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Calcimator

Spacecraft Thermal Calculator

Temperature range from solar flux, albedo, and surface properties.

Inputs

Results

Equilibrium temp (°C)

-19

Hot case temp (°C)

-1.9

Cold case temp (°C)

-75.5

Equilibrium temp (K)254.2
Total heat input (W)1,207.1
Solar heat (W)530.8
Albedo heat (W)134.9
Earth IR heat (W)341.4
Alpha/epsilon ratio0.35
Earth view factor0.85
T_fahrenheit-2.14
How to Use This Calculator
  1. Enter orbital altitude (km) and the spacecraft's solar absorptance (α) and thermal emittance (ε) surface properties.
  2. Set the projected solar area (m²), radiator area (m²), and internal heat dissipation (W).
  3. Review equilibrium temperature (°C and K), hot case temperature, and cold case temperature.
  4. Ensure all temperatures fall within the allowable operating ranges for electronics and propellant.
  5. Adjust surface coatings (α/ε ratio) or radiator area to bring temperatures within acceptable limits.

How the result changes with Radiator area (m²)

Radiator area (m²)Equilibrium temp (°C)Hot case temp (°C)Cold case temp (°C)
100-147.3-138.9-175.3
350-181.2-175-201.6
650-194.4-189.1-211.9
900-200.5-195.6-216.7

What each input means

Orbital altitude (km)
Orbit altitude affects Earth view factor (albedo and IR heating). Higher altitude = less Earth heating.
Solar absorptance (alpha)
Fraction of solar radiation absorbed. White paint: 0.2, bare aluminum: 0.15, solar cells: 0.75, black paint: 0.95.
Thermal emittance (epsilon)
IR emissivity. White paint: 0.85, polished aluminum: 0.04, black paint: 0.90, OSR: 0.80.
Solar projected area (m²)
Cross-sectional area facing the sun (projected area of body + solar panels if body-mounted).
Radiator area (m²)
Total surface area that radiates heat to space. Typically total external surface area.
Internal heat dissipation (W)
Waste heat from electronics, batteries, and instruments that must be radiated away.
Eclipse fraction (0-0.5)
Fraction of orbit spent in Earth's shadow. LEO ~0.35, GEO ~0-0.04, sun-sync dawn/dusk ~0.

What each result means

Equilibrium temp (°C)
Orbit-average equilibrium temperature.
Equilibrium temp (K)
Same temperature in Kelvin.
Hot case temp (°C)
Maximum temperature (no eclipse, full solar illumination).
Cold case temp (°C)
Minimum temperature (full eclipse, reduced internal heat).
Total heat input (W)
Sum of all heat sources.
Solar heat (W)
Absorbed direct solar radiation.
Albedo heat (W)
Absorbed reflected sunlight from Earth.
Earth IR heat (W)
Absorbed infrared radiation from Earth.
Alpha/epsilon ratio
Key thermal design parameter. Low ratio = cooler spacecraft.
Earth view factor
Geometric view factor to Earth from the spacecraft.

How this is calculated

Worked example, using the default values

  1. Identify Input Parameters
    4 parameters
    Orbital altitude (km) = 550, Solar absorptance (alpha) = 0.3, Thermal emittance (epsilon) = 0.85, Solar projected area (m²) = 2 = 7 input(s) provided
  2. Calculate Equilibrium temp
    Equilibrium temp = T_kelvin - 273.15
    -19 = -19
  3. Calculate Hot case temp
    Hot case temp = T_hot_K - 273.15
    -1.9 = -1.9
  4. Calculate Cold case temp
    Cold case temp = T_cold_K - 273.15
    -75.5 = -75.5
  5. Calculate Equilibrium temp
    254.2 = 254.2
  6. Calculate Total heat input
    Total heat input = qSolar + qAlbedo + qEarthIR + internalHeatW
    1207.1 = 1207.1

Engine last updated . Checked against 2 independently-derived tests how we verify calculators.

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