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Grid-based mapping: A method for rapidly determining the spatial distributions of small features over very large areas

机译:基于网格的映射:一种用于快速确定非常大的区域上的小要素的空间分布的方法

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摘要

The increased volume, spatial resolution, and areal coverage of high-resolution images of Mars over the past 15 years have led to an increased quantity and variety of small-scale landform identifications. Though many such landforms are too small to represent individually on regional-scale maps, determining their presence or absence across large areas helps form the observational basis for developing hypotheses on the geological nature and environmental history of a study area. The combination of improved spatial resolution and near-continuous coverage significantly increases the time required to analyse the data. This becomes problematic when attempting regional or global-scale studies of metre and decametre-scale landforms. Here, we describe an approach for mapping small features (from decimetre to kilometre scale) across large areas, formulated for a project to study the northern plains of Mars, and provide context on how this method was developed and how it can be implemented.\ud\udRather than “mapping” with points and polygons, grid-based mapping uses a “tick box” approach to efficiently record the locations of specific landforms (we use an example suite of glacial landforms; including viscous flow features, the latitude dependant mantle and polygonised ground). A grid of squares (e.g. 20 km by 20 km) is created over the mapping area. Then the basemap data are systematically examined, grid-square by grid-square at full resolution, in order to identify the landforms while recording the presence or absence of selected landforms in each grid-square to determine spatial distributions. The result is a series of grids recording the distribution of all the mapped landforms across the study area. In some ways, these are equivalent to raster images, as they show a continuous distribution-field of the various landforms across a defined (rectangular, in most cases) area. When overlain on context maps, these form a coarse, digital landform map.\ud\udWe find that grid-based mapping provides an efficient solution to the problems of mapping small landforms over large areas, by providing a consistent and standardised approach to spatial data collection. The simplicity of the grid-based mapping approach makes it extremely scalable and workable for group efforts, requiring minimal user experience and producing consistent and repeatable results. The discrete nature of the datasets, simplicity of approach, and divisibility of tasks, open up the possibility for citizen science in which crowdsourcing large grid-based mapping areas could be applied.
机译:在过去的15年中,火星高分辨率图像的体积,空间分辨率和区域覆盖率的提高,导致小型地形识别的数量和种类增加。尽管许多这样的地貌太小,无法在区域尺度的地图上单独显示,但是确定它们在大面积区域中的存在或不存在有助于形成研究区域的地质性质和环境历史假设的观察基础。改进的空间分辨率和近乎连续的覆盖范围相结合,大大增加了分析数据所需的时间。当尝试对米和十米尺度的地貌进行区域或全球规模的研究时,这成为问题。在这里,我们描述了一种在大面积上绘制小特征(从分米到千米)的方法,该方法是为研究火星北部平原的项目而设计的,并提供了有关此方法的开发方式和实施方法的背景信息。\ ud \ ud而非基于点和多边形的“映射”,基于网格的映射使用“刻度线”方法来有效记录特定地形的位置(我们使用了一组冰川地形的示例;包括粘性流特征,纬度相关的地幔和多边形地面)。在地图区域上创建了一个正方形网格(例如20 km x 20 km)。然后,以全分辨率逐格逐格地对底图数据进行系统地检查,以便识别地形,同时记录每个网格方格中是否存在所选地形以确定空间分布。结果是一系列网格记录了研究区域中所有映射地形的分布。在某些方面,它们等效于栅格图像,因为它们显示了在定义的(在大多数情况下为矩形)区域内各种地形的连续分布场。当覆盖在上下文地图上时,这些地图会形成一个粗糙的数字地形图。\ ud \ ud我们发现,基于网格的映射通过提供一致且标准化的空间数据方法,为解决在大面积区域上绘制小地形的问题提供了有效的解决方案。采集。基于网格的映射方法的简单性使其可极大地扩展和适用于小组工作,需要最少的用户体验并产生一致且可重复的结果。数据集的离散性质,方法的简单性和任务的可分性为公民科学开辟了可能应用众包的大型基于网格的地图区域的可能性。

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