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In this regard, the shortest distance from one concept to each concept in the concept map is extracted.
The PGA map is extracted from the United States Geology Survey (U.S.G.S) Shakemap (http://earthquake.usgs.gov/earthquakes/shakemap) (see Table 2).
Depicted BS information on the map is extracted from a website [6] which makes use of the Australian Communications and Media Authority's [7] RadCom registry.
Once the saliency map is extracted (using the visual attention method), we apply a Linear Discriminant Analysis (LDA) [9] to estimate the probability of object presence.
Then the texture saliency map is extracted with the local phase of hypercomplex, which is constructed by the detail signal of stationary wavelet transform (SWT) and its Hilbert transform.
This map is extracted from the geologic map of the Mesozoic basin of the Sahara Algero-Tunisian (Busson [1967]). 1 Miocene or Pliocene (with locally continental nummulitic), 2 Quaternary, 3 Pliocene or former Quaternary, 4 upper middle Eocene, 5 dunes, 6 chotts.
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The slope map was extracted from Aster DEM with resolution 30 m using spatial analyst tools.
The map was extracted from HWSD V1.1 produced by FAO which was having a resolution of 30″ × 30″ (FAO/IIASA/ISRIC/ISSCAS/JRC 2009).
Taking a certain area as the observation object, the indexes related to the map were extracted, including the road network characteristics and change rate of concerned points.
A slope thematic map was extracted from the LiDAR high-resolution DEM of the area with a spatial resolution of 5 m (Fig. 3).
Slope angle: The slope map was extracted from the DEM (30 m resolution) and classified into five classes: 0° - 5°, 6° - 15°, 16° - 25°, 26° - 35° and ≥ 35°.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com