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Phase calibration of interferometer arrays at high‐frequency radars
Author(s) -
Burrell Angeline G.,
Yeoman Timothy K.,
Milan Stephen E.,
Lester Mark
Publication year - 2016
Publication title -
radio science
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.371
H-Index - 84
eISSN - 1944-799X
pISSN - 0048-6604
DOI - 10.1002/2016rs006089
Subject(s) - backscatter (email) , radar , interferometry , remote sensing , elevation (ballistics) , calibration , phase (matter) , geodesy , signal (programming language) , geology , physics , computer science , optics , telecommunications , wireless , quantum mechanics , astronomy , programming language
Elevation angles of backscattered signals are calculated at the Super Dual Auroral Radar Network (SuperDARN) high‐frequency radars using interferometric techniques. These elevation angles make it possible to estimate the geographic location of the scattering point, an essential piece of information for many ionospheric studies. One of the most difficult parameters to measure is the effective time delay caused by the difference in the electrical path length that connects the main array and the interferometer arrays to the correlator ( δ t c ). This time delay causes a bias in the measured difference in the signal phase, also known as a phase bias. Phase calibration is difficult due to unknown physical attributes of the hardware and the remote location of many radars. This leads to the possibility of sudden external changes, slow temporal drift, and a dependence on transmission frequency. However, it is possible to estimate δ t c using the radar observations themselves. This article presents a method for estimating δ t c using backscatter with a known location, such as backscatter from artificially generated irregularities, meteor echoes, or distinct groundscatter, which incorporates the uncertainty in the observations and may be used autonomously. Applying the estimated δ t c is shown to improve elevation angle uncertainties at one of the SuperDARN radars from their current potential tens of degrees to less than a degree.