نتایج جستجو برای: landform classification

تعداد نتایج: 493310  

Journal: :Remote Sensing 2021

Landform recognition is one of the most significant aspects geomorphology research, which essential tool for landform classification and understanding geomorphological processes. Watershed object-based a new spot in field recognition. However, relevant studies, quantitative description watershed generally focused on overall terrain features watershed, ignored spatial structure topological relat...

2011
J. M. Gong T. Zhang

As a typical landform class of Qinghai-Tibetan Plateau, glacier is widely distributed in alpine terrain. However, field measurement is impossible in those areas because of complex terrain and adverse weather. At first, on the basis of analyzing the features of glacier image spectrum, object shape, spatial relations and environment distribution including terrain and climate, this paper combines ...

2013
Wen Zhang Takashi Oguchi Yuichi S. Hayakawa Hua Peng

The “Danxia landform” is an erosional landform type originally defined in China. It is characterized by redcolored sandstones and steep cliffs, and developed via long-term erosion. Detailed quantitative geomorphometric studies of the characteristics of Danxia landforms in China have not yet been conducted. Using GIS, we conducted DEM-based geomorphometric analyses of 42 watersheds on Mt. Danxia...

2005
J. Vaze J. Teng N. K. Tuteja J. Gallant G. Summerell J. Young J. Wild

A GIS method for modeling landscapes to predict total soil depth and the depth of different soil layers is presented. The method is based on terrain analysis using a DEM and the combined use of the Topographic Wetness Index (TWI) also known as the Compound Topographic Index (CTI) and the Multi-resolution Valley Bottom Flatness index (MrVBF). Examples of the output for several catchments show th...

2004
Jon D. Pelletier

[1] Numerical landscape evolution models driven by uniform vertical uplift often develop a static drainage network and a precise balance between uplift and erosion. Small-scale physical models of uplifting drainage basins, however, continually reorganize by ridge migration and do not reach an ideal steady state. Here I show that the presence or absence of persistent drainage migration in a bedr...

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