⁰
The interruption matters more than the headline.
Projects delayed are not neutral. A culvert not upgraded this year fails under next winter’s runoff. A drainage system left undersized becomes a recurring problem instead of a solved one. The cost doesn’t vanish during the pause; it compounds into the next season.
At the same time, staffing reductions—thousands of FEMA departures over the past year—have raised concerns about response capacity, not for a single catastrophic event but for the accumulation of smaller ones that require coordination, reimbursement, and follow-through.¹¹
The vulnerability isn’t failure. It’s strain—more things bending at once, more often, for longer.
A strong El Niño would not create that condition. It would align it—bringing a warmer ocean, heavier moisture, storm tracks that lean toward the East Coast, and winter patterns that are less stable than the systems beneath them were designed to handle.
The Pacific is where the signal begins, but it does not stay there. It moves through the jet stream, into the storms, into the snow that does not quite hold and the rain that arrives at the wrong time, into the water that moves faster than the drains can take it and the coastlines that take the hit without the buffer they once had.
By the time it reaches New England, it no longer looks like a climate event. It looks like a series of ordinary problems arriving out of sequence—wet snow on power lines, water backing through a drain, a repair that costs more than the last one, a budget that stretches a little further to cover it.
Most of it will be fixed. It usually is. The street dries, the slope turns green, the culvert gets replaced, and the next storm arrives on a system that is slightly more worn and slightly more expensive to maintain.
Nothing collapses. The town holds. The region holds.
But it does so on different terms than it used to, with less margin, more cost, and fewer places for the stress to go.