Serylak, MaciejFallows, Richard A.Forte, Biagio2021-02-082021-02-082020Maciej S , Fallows RA, Forte B, Astin I, Allbrook T, et al. 2020. A LOFAR observation of ionospheric scintillation from two simultaneous travelling ionospheric disturbances. J. Space Weather Space Clim. 10, 10.2115-7251https://doi.org/10.1051/swsc/2020010http://hdl.handle.net/10566/5846This paper presents the results from one of the first observations of ionospheric scintillation taken using the Low-Frequency Array (LOFAR). The observation was of the strong natural radio source Cassiopeia A, taken overnight on 18–19 August 2013, and exhibited moderately strong scattering effects in dynamic spectra of intensity received across an observing bandwidth of 10–80 MHz. Delay-Doppler spectra (the 2-D FFT of the dynamic spectrum) from the first hour of observation showed two discrete parabolic arcs, one with a steep curvature and the other shallow, which can be used to provide estimates of the distance to, and velocity of, the scattering plasma. A cross-correlation analysis of data received by the dense array of stations in the LOFAR “core” reveals two different velocities in the scintillation pattern: a primary velocity of ~20–40 ms 1 with a north-west to south-east direction, associated with the steep parabolic arc and a scattering altitude in the F-region or higher, and a secondary velocity of ~110 ms 1 with a north-east to south-west direction, associated with the shallow arc and a scattering altitude in the D-region. Geomagnetic activity was low in the mid-latitudes at the time, but a weak sub-storm at high latitudes reached its peak at the start of the observation.enIonospheric scintillationTravelling ionospheric disturbancesInstability mechanismsRadio wavesLow-frequency arrayArticle