In classical general relativity, a black hole is an “eternal” object: once something crosses the event horizon, it cannot return to the outside universe. Quantum field theory in curved spacetime changes that picture. In 1974, Stephen Hawking showed that a black hole should emit nearly thermal radiation, causing it to lose mass. This slow loss of mass is usually called black hole evaporation.
The key qualitative result is simple and counterintuitive: the smaller the black hole, the hotter it is. Because a hotter black hole radiates more power, it loses mass faster. That creates a runaway behavior where evaporation accelerates as the mass drops, ending (in the semiclassical model) in a rapid final stage.
Enter a black hole mass in solar masses (M☉). The calculator converts it to SI units (kilograms) and estimates:
These outputs are meant as order-of-magnitude physical estimates for isolated black holes in the semiclassical regime.
The Hawking temperature for a non-rotating, uncharged black hole of mass M is:
T = ħc³ / (8π G M kB)
The commonly cited semiclassical evaporation time (ignoring detailed particle “greybody” effects and changes in degrees of freedom) is:
t ≈ 5120π G² M³ / (ħ c⁴)
These show the main scaling:
This calculator uses standard SI constants:
Input mass is entered in solar masses and converted to kilograms internally. Temperature is reported in Kelvin. Evaporation time is computed in seconds and can be displayed in years for readability (1 year ≈ 365.25 days).
Hawking temperature tells you the characteristic thermal scale of the emitted radiation as measured by a distant observer. For very massive black holes, the temperature is far below the cosmic microwave background (CMB) temperature (~2.7 K), meaning they are effectively colder than the universe and would tend to gain energy from ambient radiation in realistic environments.
Evaporation time is the estimated time for the black hole to radiate away essentially all of its mass, assuming it is isolated and does not accrete. Because the lifetime scales like M³, changing the mass by a factor of 10 changes the lifetime by a factor of 1000.
Suppose you enter 1 solar mass (M = 1 M☉). The calculator will convert this to M ≈ 1.988×1030 kg and evaluate:
This sanity-check illustrates why Hawking evaporation is negligible for astrophysical black holes today, while hypothetical much smaller black holes (e.g., primordial black holes) could evaporate on cosmological timescales.
The table below summarizes how temperature and lifetime scale with mass. Values are approximate and meant for intuition; the exact numbers depend on the constant factors and modeling details.
| Mass (in M☉) | Relative temperature (T ∝ 1/M) | Relative lifetime (t ∝ M³) |
|---|---|---|
| 10 | ~0.1× (colder) | ~1000× (longer) |
| 1 | 1× | 1× |
| 0.1 | ~10× (hotter) | ~0.001× (shorter) |
| 10−12 | ~1012× (much hotter) | ~10−36× (much shorter) |