• DocumentCode
    3359675
  • Title

    Calibration of scanning low frequency microwave radiometer

  • Author

    Prytz, A. ; Heron, M.L. ; Burrage, D.M. ; Goodberlet, M.

  • Author_Institution
    James Cook Univ., Townsville, Qld., Australia
  • Volume
    4
  • fYear
    2002
  • fDate
    29-31 Oct. 2002
  • Firstpage
    2003
  • Abstract
    The scanning low frequency radiometer (SLFMR) is a narrow-band (24 MHz) radiometer operating at 1.413 GHz. It uses a Dicke-switched reference load and a sensor to match a noise temperature to the brightness temperature of a target. A Butler matrix is used to steer an 8 × 8 phased array antenna into eight beam directions. Calibration is required to obtain sea surface salinity estimates from the instrument as it is flown over an area to be mapped. Sea surface temperature, sea state, beam incidence angle and downwelling brightness temperature of the air affect the instrument readings. Consideration must also be given to the effect of solar and galactic radiation reflected off the sea surface into the instrument. This paper focuses on instrument calibrations which are needed to account for the effects of various temperatures measured by sensors at key locations within the instrument. Calibration of the SLFMR was performed by Prosensing before delivery, but it became clear that re-calibration was necessary for each flying campaign. Long-term stability of the instrument and appropriate calibration parameters in light of those suggested by the manufacturer are discussed. These are second-order corrections which arise from small variations in temperature $the whole cabinet has a feedback control loop to hold the cabinet temperature at a nominal 40°C. A multivariate linear approach is used to calibrate the instrument for a set of coefficients associated with the temperature measurements. Coefficients were evaluated for all beam positions and checks were made with the SLFMR pointing upwards to scan across known sources of the sun, moon and the centre of the galaxy. Further calculations were made in a room where the target temperature was kept constant. These calibration procedures removed imbalances between the responses at different beam positions. Success of the procedure is demonstrated with some early salinity maps made in the Great Barrier Reef Lagoon in north-east Australia.
  • Keywords
    atmospheric radiation; oceanographic techniques; radiometry; temperature; 1.413 GHz; 24 MHz; Butler matrix; Dicke-switched reference load; Great Barrier Reef Lagoon; Moon; Prosensing; SLFMR; Sun; array antenna; beam incidence angle; beam position; brightness temperature; cabinet temperature; calibration parameter; downwelling brightness temperature; eight beam direction; feedback control loop; galactic radiation; galaxy centre; long-term stability; multivariate linear approach; narrow-band radiometer; noise temperature; north-east Australia; salinity maps; scanning low frequency microwave radiometer; sea surface salinity; sea surface temperature; second-order correction; sensor; small variation; solar radiation; target temperature; Brightness temperature; Calibration; Frequency; Instruments; Microwave radiometry; Ocean temperature; Phased arrays; Sea surface; Temperature measurement; Temperature sensors;
  • fLanguage
    English
  • Publisher
    ieee
  • Conference_Titel
    OCEANS '02 MTS/IEEE
  • Print_ISBN
    0-7803-7534-3
  • Type

    conf

  • DOI
    10.1109/OCEANS.2002.1191940
  • Filename
    1191940