Projection-Based Spatial Morphology for Extracting Ridge and Valley Profiles of Mountains from 3D Amorphous Data

Author(s):  
Rajesh K Maurya ◽  
Sushil T. Kulkarni ◽  
Nehal Kalita
2013 ◽  
Vol 15 (2) ◽  
pp. 297 ◽  
Author(s):  
Zhiqing ZHANG ◽  
Dunxin JIA ◽  
Shihu DENG ◽  
Xianfeng JIN

2013 ◽  
Vol 368-370 ◽  
pp. 78-82
Author(s):  
Ping Shu ◽  
Jun Xu ◽  
Li Jun Wang

Based on theoretical studies of the urban spatial morphology, this paper introduces advanced concepts and methods of BIM (Building Information Model) into the urban design in Nanhe City ,and then respectively makes innovations of the urban design practice supported by BIM technology in the process of design, optimization and implementation of the program, attempting to explore BIM-based design patterns of the urban spatial morphology to make the traditional urban design process more rational and scientific, to expect to reach the green and sustainable urban spatial morphology.


2018 ◽  
Vol 12 (03) ◽  
pp. 1850007 ◽  
Author(s):  
J. P. Narayan ◽  
A. Kumar

The effects of ridge and valley on the characteristics of Rayleigh waves are presented in this paper. The research work carried out has been stimulated by the day by day increase of long-span structures in the hilly areas which are largely affected by the spatial variability in ground motion caused by the high-frequency Rayleigh waves. The Rayleigh wave responses of the considered triangular and elliptical ridge and valley models were computed using a fourth-order accurate staggered-grid viscoelastic P-SV wave finite-difference (FD) program. The simulated results revealed very large amplification of the horizontal component and de-amplification of the vertical component of Rayleigh wave at the top of a triangular ridge and de-amplification of both the components at the base of the triangular valley. The observed amplification of both the components of Rayleigh wave in front of elliptical valley was larger than triangular valley models. A splitting of the Rayleigh wave wavelet was inferred after interaction with ridge and valley. It is concluded that the large-scale topography acts as a natural insulator for the surface waves and the insulating capacity of the valley is more than that of a ridge. This insulation phenomenon is arising due to the reflection, diffraction and splitting of the surface wave while moving across the topography. It is concluded that insulating potential of the topography for the Rayleigh waves largely depends on their shape and shape-ratio.


2013 ◽  
Vol 96 (8) ◽  
pp. 2454-2460 ◽  
Author(s):  
Abbas Hodroj ◽  
Patrick Simon ◽  
Pierre Florian ◽  
Marie-Hélène Chopinet ◽  
Yann Vaills

Forests ◽  
2016 ◽  
Vol 7 (12) ◽  
pp. 224 ◽  
Author(s):  
Joseph Marschall ◽  
Michael Stambaugh ◽  
Benjamin Jones ◽  
Richard Guyette ◽  
Patrick Brose ◽  
...  

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