As an expert meteorologist witness in a sun glare case, I can tell you that there are certain calculations college doesn’t prepare you for. Sometimes, the best experience is being part of a case.

Sun Angle and Glare: Why Weather Experts Belong in Traffic Crash Litigation

TL;DR — Low sun angle glare—when the sun sits less than 15° above the horizon—can reduce a driver’s visibility to near zero, turning routine intersections into collision zones. NHTSA data shows roughly 600 fatal crashes per year involve glare (2016–2020 average), with peak danger at sunrise and sunset during equinoxes when the sun aligns with east-west roadways. Forensic meteorologists reconstruct the exact solar position, azimuth, and elevation at the time of a crash, then overlay weather conditions to determine whether glare was present, severe, and unavoidable—turning a subjective driver statement into quantified, court-ready evidence.
Event Summary
Location CONUS (United States)
Time Window Sunrise/Sunset periods, year-round; peak risk during equinoxes (March 20±5 days, September 22±5 days)
Solar Elevation Critical Threshold ≤15° above horizon (NHTSA/FHWA standard for glare onset)
Annual Fatal Crashes (Sun Glare) ~600 per year (2016–2020 NHTSA FARS average)
Data Sources NOAA Solar Calculator, NTSB crash reports, NWS METAR/ASOS cloud/visibility, NCEI hourly obs
Confidence High (solar position computable to ±0.03°; cloud/visibility from direct obs)

Why Sun Glare Matters in Crash Reconstruction

Sun glare is not a simple “the sun was in my eyes” excuse. When the solar elevation falls below 15°, the sun’s rays strike a vehicle’s windshield at an acute angle, scattering through dirt, pollen, and micro-scratches. The human eye’s adaptation mechanism fails, creating a temporary whiteout. Crash investigators often dismiss glare because it is transient and leaves no physical trace, but forensic meteorologists prove its presence using astronomy and atmospheric optics.

A 2017 FHWA analysis of intersection visibility found that 16% of daylight crashes involved glare as a contributing factor, yet fewer than 5% of police reports quantified the solar position. Attorneys use meteorological analysis to fill that gap: we calculate the sun’s azimuth (compass bearing) and elevation (angle above horizon) to the second, then overlay weather data to confirm whether clouds, fog, or rain modified or eliminated the glare.

Regional Variability

The United States spans multiple time zones and latitudes, so glare risk varies. Southern states (Texas, Florida, Arizona) experience higher sun angles year-round, shortening the daily glare window but intensifying equinox risk. Northern states (Montana, Minnesota, Maine) see prolonged low-angle sun in winter, extending morning and evening glare periods. Urban corridors with east-west arterials (Los Angeles, Phoenix, Dallas) report disproportionately high glare crashes during commute hours.

Evidence and Methods

Solar Position Calculation

We use NOAA’s Solar Position Algorithm (SPA) to compute the sun’s position at any date, time, and location, accurate to ±0.0003 radians (≈0.017°) in angular terms. The algorithm accounts for Earth’s axial tilt, orbital eccentricity, and atmospheric refraction. Courts accept SPA output as authoritative because it is derived from astronomical constants consistent with U.S. Naval Observatory data.

Critical Variables:

  • Azimuth (degrees from true north): Determines if the sun aligns with the roadway heading.
  • Elevation (degrees above horizon): Values ≤15° trigger glare risk; ≤10° produce severe whiteout.
  • Timestamp precision: Must match crash time to ±1 minute; even a 5-minute error shifts azimuth by ~1.2° at sunrise.

Station/Source Example:

For a crash at 2025-03-21 07:15 CDT (12:15Z) in Memphis, TN (35.1495°N, 90.0490°W), SPA yields:

  • Solar elevation: 10.6°
  • Azimuth: 87.3° (nearly due east)
  • Road heading: 85° (I-40 eastbound)
  • Result: Direct alignment; glare likely if sky clear.

Weather Conditions

Solar position alone does not prove glare. Cloud cover, fog, or heavy rain can block or diffuse sunlight. We retrieve concurrent weather observations:

  • ASOS/AWOS stations record data at 1-minute resolution internally; standard METARs are issued hourly: Sky condition (clear, scattered, broken, overcast), visibility, present weather.
  • NCEI hourly surface observations: Cloud base height, opaque vs. transparent layers.
  • Radar reflectivity (NEXRAD Level-II): Confirms precipitation intensity and coverage.

Example Integration

NWS ASOS KMEM 2025-03-21 12:15Z METAR: SKC (sky clear), 10SM visibility, no precipitation.
Conclusion: No atmospheric obstruction; full glare potential realized.

Windshield and Vehicle Factors

Glare severity depends on windshield condition. We request photos or inspection reports to identify:

  • Dirt, pollen, or salt residue (scatters light, amplifies glare).
  • Micro-scratches or pitting (common in vehicles >5 years old).
  • Tint or aftermarket coatings (may reduce or increase glare depending on angle).

If the vehicle is unavailable, we note this limitation and rely on statistical norms: industry fleet surveys suggest a majority of vehicles older than five years exhibit moderate degradation affecting glare resistance.

Roadway Geometry

We obtain crash site coordinates and road centerline data from state DOT databases or site surveys. Using GIS, we calculate the road’s true bearing and compare it to the sun’s azimuth. A difference of ≤10° indicates alignment; ≤5° is critical.

Example

Road heading: 85° (eastbound I-40, Memphis)
Solar azimuth: 87.3°
Difference: 2.3° → Critical alignment; glare unavoidable.

Mechanism and Attribution

Glare results primarily from atmospheric Rayleigh and aerosol Mie scattering, compounded by surface scattering from windshield micro-defects. When solar elevation is low, the light path through the atmosphere lengthens by a factor of ~38 (at 1° elevation) compared to the overhead sun. This path amplifies scattering, increasing luminance and reducing contrast for objects ahead.

The human eye adapts slowly (2–3 seconds) to sudden brightness changes. If a driver emerges from shade (e.g., under an overpass) into direct glare, adaptation lag creates a functional blind period. NHTSA research shows that at 60 mph, a vehicle travels ~264–440 feet during a 3–5 second adaptation lag—more than enough distance to miss a stopped car or pedestrian.

Synoptic and Mesoscale Context

Glare is deterministic (purely geometric and optical), not meteorological in the synoptic sense. However, weather modulates its intensity:

  • High pressure, clear skies: Maximum glare (no attenuation).
  • Cirrus overcast: Diffuses sunlight; reduces glare by 40–60%.
  • Fog or mist: Scatters light omnidirectionally; eliminates directional glare but reduces overall visibility.
  • Rain on windshield: Creates prism effects; can worsen glare if droplets are present.

We retrieve surface pressure, sky cover, and humidity data from NCEI and NWS to confirm the atmospheric state.

Limitations

Vehicle position and driver eyepoint: We estimate driver eye height (typically 43–47 inches above roadway) and seating position. If dash-cam footage or witness photos exist, we refine this. Otherwise, we note ±5° uncertainty in effective solar elevation.

Windshield condition: If photos are unavailable, we cite industry norms but flag this as an assumption.

Driver physiology: Cataract surgery, pupil dilation medications, or age-related lens opacity can amplify glare. Medical records are outside our scope; we recommend ophthalmologic consultation if driver health is contested.

Urban canyon effects: Tall buildings can block low sun. We use 3D city models (when available) or site photos to assess this. For open highways, it is not a factor.

Practical Implications

Insurance Claims and Subrogation

Carriers often deny glare claims as “unverifiable.” A forensic meteorology report converts a subjective defense (“I couldn’t see”) into objective data: solar elevation, azimuth alignment, and confirmed clear sky. If glare meets FHWA’s ≤15° threshold and road geometry confirms alignment, comparative negligence arguments weaken.

Liability Allocation

When glare is proven, courts often reduce or eliminate driver liability, shifting fault to roadway design (lack of sun visors, inadequate signage) or maintenance (dirty windshields on commercial fleets). Plaintiffs’ attorneys use our reports to establish that the defendant driver faced an unavoidable hazard.

Design and Code Triggers

AASHTO (American Association of State Highway and Transportation Officials) and FHWA visibility studies indicate glare risk increases sharply below 15° solar elevation. Our analysis can show that a roadway lacked recommended engineering controls, supporting claims against municipalities or DOT agencies.

Frequently Asked Questions About Sun Glare in Crash Cases

How do meteorologists calculate sun position so precisely?

We use NOAA’s Solar Position Algorithm (SPA), which incorporates Earth’s axial tilt, orbital mechanics, and atmospheric refraction. Accuracy is ±0.0003 radians (≈0.017°), corresponding to ~1 foot of error per 3 miles distance. Courts have accepted SPA as authoritative since the 1990s.

Can glare be present if there are clouds?

Yes, but it depends on cloud type and coverage. Thin cirrus or scattered cumulus allow enough direct sunlight to cause glare. Overcast or fog typically eliminates it. We retrieve METAR sky condition codes (CLR, FEW, SCT, BKN, OVC) and radar data to confirm.

What is the critical solar elevation for glare?

AASHTO and FHWA visibility studies indicate glare risk increases sharply below 15° solar elevation. Below 10°, glare becomes severe. Below 5°, it can create a total whiteout. We report the exact elevation at crash time and compare it to these thresholds.

Do windshield conditions affect glare?

Yes. Dirt, salt, pollen, and micro-scratches scatter sunlight, amplifying glare. A clean windshield reduces glare by ~30% compared to a dirty one. If vehicle photos are unavailable, we note this limitation and cite industry fleet survey norms.

How do I prove glare caused a crash if there are no witnesses?

Forensic meteorology provides objective proof: solar position aligned with road heading, elevation ≤15°, and clear sky confirmed by METAR. Combined with the lack of skid marks (indicating the driver never saw the hazard), this establishes glare as the likely cause.

Is sun glare a valid legal defense?

Yes, when properly documented. Courts recognize glare as an unavoidable hazard if (1) solar elevation was ≤15°, (2) road geometry aligned with sun azimuth, and (3) weather did not block sunlight. Our reports have been admitted in 40+ states as expert testimony.

Summary and Next Steps

  • Sun glare is quantifiable: Solar position accurate to ±0.01°, weather data from NOAA/NWS.
  • Peak risk during equinoxes when the sun aligns with east-west roads during commute hours.
  • Forensic meteorologists convert subjective claims into court-ready evidence using SPA calculations, METAR obs, and GIS road geometry.

Need expert analysis for a sun glare crash case? Contact us for a free case review. We retrieve data, calculate solar position, and deliver a defensible report within 7–10 business days.

Need Expert Weather Analysis for Your Case?

Use the contact form below or email me for a free case review.

John Bryant – Forensic Meteorologist

📞 901.283.3099

✉️ [email protected]

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The author of this article is not an attorney. This content is meant as a resource for understanding forensic meteorology. For legal matters, contact a qualified attorney.