EISCAT UHF Incoherent scatter radar

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<?xml version="1.0" encoding="UTF-8"?>
<Instrument xmlns="https://metadata.pithia.eu/schemas/2.2" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:xlink="http://www.w3.org/1999/xlink" xsi:schemaLocation="https://metadata.pithia.eu/schemas/2.2 https://metadata.pithia.eu/schemas/2.2/pithia.xsd">
    <identifier>
        <PITHIA_Identifier>
          <localID>Instrument_EISCAT_UHF</localID>
            <namespace>eiscat</namespace>
            <version>1</version>
            <creationDate>2022-10-03T10:49:00Z</creationDate>
            <lastModificationDate>2022-10-19T09:01:02Z</lastModificationDate>
        </PITHIA_Identifier>
    </identifier>
    <name>EISCAT UHF Incoherent scatter radar</name>
    <description>
      An incoherent scatter radar transmits a radiowave of high power
      and a tiny fraction of the power is scattered back. The spectrum
      of the scattered signal depends on plasma waves propagating in
      the ionosphere and from the shape of the spectrum the
      temperature of electrons and ions can be determined. The
      scattered power or electron plasma frequency shift can give the
      electron density and the Doppler shift gives the ion drift
      velocity.  Being high power large aperture radars, the
      instruments are also useful for other purposes, including meteor
      research and space debris mapping.  The mainland UHF radar in
      Troms&#248; started observing in 1981. It operates at 930 MHz and has
      a fully steerable 32m dish antenna.
    </description>
    <type xlink:href="https://metadata.pithia.eu/ontology/2.2/instrumentType/IncoherentScatterRadar"/>
    <operationalMode><InstrumentOperationalMode>
        <id>isr</id>
        <name>IncoherentScatter</name>
        <description>
	  The main use of incoherent scatter radars is ionospheric
	  research, where coded pulses are transmitted and
	  received. Decoding gives autocorrelation function estimates
	  at selectable time and range resolutions, and theoretical
	  scatter spectra can be fitted to these using standard
	  Fourier transform theory. The UHF radar operates at 930 MHz
	  and is suitable for general ionospheric E-layer, F-layer and
	  topside measurements.
	</description>
    </InstrumentOperationalMode>
    </operationalMode>
</Instrument>