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Propagation of radio waves

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Propagation of radio waves Ways of travelling Propagation in ionosphere Propagation in troposphere Special ways of reflecting Propagation depends on the properties of ... – PowerPoint PPT presentation

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Title: Propagation of radio waves


1
Propagation of radio waves
2
Ways of travelling
  • Propagation in ionosphere
  • Propagation in troposphere
  • Special ways of reflecting
  • Propagation depends on
  • the properties of the medium
  • frequency
  • weather, time of day, sun activity

3
Propagation in ionosphere
  • Solar radiation (UV, X-ray) partially ionize the
    atmosphere
  • Ionization depends on the density of the gases
  • Waves reflect (refract) from the ionized layers
  • Directly dependent
  • on day of time, most neutralized just before
    sunrise
  • actitivity of sun
  • sun spot number
  • solar flux

4
  • Ionization level and reflection properties divide
    the ionosphere in different layers
  • D 55-90 km
  • E 90-150 km
  • F 150-400 km

5
D layer
  • lowest layer exist only during daylight
  • unsuitable for contacts, absorbs radio energy
  • 7 10 MHz can travel through at high angles

6
E layer
  • A bit more stable layer, disappears at night
  • Skip from E layer is limited by D
  • hard to distinguish from F layer propagation
  • longest one skip range is 2000 km
  • home for other interesting ways of propagation
  • Es
  • Aurora, meteor scatter

7
F layer
  • Divided in two during daytime F1, F2
  • F2 more important, never absent
  • one skip almost 4000 km, multihops even longer
  • reflects from ground, E-layer once or several
    times
  • Controlled by sun activity

8
Propagation in troposphere
  • VHF, UHF microwaves
  • weather effects
  • tropospheric scattering primary form
  • rain, fog, dust, snow, clouds
  • ducting
  • Radiation inversions
  • air layers with different temperatures and dew
    points
  • can travel long (1500 km)
  • calm summer evenings

9
Other forms of propagation
  • Aurora
  • EME
  • Meteors
  • Sporadic E
  • Satellites

10
Aurora
  • High-energy particles flow into ionosphere during
    geomagnetic storm ? ionize E layer
  • 28 432 MHz
  • K index magnetic activity 0-9
  • Signals sound distorted, sometimes only CW at
    VHF-UHF (AAurora)

11
EME
  • Earth-Moon-Earth
  • 50 MHz to 10 GHz
  • Free space loss, ½ degree target, Doppler shift,
    Faraday rotation... not that easy
  • eFFe-mobiili

12
Meteor scatter
  • Ionize a column of air at E layer
  • stays ionized for a few seconds to a minute ?
    just enough time for brief contacs
  • 50 MHz, 144 MHz
  • High speed Morse code, pieced together

13
Sporadic E
  • Ionization level gets abnormally high
  • 28, 50, 144 MHz
  • Usually at summer time at morning and again at
    early evening
  • Might dissipate quickly or move

14
Satellites
  • Works as repeater station
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