summery: P1-5 Flashcards
(44 cards)
Radio and radar operate using:
Electromagnetic radiation
Electromagnetic radiation:
Has both electric and magnetic components. Each component vibrate at right angles to each other and both are right angles to the direction of propagation.
Electromagnetic radiation always travel at:
The speed of light where light itself is just a special form of electron agnetic radiation. It just happens to be at a frequency and wavelength which is detectable by our eyes.
Important characteristics of electromagnetic radiation:
- Frequency
- Wavelength
F=c/lamda where lamda is the wave length (in meters)
Electromagnetic radiation range from:
Very low frequency to very high frequencies
Frequency of radio waves:
High
radar is located:
upper end of EM spectrum
located to the right of the EM spectrum:
infrared, visible and UV light
higher frequency forms of EM radiation:
X-ray and Gamma waves
Frequency used by radars:
100 MHz through 300 GHz
Why are some frequencies designated by letters?
They are very frequent so it is convenient to assign letters
What are the nominal wavelength of L, S, C and X?
Band designation
Nominal wavelength
L
30-15 cm
S
15-8 cm
C
8-4 cm
X
4-2.5 cm
The speed of EM radiation depends on:
The material it is traveling in
When EM radiation travels trough air and other material it travels
Slower than in vacuum
Refractive index:
The ratio of the speed of light in a vacuum to the speed of light in a medium
N=c/u where c is the speed of light and u is the speed of light in the medium
Relationship between n, c and u:
- C is always greater than or equal u
- N is always greater than or equal 1
Components of the refractive index:
(two components)
- (the one above) Simple, real component of the complex refractive index (m) m=n-ik where i is (radical -1) and k is related to the absorption coefficient of the medium
- For a perfect dielectric (non conductor), k =0
Refractive index of air in the atmosphere near sea level:
1.0003 to 1.0004 this means that EM radiation travel 0.03% to 0.04% slower there than in vacuum
Refractive indexes as you go up the atmosphere
Refractive index decrease with high (1.0003 near the surface and 1 at the top of the atmosphere)
The most important part of the refractive index is in:
The 4th, 5th and 6th decimal places
Refractivity:
Because it is hard to work with very small numbers you can subtract 1 from the index of refraction and multiply the result by 106. The result is in n units
Equation of refractivity:
N=(n-1)x106
Refractivity index of the atmosphere depend on
- Temperature
- Pressure
- Vapor pressure
- Number of free electrons present
- In troposphere there aren’t enough free electrons for it to be important
- The effect of free electrons is only important high in the atmosphere
- Variation of free electrons allow wind profiling radars to detect wind in upper stratosphere and mesosphere
Explain each variable in the equation

- N: refractivity
- T: temperature (in kelvin)
- P: pressure (in mb or hpa)
- E: vapor pressure of moist air (in mb or hpa)
- Ne: number density of free electrons per m3
- F: frequency of radar signals (in hz)