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On the phase changes between oscillations in the group and phase paths due to TIDs
Affiliation:1. Maritime Museum of San Diego, 1492 N. Harbor Dr., San Diego, CA 92101, USA;2. Department of Geosciences and Archaeology, Australian Museum, 1 William Street, Sydney, NSW 2010, Australia;3. School of Social Science, University of Queensland, Brisbane, QLD 4072, Australia;4. Department of Geosciences, University of Missouri Kansas City, 500 Holmes Street, Kansas City, MO 64110, USA
Abstract:The changes in phase path. ΔP, and group path, ΔP′, of a fixed frequency CW transmission were obtained over a ground range of ≈ 120 km. During the passage of TIDs through the ray path, changes in phase of 180° between ΔP and ΔP′ were found to occur over several cycles. A simple model incorporating moving triangular irregularities superimposed on a linear background electron density profile was used to calculate ΔP and ΔP′, and using this model, phase shifts between ΔP and ΔP′ were found which were similar to those encountered experimentally.
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