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By using optimization methods and geometric methods, the boundaries of the studied angular errors are determined with reduced computation complexity.
Phase and attenuation errors are determined analytically across the entire frequency band of the low-loss single-resonance Lorentz model.
Additional infrastructure was used with the differential concept (where range errors are determined at a known location and transmitted to users) to improve this to the level of a few metres.
To estimate the geoid model, the well-known remove-compute-restore method is used while residual geoid heights are estimated through least-squares collocation so that associated errors are determined as well.
Figure 3a shows a series of AFM images obtained for different incubation times on the water/propanol (99.8/0.2 wt/wt%) substrate, which has a surface energy of γs = 69 ± 1 mN m-1 and a spreading parameter of S = 21 ± 2 mN m-1, where the experimental errors are determined by the precision of the Wilhelmy plate method (see 'Langmuir Blodget monolayers' in the Methods).
Common errors are determined including changes of syllable structure, substitution, and assimilation.
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Constant, absolute and variable POG and rotational errors were determined.
A correction of extrapolation errors was determined by fitting binary equilibrium data to the IAS theory.
The effect of using intuitive anthropometric measurements as parameters is examined and the sensitivity to measurement errors is determined.
Then the T&D model uncertainty associated with input wind errors were determined by comparing plumes calculated using wind directions varied at 2° increments to the truth plume.
The priority of the driving errors is determined dynamically by the prioritization module.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com