2017
DOI: 10.1515/jag-2016-0042
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Intrinsic random functions for mitigation of atmospheric effects in terrestrial radar interferometry

Abstract: The benefits of terrestrial radar interferometry (TRI) for deformation monitoring are restricted by the influence of changing meteorological conditions contaminating the potentially highly precise measurements with spurious deformations. This is especially the case when the measurement setup includes long distances between instrument and objects of interest and the topography affecting atmospheric refraction is complex. These situations are typically encountered with geo-monitoring in mountainous regions, e.g.… Show more

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Cited by 8 publications
(3 citation statements)
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“…If the location of an object relative to the radar instrument does not change and all other influences are constant, the phase value in the corresponding bins of the radar image remains the same for subsequent measurements. However, in most practical situations, drifts caused by changing environmental conditions (e.g., temperature and humidity [42,43]) as well as instrumental effects (e.g., stability of tripod and sensor chip temperature) are to be expected on top of noise. Figure 10a-d shows examples of time series of phase values acquired in the previously described indoor and outdoor experiments.…”
Section: Meteorological Impactsmentioning
confidence: 99%
“…If the location of an object relative to the radar instrument does not change and all other influences are constant, the phase value in the corresponding bins of the radar image remains the same for subsequent measurements. However, in most practical situations, drifts caused by changing environmental conditions (e.g., temperature and humidity [42,43]) as well as instrumental effects (e.g., stability of tripod and sensor chip temperature) are to be expected on top of noise. Figure 10a-d shows examples of time series of phase values acquired in the previously described indoor and outdoor experiments.…”
Section: Meteorological Impactsmentioning
confidence: 99%
“…Because the universal Kriging process falls into a circular problem where the drift form should be known in the Kriging system although the drift form should be estimated through the universal Kriging system, we herein apply the IRFk Kriging to predict res φ . The IRF-k Kriging is introduced for the simultaneous estimation of the drift model and the covariance function [28], [36]. In this method, the drift and the covariance are decomposed through increments of a sufficient order to filter out the drift and achieve stationarity [26].…”
Section: B Residual Aps Prediction In Spacementioning
confidence: 99%
“…Precise analysis of the structural characteristic by the geostatistical approach is thus appropriate for modeling of the short-scale APS component based on the elementary Kolmogorov turbulence theory [27]. Therefore, the analysis and inference of the structure-function and the covariance are essential to mitigate the fluctuated APS [15], [28]. Under the second-order stationarity assumption, the covariance function is inferred by a theoretical variogram to model the uncertain spatial variation [29].…”
Section: Introductionmentioning
confidence: 99%