
An ionosonde, or chirpsounder, is a special
radar for the examination of the
ionosphere
The ionosphere () is the ionized part of the upper atmosphere of Earth, from about to above sea level, a region that includes the thermosphere and parts of the mesosphere and exosphere. The ionosphere is ionized by solar radiation. It plays an ...
. The basic ionosonde technology was invented in 1925 by
Gregory Breit
Gregory Breit (russian: Григорий Альфредович Брейт-Шнайдер, ''Grigory Alfredovich Breit-Shneider''; July 14, 1899, Mykolaiv, Kherson Governorate – September 13, 1981, Salem, Oregon) was a Russian-born Jewish Am ...
and
Merle A. Tuve
Merle Anthony Tuve (June 27, 1901 – May 20, 1982) was an American geophysicist who was the Chairman of the Office of Scientific Research and Development's Section T, which was created in August 1940. He was founding director of the Johns Hopkins ...
and further developed in the late 1920s by a number of prominent physicists, including
Edward Victor Appleton
Sir Edward Victor Appleton (6 September 1892 – 21 April 1965) was an English physicist, Nobel Prize winner (1947) and pioneer in radiophysics. He studied, and was also employed as a lab technician, at Bradford College from 1909 to 1911.
He w ...
. The term ''
ionosphere
The ionosphere () is the ionized part of the upper atmosphere of Earth, from about to above sea level, a region that includes the thermosphere and parts of the mesosphere and exosphere. The ionosphere is ionized by solar radiation. It plays an ...
'' and hence, the etymology of its derivatives, was proposed by
Robert Watson-Watt.
Components
An ionosonde consists of:
* A
high frequency
High frequency (HF) is the ITU designation for the range of radio frequency electromagnetic waves (radio waves) between 3 and 30 megahertz (MHz). It is also known as the decameter band or decameter wave as its wavelengths range from one to ten ...
(HF) radio 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 (60 to 250 miles), 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.
An ionosonde is used for finding the optimum operation frequencies for broadcasts or two-way communications in the high frequency range.
Ionogram

An ionogram is a display of the data produced by an ionosonde; technically speaking one may call the data used to make the display as the ionogram but often this is simply implied. It is a graph of the virtual height of the ionosphere plotted against frequency. Ionograms are often converted into electron density profiles. Data from ionograms may be used to measure changes in the Earth's
ionosphere
The ionosphere () is the ionized part of the upper atmosphere of Earth, from about to above sea level, a region that includes the thermosphere and parts of the mesosphere and exosphere. The ionosphere is ionized by solar radiation. It plays an ...
due to
space weather events.
Note that in the ionogram above the legend can be more clearly understood as having "Vx-" and "Vx+" to replace respectively "X-" and "X+". These refer to the vertical reflection of the eXtraordinary kind. "Vo-" and "Vo+" refer to the Ordinary reflection. An Ordinarily reflected wave is the one that behaves as though there were no geomagnetic field.
ARTIST is the software program used to "scale" (deduce or calculate) the charasteristic parameter values shown in the table on the left. The version shown here is "5", which is the latest as of March 2022. Ion2Png is the software program used to create the image that we call ionogram.
Chirp transmitter
A
chirp
A chirp is a signal in which the frequency increases (''up-chirp'') or decreases (''down-chirp'') with time. In some sources, the term ''chirp'' is used interchangeably with sweep signal. It is commonly applied to sonar, radar, and laser system ...
transmitter is a
shortwave radio
Shortwave radio is radio transmission using shortwave (SW) radio frequencies. There is no official definition of the band, but the range always includes all of the high frequency band (HF), which extends from 3 to 30 MHz (100 to 10 me ...
transmitter that sweeps the
HF radio spectrum on a regular schedule. If one is monitoring a specific frequency, then a ''chirp'' is heard (in
CW or
SSB mode) when the signal passes through. In addition to their use in probing
ionospheric properties,
[Peter Martinez, G3PLX: Chirps and HF Propagation http://jcoppens.com/radio/prop/g3plx/index.en.php] these transmitters are also used for
over-the-horizon radar systems.
An analysis of current transmitters has been done using
SDR technology.
[Pieter-Tjerk de Boer, PA3FWM: Chirp Signals analyzed using SDR http://websdr.ewi.utwente.nl:8901/chirps/] For better identification of chirp transmitters the following notation is used:
:, where the repetition rate is the time between two sweeps in seconds and the chirp offset is the time of the first sweep from 0 MHz after a full hour in seconds. If the initial frequency is greater than 0 MHz, the offset time can be linearly extrapolated to 0 MHz.
See also
* Duga radar
* Ionosonde Juliusruh
* Radio propagation beacon
An amateur radio propagation beacon is a radio beacon, whose purpose is the investigation of the propagation of radio signals. Most radio propagation beacons use amateur radio frequencies. They can be found on LF, MF, HF, VHF, UHF, and micr ...
* Total electron content
* Trevor Wadley#Ionosonde
References
Further reading
*
*
*
*
* http://www.ngdc.noaa.gov/stp/IONO/ionogram.html National Geophysical Data Center
*
External links
*http://www.ngdc.noaa.gov/stp/iono/ionogram.html : NOAA Ionosonde portal to information and data services
*http://www.ngdc.noaa.gov/stp/IONO/Dynasonde/ : NOAA Dynasonde: Real-time Ionospheric Explorer by advanced and prototype analysis methods.
*http://aintel.bi.ehu.es/chirps-data/chirps.html
*http://ulcar.uml.edu/digisonde.html : Lowell Center for Atmospheric Research, MA, USA
*http://ulcar.uml.edu/stationlist.html : Ionosonde (partial) station list by location
* http://car.uml.edu/common/DIDBFastStationList : DIDBase Fast Station list
*http://www.iono.noa.gr : National Observatoy of Athens, Greece
*http://www.sil.sk.ca/content/cadi : Canadian Advanced Digital Ionosonde (CADI)
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