Elevation and elevation-change maps of Fountain Creek, southeastern Colorado, 2015-20

Q4 Earth and Planetary Sciences U.S. Geological Survey Scientific Investigations Map Pub Date : 2021-01-01 DOI:10.3133/sim3481
L. Hempel, A. Creighton, A. Bock
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Abstract

The U.S. Geological Survey, in cooperation with Colorado Springs Utilities, has collected topographic data annually since 2012 at 10 study areas along Fountain Creek, southeastern Colorado. The 10 study areas were located between Colorado Springs and the terminus of Fountain Creek at the Arkansas River in Pueblo. The purpose of this report is to present elevation maps based on topographic surveys collected in 2020 and to present maps of elevation change that occurred between 2015 and 2020 at all 10 study areas. Elevation and elevation-change maps were developed in Global Mapper, R, and ArcGIS from topographic surveys collected at each study area during the winters of 2015 and 2020. Topographic surveys in 2015 were completed using real-time kinematic Global Navigation Satellite Systems. Topographic surveys in 2020 were completed using both real-time kinematic Global Navigation Satellite Systems and light detection and ranging. Elevation-change maps were created using propagated uncertainties associated with the 95-percent confidence limit. Study areas along Fountain Creek underwent a range of geomorphic responses between 2015 and 2020 that were often related to the dominant channel planform pattern of the study area. The results of this ongoing monitoring effort can be used to assess long-term changes in land-surface elevation and to advance understanding of the geomorphic response to possible changes in flow conditions on Fountain Creek.
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2015-20年科罗拉多州东南部喷泉溪的海拔和海拔变化图
自2012年以来,美国地质调查局与科罗拉多斯普林斯公用事业公司合作,每年在科罗拉多州东南部喷泉溪沿线的10个研究区域收集地形数据。这10个研究区域位于科罗拉多斯普林斯和普韦布洛阿肯色河喷泉溪的终点之间。本报告的目的是根据2020年收集的地形调查提供高程图,并提供2015年至2020年在所有10个研究区域发生的高程变化图。根据2015年和2020年冬季在每个研究区域收集的地形调查,在Global Mapper, R和ArcGIS中制作了高程和高程变化图。2015年的地形测量使用实时运动学全球导航卫星系统完成。2020年的地形调查使用实时运动学全球导航卫星系统和光探测和测距完成。海拔变化图是利用95%置信限的传播不确定性绘制的。2015年至2020年间,喷泉溪研究区经历了一系列地貌变化,这些变化往往与研究区主要的河道台地模式有关。这项持续监测工作的结果可用于评估地表高程的长期变化,并促进对喷泉溪上水流条件可能变化的地貌反应的理解。
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来源期刊
U.S. Geological Survey Scientific Investigations Map
U.S. Geological Survey Scientific Investigations Map Earth and Planetary Sciences-Geophysics
CiteScore
0.70
自引率
0.00%
发文量
6
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