Spectral index

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In astronomy, the spectral index of a source is a measure of the dependence of radiative flux density on frequency. Given frequency and radiative flux , the spectral index is given implicitly by

Note that if flux does not follow a power law in frequency, the spectral index itself is a function of frequency. Rearranging the above, we see that the spectral index is given by

Spectral index is also sometimes defined in terms of wavelength . In this case, the spectral index is given implicitly by

and at a given frequency, spectral index may be calculated by taking the derivative

The opposite sign convention is sometimes employed,[1] in which the spectral index is given by

The spectral index of a source can hint at its properties. For example, using the positive sign convention, a spectral index of 0 to 2 at radio frequencies indicates thermal emission, while a steep negative spectral index typically indicates synchrotron emission.

Spectral Index of Thermal emission[edit]

At radio frequencies (i.e. in the low-frequency, long-wavelength limit), where the Rayleigh–Jeans law is a good approximation to the spectrum of thermal radiation, intensity is given by

Taking the logarithm of each side and taking the partial derivative with respect to yields

Using the positive sign convention, the spectral index of thermal radiation is thus in the Rayleigh-Jeans regime. The spectral index departs from this value at shorter wavelengths, for which the Rayleigh-Jeans law becomes an increasingly inaccurate approximation, tending towards zero as intensity reaches a peak at a frequency given by Wien's displacement law. Because of the simple temperature-dependence of radiative flux in the Rayleigh-Jeans regime, the radio spectral index is defined implicitly by[2]


  1. ^ Burke, B.F., Graham-Smith, F. (2009). An Introduction to Radio Astronomy, 3rd Ed., Cambridge University Press, Cambridge, UK, ISBN 978-0-521-87808-1, page 132.
  2. ^ "Radio Spectral Index". Wolfram Research. Retrieved 2011-01-19.