Abstract
In the course of the study, we have disclosed methods for correcting
and analyzing spatial data recorded in a vector format. The latter is
best suited for spatial analysis of discrete objects. However, in the
case when the spatial variable is represented as a field of #scalar or
vector magnitudes (for example, spatial concentration distribution of
concentrations of heavy metals in soils or the velocity field of
groundwater movement). Convenient ways of data recording is a raster
format. This approach is most often used for #phenomena of processes that
are characterized by significant anisotropy. However, the
characteristic feature of the inverse distance method is the fact that
the interpolated value at the measured point is equal to the measured
value.Figure 1 In it, the space consists of an infinite number of points and
is divided into a certain number of rectangular fields called pixels,
#mudflows, and a specific value is attributed [1]. Most often we own
limited information about the spatial layout of the variable being
studied. In general, our knowledge is reduced to a certain finite
measuring points, on the basis of which conclusions are drawn about the
possible distribution of quantities to the remaining points of space.
Data collection at measuring points can be considered as a random
series, based on which the forecasting of parameters outside the testing
points is performed. This process is called interpolation of spatial
data. There are many methods of interpolating data.
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Interpolation of Spatial Data by Rae Zh Aliyev in BJSTR
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