Exact(21)
Figure 6(a) illustrates the initial mass layer with the according geoid height differences plotted in Fig. 6(b) after applying the effect of the simulated mass layer.
The mass layer is further improved according the height increments given in Table 1.
(c) Simulated mass layer after the 100th iteration step with a height increment of 100 m.
Before we analyse the SEGM, we illustrate how the algorithm optimises the mass layer.
Effect on the synthetic geoid height N (b) caused by the optimised mass layer.
Quantitative results of the effect of the mass layer stiffness on wave frequencies are presented.
Similar(39)
For example, the layered structure of the Earth's interior can be modelled by a series of mass layers at different depths.
An innovative approach to characterize concentration of atmospheric aerosol particles and air mass layering along the elevation profile of glaciers is presented for the first time and validated, exploiting low weight and fast response sensors deployed on a snowmobile.
In order to improve the mass model further the developed procedure can be applied to practically an arbitrary number of mass sources (e.g., mass layers), thus it offers the possibility to incorporate other geophysical information on the Earth's interior.
The reason for the regional geoid anomaly in the Andes can be explained by sudden geoid height changes due to the presence of three different mass layers at three different depth levels that combine to produce the total regional geoid anomaly (Bowin, 2000; Lucassen et al., 2001; Tassara et al., 2006).
They are characterized by parameters such as: mass, length, layer, level, phase of construction process when element is used or produced.
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