The EISCAT mesospheric measurements during the CAMP campaign

Computer Science – Sound

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Arctic Regions, D Region, Eiscat Radar System (Europe), Ionospheric Sounding, Mesosphere, Ionospheric Electron Density, Line Spectra, Mesopause, Negative Ions, Radar Echoes

Scientific paper

A brief outline is given of the experimental technique used during the Cold Arctic Mesopause Project (CAMP) to record the first D-region ion line spectra with the EISCAT incoherent-scatter radar. The data analysis shows that echoes from mesospheric heights between about 70 km and 90 km can be detected during disturbed periods of enhanced electron density during particle-precipitation events. Electron-density profiles were determined which show a fairly high density, up to 5 x 10 to the 10th/cu m in the upper D-region. The measured meridional winds were lower than 10 m/s. A fit of the measured height profile of spectral width to temperature and neutral-density models yielded a measured temperature profile in good agreement with simultaneous rocket data. The mesopause temperature was determined to be as low as 130 K. This detailed analysis of the spectral-width profile indicates that below about 77-80 km the ratio of negative ions to electrons exceeded unity. Finally, some discussions are added on the limitations and significance of these first mesosphere observations.

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