Lesson 1
Meteorological Satellite Orbits
Lesson 2
Review of Radiative Transfer
Lesson 3
Visible Image Interpretation
Lesson 4
Infrared Image Interpretation
Lesson 5
Multispectral Image Interpretation
Lesson 6
Fires & Aerosols
Lesson 7
Winds
Lesson 8
Sounders
Lesson 9
Fog and Stratus
Lesson 10
Thunderstorm
Lesson 11
Energy Budget
Lesson 12
Hurricanes
Lesson 13
Global Circulation
Lesson 14
Synoptic Scale
Lesson 15
Local Circulation
Lesson 16
Satellite Oceanography
Lesson 17
Precipitation

The Planck Function

    A theoretical explanation for cavity radiation was the single most compelling unsolved problem in physics at the beginning of the twentieth century. The best fit to observations had been suggested by Wein:


  1. where c1 and c2 were determined experimentally. In October 1900 Max Planck proposed a small modification to this relationship, namely

Planck’s relationship, now called the Planck function, was a better fit to the data but was not an explanation for why radiation behaves this way. To develop a theoretical model, Planck imagined that the atoms in the cavity walls behave like tiny oscillators, each with its own characteristic frequency, each emitting radiation into the cavity and absorbing energy from it. But it proved impossible to derive the properties of cavity radiation until he made two radical assumptions:
  1. that the atomic oscillators cannot take on arbitrary values of energy E. Instead, the oscillators have only values of E that satisfy  where n is an integer called the quantum number, n the oscillator frequency, and h a constant.
  2. that radiation occurs only when an oscillator changes from one of its possible energy levels to another; that is, when n changes value. This implies that the oscillators cannot radiate energy continuously, but only in discrete packets, or quanta.
By December of 1900 Planck had worked out a complete theory for cavity radiation, including the values of c1 and c2:


In these equations k is Boltzmann’s constant, which appears in statistical mechanics and thermodynamics, and h is Planck’s constant. Planck used observations of  to determine the values J s and  J K-1.



Next

Back

Return to Lesson 2
Return to Satellite Meteorology Main Page