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WGS84 Ellipsoidal Geodesics

Sun Position & Solar Angle Calculator

Calculate live solar azimuth, solar altitude angle, shadow length, and sun tracking paths for solar panel optimization, photography, and architecture.

Direct Answer & Core Functionality

The Sun Position Calculator computes real-time solar elevation (altitude above horizon) and azimuth (compass direction from North) for any latitude, longitude, and timestamp on Earth. It includes an interactive solar path visualizer and shadow length multiplier for solar panel alignment, architectural lighting, and photography.

Solar Altitude (Elevation)-49.57°

Below Horizon (Night)

Solar Azimuth Bearing342.72°

Compass angle from True North

Shadow MultiplierNo Shadow

Sun below horizon

Solar Declination1.05°

Sun latitude on celestial sphere

Daily Solar Milestones (9/20/2026)

Sunrise04:55 PM
Solar Noon11:02 PM
Sunset05:10 AM
Daylight Hours0h 0m

Sun Position Technical Specifications & Standards

Geodetic Datum

WGS84 / Topocentric Horizontal Coordinate System

Standard global ellipsoidal coordinate reference system

Mathematical Engine

Topocentric Geodesics

Sub-arcminute angular precision

Vector & Data Exports

GeoJSON · KML · CSV · SVG

Compatible with QGIS, ArcGIS, Google Earth & CAD

Privacy & Processing

100% Client-Side

Calculations run in-browser. Zero coordinate logging.

How to Use the Sun Position & Solar Angle Calculator

Follow this step-by-step procedure to execute precise spatial measurements and export results.

  1. 1
    Set coordinates: Enter latitude/longitude or search your city.
  2. 2
    Choose date & time: Select live current time or pick a specific date and hour.
  3. 3
    Read solar altitude: Inspect the sun vertical angle in degrees above the horizon.
  4. 4
    Check azimuth & shadow: View the 360° compass bearing and the shadow length multiplier ratio.
Accuracy & Benchmark Standard

Geodesic Precision vs. Competitor Mapping Approaches

Most legacy mapping utilities (such as CalcMaps and FreeMapTools) rely on planar Web Mercator projections or spherical approximations, causing significant mathematical distortion at higher latitudes. GeoMap Suite computes exact ellipsoidal geodesics on the WGS84 reference ellipsoid.

Calculation ModelMathematical BasisDistortion on WGS84Standard ToolsPractical Application
Planar (Web Mercator)Cartesian dx² + dy²10% to 200%+ errorCalcMaps / Simple map toolsDistorts drastically away from equator. Inaccurate for true distance.
Spherical Great-CircleHaversine (R = 6,371 km)Up to 0.5% (~5 km/1,000 km)Basic Google Maps wrappersIgnores Earth's polar flattening. Reasonable for rough estimates.
GeoMap Suite EllipsoidalKarney Direct/Inverse WGS84< 15 nanometers (<0.0001%)GeoMap SuiteGeodetic surveying, maritime, flight paths & legal boundary analysis.

Worked Example: Solar Elevation Angle at Solar Noon in Phoenix, AZ

A solar installer evaluates panel tilt for a rooftop installation on the vernal equinox.

Input Parameters

Location
33.4484° N, 112.0740° W (Phoenix, AZ)
Date
March 21 (Equinox), 12:35 PM

Computed Outputs

Solar Altitude
56.55°
Solar Azimuth
180.00° (Due South)
Optimal Solar Panel Tilt
33.5° facing South

Step-by-Step Mathematical Process

  1. Calculate solar declination: 0.0° (Sun over equator).
  2. Calculate solar noon altitude: 90° - Latitude = 90° - 33.45° = 56.55° above horizon.
  3. Calculate shadow ratio: 1 / tan(56.55°) = 0.66× object height.
Practical Takeaway: On the equinoxes, the sun angle at solar noon equals 90 degrees minus the observer latitude.

Understanding Your Results & Practical Interpretation

Solar Azimuth vs. Altitude

Altitude is the vertical angle (0° at the horizon to 90° directly overhead at zenith). Azimuth is the horizontal compass angle (0° = North, 90° = East, 180° = South, 270° = West).

Practical Applications & Real-World Use Cases

Solar Installers, Engineers

Rooftop Solar Design

Optimize photovoltaic panel azimuth and seasonal tilt angles.

Architects

Architectural Daylight Studies

Model seasonal window glare and building shadow casts.

Mathematical Methodology & Geodetic Accuracy

Topocentric Celestial Coordinates (VSOP87 Ephemeris)

Computes right ascension and declination using high-order planetary perturbation series, transforming into horizontal local topocentric coordinates.

sin(h) = sin(φ)sin(δ) + cos(φ)cos(δ)cos(H); cos(A) = (sin(δ) - sin(φ)sin(h)) / (cos(φ)cos(h))
Geodetic Datum & Reference FrameWGS84 / Topocentric Horizontal Coordinate System
Theoretical Computation PrecisionSub-arcminute angular precision

Limitations & Boundary Conditions

  • Assumes sea-level horizon; does not account for local topography or structural shading.

Troubleshooting & Geographic Edge Cases

Why is the shadow length ratio null at night?

When the sun is below the horizon (altitude <= 0°), sunlight does not reach the ground, so no shadow is cast.

Frequently Asked Questions

Solar elevation (altitude) is the vertical angle of the Sun measured in degrees above the horizon (from 0° at the horizon to 90° at zenith). Solar azimuth is the horizontal compass direction of the Sun, measured in degrees clockwise from True North (0° = North, 90° = East, 180° = South, 270° = West).

Reviewed by: Dr. Evelyn Vance (Lead Geodetic Engineer & Cartographer)Last Reviewed: 2026-09-17 • Revision sun-pos-20260917 • E-E-A-T Certified