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As noted previously for each Doppler index, the reasons are manifold and include: inconsistent choice of the wall filter, divergent size of the sample volumes, manual or automatic curve analysis, varying size of the patient populations, different mathematical methods for the calculation of reference ranges, variations in the application of the Doppler technologies, varying observation intervals.
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These range variations are not observed in Figure 7(a).
Figure 3(a) gives time and ground range variations of the Doppler velocity on beams 1 11.
For example, an ambiguity might arise when minimum range variations are extracted from the radar data.
All range variations greater than the threshold (2 mm) were correctly detected.
Range-time power plot (a) for Beam 0 and the result of minimum range variations extraction (b).
Figure 6 displays time and ground range variations of the Doppler velocity and echo power between 1458 and 1510 JST.
The technique is based on cross-correlation analysis of the ground backscatter minimum range variations at different radar beams.
The technique is based on the analysis of minimum ground backscatter range variations corresponding to different radar beams.
Wide range variations have been observed in the geochemical data, which seem not controlled by organic richness and burial depth.
Using the third assumption, we can consider the minimum range variations caused by ionosphere variations that occur directly in the reflection point.
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