1995
DOI: 10.1029/94rs03183
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Mode angles of arrival in the 55‐ to 3500‐km range

Abstract: A direction‐finding ionosonde consisting of an interferometer using seven‐element, 50‐ and 150‐meter crossed baselines, has been developed to provide group path delay, azimuth, and elevation of each resolved mode over the sounding frequency range. Direction‐finding (DF) ionograms have been acquired automatically, using various noncooperative, compatible sounder transmissions. Diurnal sequences of DF ionograms were obtained for mid‐latitude paths at nominal ranges of 55‐, 1000‐, 2300‐ and 3500‐km. Data measured… Show more

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Cited by 7 publications
(4 citation statements)
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“…Important parameters for NVIS antenna optimization are antenna diagram, polarization and bandwidth. As only high elevation angles contribute to NVIS propagation [55], optimizing the antenna diagram for these elevation angles will increase the effectively transmitted power and improve the signalto-interference ratio at reception.…”
Section: Nvis Antennasmentioning
confidence: 99%
“…Important parameters for NVIS antenna optimization are antenna diagram, polarization and bandwidth. As only high elevation angles contribute to NVIS propagation [55], optimizing the antenna diagram for these elevation angles will increase the effectively transmitted power and improve the signalto-interference ratio at reception.…”
Section: Nvis Antennasmentioning
confidence: 99%
“…The raw data collected from the SSL included the azimuth and elevation angles, as well as the signal strength for the signal recorded in each frame. In addition, a phase linear error that describes the deviation from plane wave conditions of the phase resolution across the array was recorded for each frame [7]. Typical distributions in azimuth and elevation are shown in Figure 2…”
Section: Cit Experimentsmentioning
confidence: 99%
“…In this paper, we analyze direction finding (DF) sounding measurements originally reported by Black et al [1995] on one-and two-hop modes, comparing one-hop angular spread resulting from a single traverse of the ionosphere with two-hop angular spread including two ionospheric traverses plus a ground scatter at the path midpoint. We use this data to separate the ionospheric from the ground scatter components of azimuth spread and estimate the ground scatter component separately for two types of terrain.…”
Section: Introductionmentioning
confidence: 99%