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Presented by
Muhammad Safdar
Outline
 Introduction of A Study Area
 Interpolation
 Spatial Interpolation & Methods
- Spline
- Inverse Distance Weighting(IDW)
- Kriging
 Methodology
- Study site
 Data Collection Process & Representation Tools
 Results
 Conclusion
Introduction of A Study Area
 In a pilot Area of Caracas, Venezuela
 Frequency range of 100 kHz to 6 GHz
 Taking 35 samples per second during a 6
minutes , 206 measurements points
 Data points spaced approximately 100m
from each other is fixed over the 2.64km2
pilot area
Interpolation?
 Interpolation is a method of constructing
new data points within the range of a
discrete set of known data points.
Spatial Interpolation?
 Interpolation predicts values for cells in a raster from a
limited number of sample data points. It can be used to
predict unknown values for any geographic point data:
elevation, rainfall, chemical concentrations, noise levels,
and so on.
Spatial Interpolation Methods
1.Spline
 method estimates values using a mathematical function
that minimizes the total surface curvature, resulting in a
smooth surface that passes exactly through the
sampled points
2.Inverse Distance Weighting(IDW)
• is based on the assumption that the nearby values
contribute more to the interpolated values than
distant observations.
3. Kriging
 depends on spatial and statistical relationships to
calculate the surface.
Methodology
Study Site.
The measurements were taken in a pilot zone of Caracas,
Venezuela(Figure 1)with an approximate area of 2.64km2,
which represents 0.609% of the total geographical area of
the Caracas. A total of 206 measurements points, were
selected over the pilot zone. This area is characterized by
a dynamic economic-business activity which is evident
given the presence of shopping centers, office buildings of
the national telephone operators and other
telecommunications companies. On the other hand, this
area also boasts a large number of hospitals and schools,
which is of interest to know the impact of electromagnetic
fields.
Data Collection Process
 Time considerations :
Measurements were taken over a period of 30 days, from
February 15th to March 15th of 2010. Measurements
were performed only on working days (from Mondays
to Fridays).Each measurement was taken between
8:00 am and 5:00 pm.
 Geographical considerations:
each measurement point geographical coordinates were
taken using a GPS navigation unit.
 Measurement considerations:
Data Process and Representation Tools
 Two informatics tools
1: GvSIG 1.9
2: Past 2.02. GvSIG is a Geographic Information
System (GIS)
Both free software tools distributed under the
GNU/GPL license.
Results
Magnitude. (a) IDW, (b) SPLINES, (c) KRIGING.
.
Table 1. Results of the measures of ¯t applied to the interpolation
methods.
MEASURES MAE MSE
D (V/m)
Max Error Min Error
OF FIT (V/m) (V/m)
2
(V/m) (V/m)
IDW 0.17 0.05 1.01 0.55 0.008
KRINGING 0.74 0.73 3.81 1.66 0.111
SPLINE 0.89 1.11 4.71 1.98 0.034
.
AverageMagnitud
e(V/m)
EstimatedElectricField
Comparison of Spatial Interpolation Methods IDW, KIRGING and SPLINE
for Estimation of Average Electric Fiels Magnitude
3
2.5
2
1.5
1
0.5 Perfect prediction
IDW Method
KRIGING Method
SPLINE Method
Upper acceptance limit
0 Lower acceptance limit
0 0.5 1 1.5 2 2.5 3
Measured Electric Field Average Magnitude (V/m)
.
.
Conclusion
This study has shown that IDW interpolation
method is most likely to produce the best
estimation of a continuous surface of the
average magnitude of electric field intensity.
The IDW method exactness was superior to
the one shown by the SPLINES and
KRIGING techniques.
Thanks
Questions?

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Presentation adv gis 08 01-2014

  • 2. Outline  Introduction of A Study Area  Interpolation  Spatial Interpolation & Methods - Spline - Inverse Distance Weighting(IDW) - Kriging  Methodology - Study site  Data Collection Process & Representation Tools  Results  Conclusion
  • 3. Introduction of A Study Area  In a pilot Area of Caracas, Venezuela  Frequency range of 100 kHz to 6 GHz  Taking 35 samples per second during a 6 minutes , 206 measurements points  Data points spaced approximately 100m from each other is fixed over the 2.64km2 pilot area
  • 4. Interpolation?  Interpolation is a method of constructing new data points within the range of a discrete set of known data points.
  • 5. Spatial Interpolation?  Interpolation predicts values for cells in a raster from a limited number of sample data points. It can be used to predict unknown values for any geographic point data: elevation, rainfall, chemical concentrations, noise levels, and so on.
  • 6. Spatial Interpolation Methods 1.Spline  method estimates values using a mathematical function that minimizes the total surface curvature, resulting in a smooth surface that passes exactly through the sampled points 2.Inverse Distance Weighting(IDW) • is based on the assumption that the nearby values contribute more to the interpolated values than distant observations. 3. Kriging  depends on spatial and statistical relationships to calculate the surface.
  • 7. Methodology Study Site. The measurements were taken in a pilot zone of Caracas, Venezuela(Figure 1)with an approximate area of 2.64km2, which represents 0.609% of the total geographical area of the Caracas. A total of 206 measurements points, were selected over the pilot zone. This area is characterized by a dynamic economic-business activity which is evident given the presence of shopping centers, office buildings of the national telephone operators and other telecommunications companies. On the other hand, this area also boasts a large number of hospitals and schools, which is of interest to know the impact of electromagnetic fields.
  • 8.
  • 9. Data Collection Process  Time considerations : Measurements were taken over a period of 30 days, from February 15th to March 15th of 2010. Measurements were performed only on working days (from Mondays to Fridays).Each measurement was taken between 8:00 am and 5:00 pm.  Geographical considerations: each measurement point geographical coordinates were taken using a GPS navigation unit.  Measurement considerations:
  • 10. Data Process and Representation Tools  Two informatics tools 1: GvSIG 1.9 2: Past 2.02. GvSIG is a Geographic Information System (GIS) Both free software tools distributed under the GNU/GPL license.
  • 11. Results Magnitude. (a) IDW, (b) SPLINES, (c) KRIGING.
  • 12. . Table 1. Results of the measures of ¯t applied to the interpolation methods. MEASURES MAE MSE D (V/m) Max Error Min Error OF FIT (V/m) (V/m) 2 (V/m) (V/m) IDW 0.17 0.05 1.01 0.55 0.008 KRINGING 0.74 0.73 3.81 1.66 0.111 SPLINE 0.89 1.11 4.71 1.98 0.034
  • 13. . AverageMagnitud e(V/m) EstimatedElectricField Comparison of Spatial Interpolation Methods IDW, KIRGING and SPLINE for Estimation of Average Electric Fiels Magnitude 3 2.5 2 1.5 1 0.5 Perfect prediction IDW Method KRIGING Method SPLINE Method Upper acceptance limit 0 Lower acceptance limit 0 0.5 1 1.5 2 2.5 3 Measured Electric Field Average Magnitude (V/m)
  • 14. .
  • 15. .
  • 16. Conclusion This study has shown that IDW interpolation method is most likely to produce the best estimation of a continuous surface of the average magnitude of electric field intensity. The IDW method exactness was superior to the one shown by the SPLINES and KRIGING techniques.