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

Lesson 3: Background

Interpreting Satellite Visible Images

Imagine two layers, one of which overlies the other. The upper layer has flux transmittance and reflectance T1 and R1, and the lower layer T2 and R2. How much total flux RT is reflected from the combination of layers? Some flux is reflected from the first layer (R1); some of the flux transmitted through the first layer is reflected from the second layer and transmitted through the first layer (T1R2T1); some of this flux reflected from the second layer is reflected back downwards, where some portion is reflected back up (T1R2R1R2T1), and so on. Because reflection and transmission are both less than one, we can use the summation formula for geometric series to compute the total reflection is:

where the term in square brackets accounts for the multiple reflections between the layers. There is a similar relation for transmission.



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