TY - JOUR
T1 - STUDY OF A METHOD FOR EXTRACTING SMALL-SCALE TOPOGRAPHIC IRREGULARITIES USING WAVELET ANALYSIS MAPS
AU - Imanishi, Masafumi
AU - Nakamura, Koichi
AU - Nishiyama, Satoshi
N1 - Publisher Copyright:
© Int. J. of GEOMATE All rights reserved, including making copies, unless permission is obtained from the copyright proprietors.
PY - 2023
Y1 - 2023
N2 - Microtopography and topographic parameter maps created from aerial laser profiler (LP) survey data are increasingly being used for business purposes. Wavelet analysis maps, unlike slope gradation maps, can be used to extract topographic irregularities without being affected by slope inclinations. First, a simulated terrain was created by changing the slope and the size of steps, and the size of steps that can be represented by a wavelet analysis map and by a slope gradation map was examined. Next, we examined the size of steps that can be extracted from the wavelet analysis and the slope gradation map for a slope with an average value of approximately 40 degrees, including the source of falling rocks, by using the results of the field survey. The size of the steps that can be extracted from the wavelet analysis map is approximately 2 m, and with the slope gradation map, it is more than 4 m. Hence, the wavelet analysis map is more accurate than the slope gradation map. Therefore, the wavelet analysis map can be used to extract smaller steps than those obtained with the slope gradation map.
AB - Microtopography and topographic parameter maps created from aerial laser profiler (LP) survey data are increasingly being used for business purposes. Wavelet analysis maps, unlike slope gradation maps, can be used to extract topographic irregularities without being affected by slope inclinations. First, a simulated terrain was created by changing the slope and the size of steps, and the size of steps that can be represented by a wavelet analysis map and by a slope gradation map was examined. Next, we examined the size of steps that can be extracted from the wavelet analysis and the slope gradation map for a slope with an average value of approximately 40 degrees, including the source of falling rocks, by using the results of the field survey. The size of the steps that can be extracted from the wavelet analysis map is approximately 2 m, and with the slope gradation map, it is more than 4 m. Hence, the wavelet analysis map is more accurate than the slope gradation map. Therefore, the wavelet analysis map can be used to extract smaller steps than those obtained with the slope gradation map.
KW - Aerial laser survey
KW - Microtopography
KW - Terrain interpretation
KW - Wavelet analysis map
UR - https://www.scopus.com/pages/publications/85172295752
UR - https://www.scopus.com/pages/publications/85172295752#tab=citedBy
U2 - 10.21660/2023.110.3941
DO - 10.21660/2023.110.3941
M3 - Article
AN - SCOPUS:85172295752
SN - 2186-2982
VL - 25
SP - 148
EP - 158
JO - International Journal of GEOMATE
JF - International Journal of GEOMATE
IS - 110
ER -