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A '''ionosonde''', or '''chirpsounder''', is a special [[radar]] for the examination of the [[ionosphere]]. An ionosonde consists of:
A '''ionosonde''', or '''chirpsounder''', is a special [[radar]] for the examination of the [[ionosphere]]. An ionosonde consists of:


* A [[high frequency]] (HF) transmitter, automatically tunable over a wide range. Typically the frequency coverage is 0.5–23 MHz or 1–40 MHz, though normally sweeps are confined to approximately 1.6–12 MHz.
* A [[high frequency]] (HF) transmitter, automatically tunable over a wide range. Typically the frequency coverage is 0.5–23 MHz or 1–40 MHz, though normally sweeps are confined to approximately 1.6–12 MHz.
* A tracking HF receiver which can automatically track the frequency of the transmitter.
* A tracking HF receiver which can automatically track the frequency of the transmitter.
* An antenna with a suitable radiation pattern, which transmits well vertically upwards and is efficient over the whole frequency range used.
* An antenna with a suitable radiation pattern, which transmits well vertically upwards and is efficient over the whole frequency range used.
* Digital control and data analysis circuits.
* Digital control and data analysis circuits.


The transmitter sweeps all or part of the HF frequency range, transmitting short pulses. These pulses are reflected at various layers of the ionosphere, at heights of 100–400 km, and their echos are received by the receiver and analyzed by the control system. The result is displayed in the form of an [[ionogram]], a graph of reflection height (actually time between transmission and reception of pulse) versus carrier frequency.
The transmitter sweeps all or part of the HF frequency range, transmitting short pulses. These pulses are reflected at various layers of the ionosphere, at heights of 100–400 km, and their echos are received by the receiver and analyzed by the control system. The result is displayed in the form of an [[ionogram]], a graph of reflection height (actually time between transmission and reception of pulse) versus carrier frequency.


The basic ionosonde technology was invented in 1925 by [[Gregory Breit]] and [[Merle A. Tuve]] <ref name="Judd1988">{{cite book|publisher=Heinemann|title=Radio Wave Propagation (HF Bands)|author=F.C. Judd, G2BCX|year=1987|location=London|isbn=0-434-90926-2|pages=12–20,27–37}}</ref> and further developed in the late 1920s by a number of prominent physicists, including [[Edward Victor Appleton]]. The term ''[[ionosphere]]'' and hence, the etymology of its derivatives, was proposed by [[Robert Watson-Watt]].
The basic ionosonde technology was invented in 1925 by [[Gregory Breit]] and [[Merle A. Tuve]] <ref name="Judd1988">{{cite book|publisher=Heinemann|title=Radio Wave Propagation (HF Bands)|author=F.C. Judd, G2BCX|year=1987|location=London|isbn=0-434-90926-2|pages=12–20,27–37}}</ref> and further developed in the late 1920s by a number of prominent physicists, including [[Edward Victor Appleton]]. The term ''[[ionosphere]]'' and hence, the etymology of its derivatives, was proposed by [[Robert Watson-Watt]].
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*http://www.sil.sk.ca/cadi.html : Canadian Advanced Digital Ionosonde (CADI)
*http://www.sil.sk.ca/cadi.html : Canadian Advanced Digital Ionosonde (CADI)
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{{refend}}



{{Uncategorized|date=August 2010}}



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{{geophysics-stub}}

Revision as of 02:37, 29 August 2010

Typical ionogram indicating foF2 of approximately 5.4 MHz.

A ionosonde, or chirpsounder, is a special radar for the examination of the ionosphere. An ionosonde consists of:

  • A high frequency (HF) transmitter, automatically tunable over a wide range. Typically the frequency coverage is 0.5–23 MHz or 1–40 MHz, though normally sweeps are confined to approximately 1.6–12 MHz.
  • A tracking HF receiver which can automatically track the frequency of the transmitter.
  • An antenna with a suitable radiation pattern, which transmits well vertically upwards and is efficient over the whole frequency range used.
  • Digital control and data analysis circuits.

The transmitter sweeps all or part of the HF frequency range, transmitting short pulses. These pulses are reflected at various layers of the ionosphere, at heights of 100–400 km, and their echos are received by the receiver and analyzed by the control system. The result is displayed in the form of an ionogram, a graph of reflection height (actually time between transmission and reception of pulse) versus carrier frequency.

The basic ionosonde technology was invented in 1925 by Gregory Breit and Merle A. Tuve [1] and further developed in the late 1920s by a number of prominent physicists, including Edward Victor Appleton. The term ionosphere and hence, the etymology of its derivatives, was proposed by Robert Watson-Watt.

An ionosonde is used for finding the optimum operation frequencies for broadcasts or two-way communications in the high frequency range.

See also

References

  1. ^ F.C. Judd, G2BCX (1987). Radio Wave Propagation (HF Bands). London: Heinemann. pp. 12–20, 27–37. ISBN 0-434-90926-2.{{cite book}}: CS1 maint: numeric names: authors list (link)

Further reading

  • Gwyn Williams, G4FKH (2009). "Interpreting Digital Ionograms". RadCom. 85 (05). RSGB: 44–46. {{cite journal}}: Unknown parameter |month= ignored (help)CS1 maint: numeric names: authors list (link)
  • Breit, G. and Tuve, M.A. (1926). "A Test of the Existence of the Conducting Layer". Physical Review. 28 (3): 554–575. doi:10.1103/PhysRev.28.554.{{cite journal}}: CS1 maint: multiple names: authors list (link)
  • Appleton, E. V. (1931). "The Timing of Wireless Echoes, the use of television and picture transmission". Wireless World (14): 43–44. {{cite journal}}: Unknown parameter |month= ignored (help)



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