Lecture 2 EMR Flashcards
Name 3 Sources of EMR
Solar
Terrestrial
Artificial
3 types of atmospheric scattering
Rayleigh - gas molecules in upper atmosphere
Mie - when particles are same diameter as radiation wavelength
Non-selective - Particles larger than radiation
3 wave types of radiation is measured
Energy reflected from sun
Radiation emitted from objects
Radiation reflected when instrument sends out a signal,
Visible Spectrum
Blue - 400-500nm
Green 500-600nm
Red 600-700nm
Infrared Spectrum
Near IR 0.7 - 1 µm
Shortwave IR 1- 3 µm
Mid IR 3 - 5 µm
Far IR 5 µm - 1 mm
What is Far Infrared known as
Thermal infrared
Microwave Spectrum
> 1mm
What changes the type of atmospheric scattering?
The wavelength of the incident radiant energy
The size of the gas molecule, dust particle and/or water vapour droplet encountered
Atmospheric windows
Bands in spectrum where absorption is least
Primary absorbers of EMR
Ozone
Carbon dioxide
Water Vapour