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Can Hail Damage Solar Panels?

Updated 8 October 20267 min readSolar Energy

Rarely, and almost never in the way people picture it. Module glass is tempered and tested against ice balls fired at it, so ordinary storm hail bounces off. The damage that actually costs output is usually invisible from the roof — cracks in the silicon beneath glass that looks perfect.

Key takeaways

  • Impact energy rises with the cube of stone diameter and the square of its speed, so a stone twice as wide arrives with far more than twice the punch.
  • Module glass is thermally tempered: it is several times stronger than ordinary glass of the same thickness and fails by shattering into blunt fragments rather than shards.
  • Certification testing fires ice balls at eleven points across a module. Passing proves the module survives that specified impact, not any hailstorm.
  • Tilt helps. Only the component of the impact perpendicular to the glass does the damage, so a steeply tilted array is struck more obliquely.
  • The failure mode that matters is a cracked cell under unbroken glass, which shows up as gradually falling output rather than as visible breakage.
On this page
  1. What a hailstone actually delivers
  2. Why the glass usually wins
  3. What the certification test actually proves
  4. The damage you cannot see
  5. What to check after a storm
  6. When hail is genuinely a design problem

What a hailstone actually delivers

A hailstone is a lump of ice arriving at terminal velocity, and the damage it can do is governed by kinetic energy: E = ½mv². Both terms work against the glass as stones grow. Mass rises with the cube of diameter, and larger stones also fall faster, so energy climbs steeply with size.

The arithmetic is worth doing once, because it explains why hail reports are dominated by a narrow band of stone sizes.

Approximate impact energy by stone size
Stone diameterMassApproximate fall speedKinetic energy
15 mm (0.6 in)about 1.6 g17 m/s (38 mph)about 0.2 J
25 mm (1 in)about 7.5 g23 m/s (51 mph)about 2 J — the MQT 17 standard class
35 mm (1.4 in)about 21 g27 m/s (60 mph)about 7.6 J
50 mm (2 in)about 60 g32 m/s (72 mph)about 31 J

Energies calculated from the volume of a sphere of ice at about 917 kg/m³ and the fall speed shown. Fall speeds are approximate, within the ranges published by NOAA's National Severe Storms Laboratory, and vary with stone shape, density and updraft strength; treat the ratios as the message rather than the absolute joules.

Doubling the diameter from 25 mm to 50 mm multiplies the energy by roughly fifteen. That is why a storm producing golf-ball hail is a different event from one producing pea hail, and why "it hailed" on its own says very little about the risk.

Chart of hailstone kinetic energy against stone diameter, rising steeply from a fraction of a joule at fifteen millimetres to roughly thirty joules at fifty millimetres, with the certification test point marked at twenty-five millimetres.Chart of hailstone kinetic energy against stone diameter, rising steeply from a fraction of a joule at fifteen millimetres to roughly thirty joules at fifty millimetres, with the certification test point marked at twenty-five millimetres.
Energy climbs with the cube of diameter and the square of speed. The certification test sits near the lower end of what a serious storm can produce.

Why the glass usually wins

The front sheet of a module is not window glass. It is thermally tempered: heated and then cooled rapidly so the outer surfaces end up in compression and the core in tension. A crack has to overcome that built-in compression before it can start, which makes tempered glass several times stronger in bending than annealed glass of the same thickness.

It also fails differently. When tempered glass does break, the stored stress releases at once and the pane disintegrates into small blunt fragments rather than long shards — which is why a hail-broken module looks like a crazed sheet held together by the laminate rather than a hole.

Cross-section of a photovoltaic module showing the tempered front glass, the encapsulant layer, the silicon cell, the rear encapsulant and the backsheet, with an arrow tracing how impact energy passes from the glass through the encapsulant into the brittle cell beneath.Cross-section of a photovoltaic module showing the tempered front glass, the encapsulant layer, the silicon cell, the rear encapsulant and the backsheet, with an arrow tracing how impact energy passes from the glass through the encapsulant into the brittle cell beneath.
The glass is the armour; the cell beneath it is the fragile part. Energy that the glass does not absorb or spread passes straight into silicon a fraction of a millimetre thick.

Underneath sits the part that cannot be toughened. A silicon cell is brittle, wafer-thin — a slice cut from a grown or cast crystal — and bonded into a polymer encapsulant. The encapsulant cushions it, but a sharp enough impulse through intact glass can still crack the wafer.

What the certification test actually proves

Modules qualified to the IEC 61215 series undergo a hail impact test — IEC 61215-2, test MQT 17. In the standard class, a 25 mm ice ball is fired at about 23 m/s at eleven impact points across the module: the corners, points along the edges, over the gaps between cells, the centre, and above the junction box. Those locations are chosen because they are where the laminate is least forgiving. Larger ice-ball diameters exist as optional, harsher classes for regions where big hail is routine.

Diagram of a module face marked with the impact locations used in hail testing: each corner, points along the edges, the centre of the module, over cell gaps and above the junction box, with a launcher firing an ice ball at the module at a stated speed.Diagram of a module face marked with the impact locations used in hail testing: each corner, points along the edges, the centre of the module, over cell gaps and above the junction box, with a launcher firing an ice ball at the module at a stated speed.
Eleven impact points in the standard class of IEC 61215-2 MQT 17, chosen where a laminate is least forgiving rather than at the easy middle of a cell.

Two things follow, and both get forgotten. Passing the test proves the module survives that impact at those points — it is a qualification threshold, not a guarantee against any storm. And the test uses a standard ice ball on a bench: a real stone may be irregular, denser, driven by wind at an angle, and landing on glass already weathered for a decade.

Those harsher classes are specified before purchase rather than discovered afterwards.

Tilt helps, quietly

Only the component of the impact perpendicular to the glass does the work of breaking it. A stone falling vertically onto a panel tilted at 30° strikes at 30° from the surface normal, and the perpendicular component of its velocity is reduced by the cosine of that angle — with energy scaling as the square of velocity, the normal-direction energy falls by about a quarter.

Vector diagram comparing a hailstone striking a flat panel head-on with one striking a tilted panel, showing the velocity resolved into components perpendicular and parallel to the glass, and the reduced perpendicular component on the tilted panel.Vector diagram comparing a hailstone striking a flat panel head-on with one striking a tilted panel, showing the velocity resolved into components perpendicular and parallel to the glass, and the reduced perpendicular component on the tilted panel.
A tilted panel is struck obliquely. The sliding component does little; only the perpendicular part loads the glass.

Steeper arrays therefore fare better in hail, all else equal — though tilt is chosen mainly for yield, which is its own trade-off and the subject of choosing tilt angle and direction.

The damage you cannot see

Here is the part that costs money. A module can pass a visual inspection and still have lost cells.

A microcrack is a fracture in the silicon wafer beneath unbroken glass. The cell still conducts, so nothing looks wrong, but the crack interrupts the fine metal fingers that carry current across the cell face. Sections of the cell become electrically isolated, and because cells are wired in series, the weakened cell limits the string current — the same mismatch mechanism described in how partial shade affects solar panels, arriving from a different cause.

Close-up of a solar cell face showing fine metal fingers carrying current to the busbars, with a crack running across them. The region beyond the crack is shaded to show that it is electrically isolated and no longer contributing current.Close-up of a solar cell face showing fine metal fingers carrying current to the busbars, with a crack running across them. The region beyond the crack is shaded to show that it is electrically isolated and no longer contributing current.
The crack does not have to break the cell in two. Cutting the fingers is enough to strand whatever lies beyond it.

Cracks also tend to progress. Thermal cycling flexes the laminate daily, and a crack that isolated a sliver of cell after the storm can isolate a larger area two winters later. A module that lost 2% of its output in March may have lost considerably more by its third summer.

What to check after a storm

  1. Take the production data first. Compare daily output against a comparable period before the storm, at similar irradiance. A step change on the day of the storm is the clearest evidence there is.
  2. Compare strings. If two strings share an orientation and only one has dropped, the weather affected them equally and something else did not. Where the system has module-level electronics, the per-module data narrows it further, to individual panels.
  3. Look at the glass, carefully. Crazing, chips at the edges, and a spidery pattern radiating from a point are all worth photographing.
  4. Check the frames and mounts. Hail arrives with wind; bent frames and loosened clamps are ordinary findings and matter for the next storm.
  5. Ask for electroluminescence imaging if output has dropped without visible damage. Passing a current through the module in darkness makes it emit infrared light, and cracked or isolated regions show up black. It is the only practical way to see a microcrack.

If output has fallen and none of this explains it, the systematic hunt in why a system produces less power than expected covers the non-weather causes — and a storm is a good moment to rule out the mundane ones, since soiling and cleaning affect output in the same direction.

When hail is genuinely a design problem

In most climates, hail belongs on the list of things that occasionally happen rather than things that drive design. Where large hail is a recurring seasonal event, it becomes a specification question — impact class, glass thickness, mounting tilt, and whether the array can be stowed at a steeper angle — and all of those are decided before anything is bolted down.

What does not work is improvisation during the storm warning. The useful preparation is a production baseline you can compare against afterwards, which costs nothing and is the difference between knowing and guessing.

Frequently asked questions

How big does hail have to be before panels are at risk?

There is no single threshold, because speed, angle, glass thickness and the stone's density all matter. What can be said is that the energy grows very fast with size: the step from a 25 mm stone to a 50 mm one is roughly a factor of fifteen in impact energy, not a factor of two.

Should I cover my panels when hail is forecast?

In almost all cases the risk of working on a roof in a storm outweighs the risk to the glass. Permanently mounted protection is a design decision made before installation, not something to improvise as a squall line arrives.

My panels look fine after a hailstorm. Can I stop worrying?

Not entirely. Intact glass does not prove intact cells. The reliable signal is production: compare output against the weeks before the storm at similar irradiance, and against any neighbouring string that was not hit.

Does hail damage get worse over time?

Cell cracks often do. Thermal cycling and mechanical flexing can extend a crack or separate contacts across it, so a module that lost a little output after a storm may lose more over the following seasons. This is why a post-storm baseline measurement is worth taking.

Are thicker or specially rated modules worth it in hail country?

Where large hail is a regular event, modules tested to a harsher impact class are a reasonable specification, as is mounting geometry that increases tilt. Both are decisions to make before installation, since neither can be retrofitted.

Sources

Named organisations whose published material underpins this article. Where no link is given, the source is named rather than linked.

Editorial Team

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Last reviewed 8 October 2026. How we research and review