Measure planetary or surface reflectivity with flexible inputs. Review absorbed energy, percentages, and quick interpretations. Export clean reports and compare scenarios with confidence today.
Albedo is dimensionless. A value of 0 means total absorption, while 1 means total reflection. Most real surfaces fall between these limits.
| Surface | Incident Radiation (W/m²) | Reflected Radiation (W/m²) | Albedo Fraction | Albedo Percent |
|---|---|---|---|---|
| Fresh Snow | 800 | 680 | 0.8500 | 85.00% |
| Desert Sand | 900 | 360 | 0.4000 | 40.00% |
| Grassland | 850 | 170 | 0.2000 | 20.00% |
| Ocean Surface | 900 | 54 | 0.0600 | 6.00% |
| Bright Cloud Layer | 700 | 490 | 0.7000 | 70.00% |
Albedo is the fraction of incoming radiation reflected by a surface. It ranges from 0 to 1 and is often reported as a percentage.
A high albedo means the surface reflects a large share of incoming energy. Snow, ice, and bright clouds usually have high albedo values.
A low albedo means the surface absorbs more energy and reflects less. Dark soil, forests, asphalt, and water often show low values.
In normal physical conditions, no. Values above 1 usually point to inconsistent measurements, bad unit handling, or an incorrect incident radiation estimate.
Area lets the calculator convert flux into total reflected and absorbed power. That is useful for surface studies, energy balance checks, and comparison scenarios.
The albedo ratio stays the same if incident and reflected values use the same unit. Total power outputs still depend on the selected flux and area units.
Reflectance can describe reflection for a specific wavelength or angle. Albedo usually refers to an integrated, overall reflective behavior across incoming radiation.
Uncertainty inputs help estimate how measurement error may shift the albedo result. This is useful when comparing field readings or instrument-based observations.
Important Note: All the Calculators listed in this site are for educational purpose only and we do not guarentee the accuracy of results. Please do consult with other sources as well.