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 Waves and ionisation
 Atmosphere
 Ionosphere
 Troposphere
 Other methods
 Electromagnetic energy
 Models
 Waves
 Particles
 Electrical part
 Magnetic part
 Polarisation
 Vertical
 Horizontal
 Ion
 Protons != electrons
 Ionisation
 Removal or addition of an electron
 Energy
 Troposphere
 Ground to 7-17 km out - Temp dec. with height
 80% of the mass
 Stratosphere
 About 51 km out – Temp inc. with height
 Mesosphere
 80-85 km out – temp at – 85 deg C
 Thermosphere
 350 – 800 km out – temp +1 500 Deg C
 Exosphere
 Troposphere
 Thermosphere
 Exosphere
ionosphere
 100 – 300 km
 Ionisation of particles
 Sun
 Thin atmosphere
 Shell of electrons
 Layers
 Radio propagation
 “acts like a mirror”
 At certain frequencies
 D layer
 Ionising NO (some N2 and O2)
 Electron collision high
 Results in blocking of HF radio waves
 < 10 MHz
 Almost disappears after sunset
 HF can pass through if broadcasted directly up
 E (Heavyside) layer
 Ionisation of O2
 Refracts radio waves < 10 MHz
 Nordic area
 At night, increasing height inc. range
 Es layer
 Sporadic – best during the summer
 Refracts up to 50 Mhz
 Distance of 1000 km
 F (Appleton) layer
 Ionising of O – dense
 Refracts most HF radio waves (3-30 MHz)
 Skywaves
 F1 and F2 layers
 Exist during the day
 Fading
 Changes in the ionosphere
 Changes the polarisation
 Angle
 Critical angle
 Depends on ionosphere and frequency used
 Hi angle and Hi F pass through.
 Nordic region
 3.5 – 7 MHz
 Dipole
 Straight out
 Using D layer
 14 – 30 MHz
 Uses E and F layers (low elevation angle)
 2 000 – 4 000 Km
 DX traffic
 DX – distance
 Dipole or yagi array
 For Europe
 30 Deg
 0.5 Wave length
 Out side Europe
 1 -2 X wave length
 10 Deg 1.5 X wave length
 Its damp!
 99% of the water vapour!
 Effects radio transmissions
 Hi F = more absorption
 Used for VHF, UHF and SHF transmissions
 Line of sight
 20- 30 km (depends on power)
 Can scatter (refraction)
 Up to 2 000 km
 Earth-Moon-Earth (EME)
 144 MHz, 434 MHz and 1 296 MHz
 As far away as Australia!
 Meteors
 Same as EME
 Short burst
 Auroras
 > 25 MHz
 NW -> NE aerial
Wave probigation

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Wave probigation

  • 1.
  • 2.  Waves and ionisation  Atmosphere  Ionosphere  Troposphere  Other methods
  • 3.  Electromagnetic energy  Models  Waves  Particles  Electrical part  Magnetic part  Polarisation  Vertical  Horizontal
  • 4.
  • 5.  Ion  Protons != electrons  Ionisation  Removal or addition of an electron  Energy
  • 6.
  • 7.  Troposphere  Ground to 7-17 km out - Temp dec. with height  80% of the mass  Stratosphere  About 51 km out – Temp inc. with height  Mesosphere  80-85 km out – temp at – 85 deg C  Thermosphere  350 – 800 km out – temp +1 500 Deg C  Exosphere
  • 9.
  • 10.  100 – 300 km  Ionisation of particles  Sun  Thin atmosphere  Shell of electrons  Layers  Radio propagation  “acts like a mirror”  At certain frequencies
  • 11.
  • 12.  D layer  Ionising NO (some N2 and O2)  Electron collision high  Results in blocking of HF radio waves  < 10 MHz  Almost disappears after sunset  HF can pass through if broadcasted directly up
  • 13.  E (Heavyside) layer  Ionisation of O2  Refracts radio waves < 10 MHz  Nordic area  At night, increasing height inc. range  Es layer  Sporadic – best during the summer  Refracts up to 50 Mhz  Distance of 1000 km
  • 14.  F (Appleton) layer  Ionising of O – dense  Refracts most HF radio waves (3-30 MHz)  Skywaves  F1 and F2 layers  Exist during the day
  • 15.  Fading  Changes in the ionosphere  Changes the polarisation  Angle  Critical angle  Depends on ionosphere and frequency used  Hi angle and Hi F pass through.
  • 16.
  • 17.
  • 18.  Nordic region  3.5 – 7 MHz  Dipole  Straight out  Using D layer  14 – 30 MHz  Uses E and F layers (low elevation angle)  2 000 – 4 000 Km
  • 19.  DX traffic  DX – distance  Dipole or yagi array  For Europe  30 Deg  0.5 Wave length  Out side Europe  1 -2 X wave length  10 Deg 1.5 X wave length
  • 20.  Its damp!  99% of the water vapour!  Effects radio transmissions  Hi F = more absorption  Used for VHF, UHF and SHF transmissions  Line of sight  20- 30 km (depends on power)  Can scatter (refraction)  Up to 2 000 km
  • 21.  Earth-Moon-Earth (EME)  144 MHz, 434 MHz and 1 296 MHz  As far away as Australia!  Meteors  Same as EME  Short burst  Auroras  > 25 MHz  NW -> NE aerial