Hotter. Brighter. Shorter.
Change the temperature. Watch the spectrum shift.
Compare curves to see where the extra radiation goes.
Ideal blackbody · emissivity = 1
Wavelength distribution · absolute scale
Set the temperature
Keep up to three reference curves, then change the temperature.
The emission spectrum
Spectral intensityMW m⁻² μm⁻¹
Visible wavelengths are approximately 0.38–0.75 μm.
Predict, then explore
Keep a curve at 3000 K, then double the temperature. Does the peak wavelength double or halve? How much does the total emitted power increase?
With auto-scale on, the tallest peak stays at the same screen height while the Y-axis values change. This is a changing axis scale, not constant physical intensity. Save a curve for comparison, or turn auto-scale off to hold the vertical axis fixed.
IB takeaways: higher temperature means a shorter peak wavelength, greater intensity at every fixed wavelength, and a larger total area under the full curve. Graph clipped? Widen the wavelength range or enable auto-scale. All curves always share one scale.
The physics behind the curve
M = σT4
IB graph convention: the Y-axis shows emitted intensity per unit wavelength. More precisely, this is spectral radiant exitance Mλ: emitted power per surface area per wavelength interval, integrated over the outward hemisphere. It is not spectral radiance per steradian.
Presets are ideal-blackbody approximations. A 300 K object radiates mainly in the infrared; a visible-band peak does not mean monochromatic body colour.