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RADIO WAVE PROPAGATION
REFERENCES “ Almost Everything You Need to Know …”: Chapter 7: 53-68   “ RAC Basic Study Guide 6th Ed :”  6.2, 6.3, 6.4, 6.5, 6.6, 6.8, 6.9, 6.10 “ RAC Operating Manual 2nd Ed :” “ The ARRL Handbook For Radio Amateurs 2001,78 th Ed:” Chapter 21: 1-37   "Radio Propagation."   Wikipedia, The Free Encyclopedia. 6 Nov 2007 http://en.wikipedia.org/ “ Chelmsford Amateur Radio Society”   Intermediate Course (5) Antennas and Feeders
OBJECTIVES: ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
 
PROPAGATION - INTRO Propagation:   how radio waves get from point A to point B.  The events occurring in the transmission path between two stations that affect the communications between the stations. When the electrons in a conductor, (antenna wire) are made to oscillate back and forth, Electromagnetic Waves (EM waves) are produced. These waves radiate outwards from the source at the speed of light, 300 million meters per second.  Light waves and radio waves are both EM waves, differing only in frequency and wavelength.
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],PROPAGATION – INTRO CONT’D
RADIO WAVES ,[object Object],[object Object],[object Object],z x y Electric Field, E Magnetic Field, H Direction of Propagation
RADIO WAVES CONT’D ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
RADIO WAVES CONT’D ,[object Object],[object Object],[object Object]
POLARIZATION ,[object Object],[object Object],[object Object]
Direction of Propagation Direction of Propagation
Horizontally polarized directional yagi antenna  Vertically polarized omnidirectional  dipole antenna
RADIO WAVES CONT’D RADIO WAVES SPACE GROUND SKY REFLECTED DIRECT  SURFACE
LINE OF SIGHT, GROUND WAVE, SKY WAVE ,[object Object],[object Object],[object Object],[object Object]
LINE OF SIGHT, GROUND WAVE, SKY WAVE
LINE OF SIGHT, GROUND WAVE, SKY WAVE CONT’D
IONOSPHERE REGIONS ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
IONOSPHERE REGIONS
IONOSPHERE REGIONS CONT’D
PROPAGATION, HOPS, SKIPS ZONES ,[object Object],[object Object],[object Object]
PROPAGATION, HOPS, SKIPS ZONES ,[object Object],[object Object],[object Object]
PROPAGATION, HOPS, SKIPS ZONES ,[object Object],[object Object],[object Object]
Refraction is the change in direction of a wave due to a change in its speed Reflection is the change in direction of a wave front at an interface between two different media
Diffraction  refers to various phenomena associated with wave propagation, such as the bending, spreading and interference of waves passing by an object or aperture that disrupts the wave Attenuation  is the reduction in amplitude and intensity of a signal. Can also be understood to be the opposite of amplification. Attenuation is important in determining signal strength as a function of distance.
 
PROPAGATION, HOPS SKIPS ZONES
PROPAGATION, HOPS SKIPS ZONES CONT’D The maximum distance along the earth’s surface that is normally covered in one hop using the  F2 region is 4000 Km (2500 miles). The maximum distance along the earth’s surface that is normally covered in one hop using the E region is 2000 Km (1200 miles) The distance to Europe from your location is approximately 5000 Km. Multihop propagation  is most likely to be involved.
THE IONOSPHERIC LAYERS ,[object Object],[object Object],[object Object],[object Object]
PROPAGATION, HOPS SKIPS ZONES CONT’D
THE IONOSPHERIC LAYERS CONT’D ,[object Object],[object Object],[object Object],[object Object]
THE IONOSPHERIC LAYERS CONT’D ,[object Object],[object Object],[object Object],[object Object],[object Object]
ABSORPTION AND FADING ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
ABSORPTION AND FADING
ABSORPTION AND FADING Received signal Transmission signal Different paths
SOLAR ACTIVITY AND SUN SPOTS ,[object Object],[object Object],[object Object]
SOLAR ACTIVITY AND SUN SPOTS CONT’D ,[object Object],[object Object],[object Object],[object Object],Coronal Mass Ejections (CME)
SOLAR ACTIVITY AND SUN SPOTS CONT’D ,[object Object],[object Object],[object Object]
SOLAR ACTIVITY AND SUN SPOTS
MF, HF CRITICAL FREQUENCIES ,[object Object],[object Object],[object Object],[object Object],[object Object]
MF, HF CRITICAL FREQUENCIES Maximum Useful Frequency (MUF)  Frequency of optimum transmission (FOT) /Optimal Working Frequency (OWF) Lower Absorption Frequency (ALF) /  The lowest Usable frequency (LUF):  Above Critical Frequency
MF, HF CRITICAL FREQUENCIES ,[object Object],incident angle and refraction transmission angle is  higher frequency than the MUF.  waves of the same frequency at several different transmission (and incident) angles
BEACONS - 10 METERS Operated by Amateur operators to determine propagation conditions. Ten meter beacons can be found between 28.175 and 28.300 MHZ. Beacons usually identify their location and power output by CW. Amateur operators can use this information to determine if favorable conditions exist between their location and the beacon’s location. NCDXF/IARU International Beacon Network 28.200  4S7B  SRI LANKA  28.200  ZS6DN  WINGATE PK S. AFRICA  28.200  5Z4B  KENYA, AFRICA  28.200  4X6TU  TEL AVIV 28.200  OH2B  KIRKKILA, FINLAND  28.200  CS3B  MADERIA IS  28.200  LU4AA  ARGENTINA  28.200  OA4B  PERU  28.200  YV5B   CARACAS, VEN 28.200  4U1UN  UNITED NATIONS  28.200  VE8AT  CANADA  28.200  W6WX  SAN JOSE, CA  28.200  KH6WO  HONOLULU, HI  28.200  ZL6B  NEW ZEALAND  28.200  VK6RBP  AUSTRALIA  28.200  JA2IGY  MT ASAMA, JAPAN  28.200  RR9O  NOVOSIBIRSK  RUSSIA 28.200  VR2R  HONG KONG CHINA
BEACONS (HF)1.8170 - 24.9860 MHZ (THERE ARE MANY MORE!!!!) N/A N/A Fukushima QM07  24.9860 JE7YNQ dipole N-S 10 Hamburg-Rothenburgsort JO53AM 24.9310 DK0HHH GP 2 Bologna(Marconi Memorial) JN54OK 24.9200 IY4M 2 dipoles 12 N/A JN63KR 24.9150 IK6BAK slope dipole 4 Porto Alegre, 85m asl GF49KX 21.3935v PY3PSI N/A 220m Crabbe Mtn, NB FN66  21.1455 VE9BEA/B vertic.AV640 50 off (Kihei/Maui, HI) N/A 21.1420 KH6AP 1/2 vertical 1 Cerro Jefe FJ09HD 18.0990 HP1AVS/B N/A N/A South Atlantic N/A 14.0460 LU0ARC Horiz.loop 30 Scheggerott JO44VQ 10.1440 DK0WCY N/A N/A off (ausser Betrieb) N/A 10.1400 HB9TC dipole N-S 2 Porto Alegre, 85m asl GF49KX 10.1400 PY3PSI vertical 2 testing,intermittant FJ09HD 10.1390 HP1RCP/B dipole  500m Kladno JO70BC 10.1340 OK0EF N/A N/A Plettenberg Bay KF16PF 10.1235 ZS1J/B dipole 1 George Airport KF16EA 7.0250 ZS1AGI dipole  150m Kam.Zehrovice JO70AC 3.6000 OK0EN N/A N/A Plettenberg Bay KF16PF 3.5865 ZS1J/B dipole 30 Scheggerott JO44VQ 3.5790 DK0WCY N/A N/A N/A N/A 1.8450 OK0EV N/A N/A Plettenberg Bay KF16PF 1.8170 ZS1J/B ANTENNA POWER LOCATION GRID FREQUENCY CALLSIGN
MF, HF CRITICAL FREQUENCIES
MF, HF CRITICAL FREQUENCIES CONT’D
UHF, VHF, SPORADIC E, AURORAS, DUCTING ,[object Object],[object Object],[object Object]
UHF, VHF, SPORADIC E, AURORAS, DUCTING ,[object Object]
UHF, VHF, SPORADIC E, AURORAS, DUCTING Auroral Effects:  Borealis or Northern Lights is evidence of strong ionization in the upper atmosphere and can be utilized to reflect signals. Requires a relatively high power transmitter and both stations point their antennas north toward the aurora. The preferred mode when working VHF aurora is CW although SSB can be used at 50 MHz. The received tone quality when using CW is very different than what you may be used to. Characteristic buzz, echo, very raspy and garbled tones can be expected.  The reason auroral signals sound different is they are being reflected by changing and rapidly-moving reflector (the ionised gases in the aurora). This results in multi-path reflections and the introduction of doppler shift into the signals.
UHF, VHF, SPORADIC E, AURORAS, DUCTING ,[object Object],[object Object],[object Object],[object Object]
UHF, VHF, SPORADIC E, AURORAS, DUCTING
SCATTER, HF, VHF,UHF ,[object Object],[object Object]
SCATTER, HF, VHF,UHF Trans-Equatorial Scatter:  it possible for DX reception of television and radio stations between 3000–5000 miles or 4827–8045Km across the equator on frequencies as high as 432MHz., DX reception of lower frequencies in the 30–70MHz range is far more common. For this mode to work both transmitting and receiving stations should be almost the same distance from the equator. Aircraft Scatter (Tropospheric Reflection):  reflection off aircraft, (reflections off of flocks of birds are also possible). A rare form of reflection is "Chaf Scatter“(strips of metal foil sent out by the military during training exercises). Chaf helps to confuse enemy radars. but also helps to produce DX. Maximum distances for all reflection modes are again up to 800 km (500 mi). Rain Scatter : A band of very heavy rain (or rain and hail) can scatter or even reflect signals. Distances are typically around 160 km. though up to 650 km (400 mi) is theoretically possible. (Note that heavy snow is not an useful reflector).  Ice Pellet Scatter  (called Sleet Scatter in the US). is similar to Rain Scatter but is caused by bands of Ice Pellets in the wintertime.
SCATTER, HF, VHF,UHF Meteor Scatter:  as Meteors burn up entering  the atmosphere it creates a quantity of ionized particles which reflect VHF radio waves. CW or SSB can make several rapid contacts during the brief openings that do occur. These openings may last from a few seconds to a minute or so. Lightning Scatter:  there is little documentation on it but the theory is that lightning strikes produce ionized trails a mode that is very hard to distinguish and rarely reported.
SCATTER, HF, VHF,UHF Scatter propagation  would best be used by two stations within each other’s skip zone on a certain  frequency. If you receive a weak, distorted signal from a distance, and close to maximum usable frequency,  scatter propagation  is probably occurring. A  wavering sound  is characteristic of HF scatter signals Energy scattered into the skip zone through several radio-wave paths  makes HF scatter Signals often sound distorted. HF scatter signals are usually weak because  only a small part of the signal energy is scattered into the skip zone. Scatter  propagation allows a signal to be detected at a distance to far for ground-wave propagation but to near for normal sky-wave propagation. Scatter propagation on the HF bands most often occurs  when communicating on  frequencies above the maximum usable frequency (MUF) Side, Back, and Forward, Meteor, Ionospheric, and Tropospheric  are all scatter modes. Inverted and Absorption are  NOT scatter modes. In the  30 – 100 MHz  frequency range, meteor scatter is the most effective for extended-range communications. Meteor scatter is the most effective on the  6 metre band .
Sample Questions From The IC Question Bank ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
[object Object]

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Srikarsh Awp

  • 2. REFERENCES “ Almost Everything You Need to Know …”: Chapter 7: 53-68 “ RAC Basic Study Guide 6th Ed :” 6.2, 6.3, 6.4, 6.5, 6.6, 6.8, 6.9, 6.10 “ RAC Operating Manual 2nd Ed :” “ The ARRL Handbook For Radio Amateurs 2001,78 th Ed:” Chapter 21: 1-37 "Radio Propagation." Wikipedia, The Free Encyclopedia. 6 Nov 2007 http://en.wikipedia.org/ “ Chelmsford Amateur Radio Society” Intermediate Course (5) Antennas and Feeders
  • 3.
  • 4.  
  • 5. PROPAGATION - INTRO Propagation: how radio waves get from point A to point B. The events occurring in the transmission path between two stations that affect the communications between the stations. When the electrons in a conductor, (antenna wire) are made to oscillate back and forth, Electromagnetic Waves (EM waves) are produced. These waves radiate outwards from the source at the speed of light, 300 million meters per second. Light waves and radio waves are both EM waves, differing only in frequency and wavelength.
  • 6.
  • 7.
  • 8.
  • 9.
  • 10.
  • 11. Direction of Propagation Direction of Propagation
  • 12. Horizontally polarized directional yagi antenna Vertically polarized omnidirectional dipole antenna
  • 13. RADIO WAVES CONT’D RADIO WAVES SPACE GROUND SKY REFLECTED DIRECT SURFACE
  • 14.
  • 15. LINE OF SIGHT, GROUND WAVE, SKY WAVE
  • 16. LINE OF SIGHT, GROUND WAVE, SKY WAVE CONT’D
  • 17.
  • 20.
  • 21.
  • 22.
  • 23. Refraction is the change in direction of a wave due to a change in its speed Reflection is the change in direction of a wave front at an interface between two different media
  • 24. Diffraction refers to various phenomena associated with wave propagation, such as the bending, spreading and interference of waves passing by an object or aperture that disrupts the wave Attenuation is the reduction in amplitude and intensity of a signal. Can also be understood to be the opposite of amplification. Attenuation is important in determining signal strength as a function of distance.
  • 25.  
  • 27. PROPAGATION, HOPS SKIPS ZONES CONT’D The maximum distance along the earth’s surface that is normally covered in one hop using the F2 region is 4000 Km (2500 miles). The maximum distance along the earth’s surface that is normally covered in one hop using the E region is 2000 Km (1200 miles) The distance to Europe from your location is approximately 5000 Km. Multihop propagation is most likely to be involved.
  • 28.
  • 29. PROPAGATION, HOPS SKIPS ZONES CONT’D
  • 30.
  • 31.
  • 32.
  • 34. ABSORPTION AND FADING Received signal Transmission signal Different paths
  • 35.
  • 36.
  • 37.
  • 38. SOLAR ACTIVITY AND SUN SPOTS
  • 39.
  • 40. MF, HF CRITICAL FREQUENCIES Maximum Useful Frequency (MUF) Frequency of optimum transmission (FOT) /Optimal Working Frequency (OWF) Lower Absorption Frequency (ALF) / The lowest Usable frequency (LUF): Above Critical Frequency
  • 41.
  • 42. BEACONS - 10 METERS Operated by Amateur operators to determine propagation conditions. Ten meter beacons can be found between 28.175 and 28.300 MHZ. Beacons usually identify their location and power output by CW. Amateur operators can use this information to determine if favorable conditions exist between their location and the beacon’s location. NCDXF/IARU International Beacon Network 28.200 4S7B SRI LANKA 28.200 ZS6DN WINGATE PK S. AFRICA 28.200 5Z4B KENYA, AFRICA 28.200 4X6TU TEL AVIV 28.200 OH2B KIRKKILA, FINLAND 28.200 CS3B MADERIA IS 28.200 LU4AA ARGENTINA 28.200 OA4B PERU 28.200 YV5B CARACAS, VEN 28.200 4U1UN UNITED NATIONS 28.200 VE8AT CANADA 28.200 W6WX SAN JOSE, CA 28.200 KH6WO HONOLULU, HI 28.200 ZL6B NEW ZEALAND 28.200 VK6RBP AUSTRALIA 28.200 JA2IGY MT ASAMA, JAPAN 28.200 RR9O NOVOSIBIRSK RUSSIA 28.200 VR2R HONG KONG CHINA
  • 43. BEACONS (HF)1.8170 - 24.9860 MHZ (THERE ARE MANY MORE!!!!) N/A N/A Fukushima QM07 24.9860 JE7YNQ dipole N-S 10 Hamburg-Rothenburgsort JO53AM 24.9310 DK0HHH GP 2 Bologna(Marconi Memorial) JN54OK 24.9200 IY4M 2 dipoles 12 N/A JN63KR 24.9150 IK6BAK slope dipole 4 Porto Alegre, 85m asl GF49KX 21.3935v PY3PSI N/A 220m Crabbe Mtn, NB FN66 21.1455 VE9BEA/B vertic.AV640 50 off (Kihei/Maui, HI) N/A 21.1420 KH6AP 1/2 vertical 1 Cerro Jefe FJ09HD 18.0990 HP1AVS/B N/A N/A South Atlantic N/A 14.0460 LU0ARC Horiz.loop 30 Scheggerott JO44VQ 10.1440 DK0WCY N/A N/A off (ausser Betrieb) N/A 10.1400 HB9TC dipole N-S 2 Porto Alegre, 85m asl GF49KX 10.1400 PY3PSI vertical 2 testing,intermittant FJ09HD 10.1390 HP1RCP/B dipole 500m Kladno JO70BC 10.1340 OK0EF N/A N/A Plettenberg Bay KF16PF 10.1235 ZS1J/B dipole 1 George Airport KF16EA 7.0250 ZS1AGI dipole 150m Kam.Zehrovice JO70AC 3.6000 OK0EN N/A N/A Plettenberg Bay KF16PF 3.5865 ZS1J/B dipole 30 Scheggerott JO44VQ 3.5790 DK0WCY N/A N/A N/A N/A 1.8450 OK0EV N/A N/A Plettenberg Bay KF16PF 1.8170 ZS1J/B ANTENNA POWER LOCATION GRID FREQUENCY CALLSIGN
  • 44. MF, HF CRITICAL FREQUENCIES
  • 45. MF, HF CRITICAL FREQUENCIES CONT’D
  • 46.
  • 47.
  • 48. UHF, VHF, SPORADIC E, AURORAS, DUCTING Auroral Effects: Borealis or Northern Lights is evidence of strong ionization in the upper atmosphere and can be utilized to reflect signals. Requires a relatively high power transmitter and both stations point their antennas north toward the aurora. The preferred mode when working VHF aurora is CW although SSB can be used at 50 MHz. The received tone quality when using CW is very different than what you may be used to. Characteristic buzz, echo, very raspy and garbled tones can be expected. The reason auroral signals sound different is they are being reflected by changing and rapidly-moving reflector (the ionised gases in the aurora). This results in multi-path reflections and the introduction of doppler shift into the signals.
  • 49.
  • 50. UHF, VHF, SPORADIC E, AURORAS, DUCTING
  • 51.
  • 52. SCATTER, HF, VHF,UHF Trans-Equatorial Scatter: it possible for DX reception of television and radio stations between 3000–5000 miles or 4827–8045Km across the equator on frequencies as high as 432MHz., DX reception of lower frequencies in the 30–70MHz range is far more common. For this mode to work both transmitting and receiving stations should be almost the same distance from the equator. Aircraft Scatter (Tropospheric Reflection): reflection off aircraft, (reflections off of flocks of birds are also possible). A rare form of reflection is "Chaf Scatter“(strips of metal foil sent out by the military during training exercises). Chaf helps to confuse enemy radars. but also helps to produce DX. Maximum distances for all reflection modes are again up to 800 km (500 mi). Rain Scatter : A band of very heavy rain (or rain and hail) can scatter or even reflect signals. Distances are typically around 160 km. though up to 650 km (400 mi) is theoretically possible. (Note that heavy snow is not an useful reflector). Ice Pellet Scatter (called Sleet Scatter in the US). is similar to Rain Scatter but is caused by bands of Ice Pellets in the wintertime.
  • 53. SCATTER, HF, VHF,UHF Meteor Scatter: as Meteors burn up entering the atmosphere it creates a quantity of ionized particles which reflect VHF radio waves. CW or SSB can make several rapid contacts during the brief openings that do occur. These openings may last from a few seconds to a minute or so. Lightning Scatter: there is little documentation on it but the theory is that lightning strikes produce ionized trails a mode that is very hard to distinguish and rarely reported.
  • 54. SCATTER, HF, VHF,UHF Scatter propagation would best be used by two stations within each other’s skip zone on a certain frequency. If you receive a weak, distorted signal from a distance, and close to maximum usable frequency, scatter propagation is probably occurring. A wavering sound is characteristic of HF scatter signals Energy scattered into the skip zone through several radio-wave paths makes HF scatter Signals often sound distorted. HF scatter signals are usually weak because only a small part of the signal energy is scattered into the skip zone. Scatter propagation allows a signal to be detected at a distance to far for ground-wave propagation but to near for normal sky-wave propagation. Scatter propagation on the HF bands most often occurs when communicating on frequencies above the maximum usable frequency (MUF) Side, Back, and Forward, Meteor, Ionospheric, and Tropospheric are all scatter modes. Inverted and Absorption are NOT scatter modes. In the 30 – 100 MHz frequency range, meteor scatter is the most effective for extended-range communications. Meteor scatter is the most effective on the 6 metre band .
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  • 56.