数字高程模型综述与关键分析

IF 0.9 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS
Geofizika Pub Date : 2019-01-14 DOI:10.15233/GFZ.2018.35.7
S. Lakshmi, K. Yarrakula
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引用次数: 28

摘要

目前,数字高程模型(DEM)已成为遥感和GIS领域不可缺少的组成部分。DEM反映了地球的物理表面,通过使用现代技术和高分辨率卫星图像来解释景观,有助于了解地形的性质。为了了解和分析地形的性质,许多领域都需要DEM来改进产品开发和决策,测绘目的,准备3D模拟,估计河道和创建等高线图以提取高程等。各种应用中的DEM将有助于复制全球范围内一致的高质量数字高程模型可用性的总体重要性。本文代表了dem的总体回顾,它的产生,发展使用各种技术从地形图和高分辨率卫星图像派生的十年来。通过应用创新的想法、即将到来的高分辨率卫星图像和技术,了解地形的本质、解决实际问题并解决问题是有用的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Review and critical analysis on digital elevation models
Nowadays, digital elevation model (DEM) acts as an inevitable component in the field of remote sensing and GIS. DEM reflects the physical surface of the earth helps to understand the nature of terrain by means of interpreting the landscape using modern techniques and high-resolution satellite images. To understand and analyze the nature of the terrain, DEM is required in many fields in the improvement of developing the product and decision making, mapping purpose, preparing 3D simulations, estimating river channel and creating contour maps to extract the elevation and so on. DEM in various applications will be useful to replicate the overall importance of the availability of worldwide, consistent, high-quality digital elevation models. The present article represents the overall review of DEMs, its generation, development using various techniques derived from topographic maps and high-resolution satellite images over a decade to present. It is useful to understand the nature of topography, address the practical problems and fix them by applying innovative ideas, upcoming high-resolution satellite images and techniques.
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来源期刊
Geofizika
Geofizika 地学-地球化学与地球物理
CiteScore
1.60
自引率
0.00%
发文量
17
审稿时长
>12 weeks
期刊介绍: The Geofizika journal succeeds the Papers series (Radovi), which has been published since 1923 at the Geophysical Institute in Zagreb (current the Department of Geophysics, Faculty of Science, University of Zagreb). Geofizika publishes contributions dealing with physics of the atmosphere, the sea and the Earth''s interior.
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