Understanding grid stability
To understand what’s at stake, a quick refresher: Traditional power plants – like those running on coal, gas, or nuclear – provide what’s called “rotational inertia.” Their large spinning generators help stabilize the grid by keeping voltage and frequency steady.
By contrast, the power electronics that connect solar panels and wind turbines to the grid don’t naturally provide the same stabilizing effect. So, as the share of renewable electricity grows, the system becomes more sensitive to sudden shifts in supply or demand.
When an incident disrupts that balance – if a transmission line goes offline, for example – the voltage and frequency can start to drift. To contain the problem, safety systems isolate the affected area. That’s what happened on 28 April, and it’s why the rest of Europe, including France, didn’t experience a blackout.
This kind of cascading failure isn’t new, nor is it specific to renewable power. Large blackouts have occurred well before wind and solar took off – in Italy, Canada, and the US in 2003, India in 2012, Turkey in 2015, Australia in 2016, and more recently in Texas, Spain, and Pakistan.
Some blackouts stem from “low voltage” issues during high demand. More recent challenges come from “high voltage” conditions, which can arise when demand is low and decentralized sources like wind and solar are generating more than the system can easily absorb.