4.7 Article

Tracking Dynamic Northern Surface Water Changes with High-Frequency Planet CubeSat Imagery

期刊

REMOTE SENSING
卷 9, 期 12, 页码 -

出版社

MDPI
DOI: 10.3390/rs9121306

关键词

Arctic hydrology; CubeSats; remote sensing of lakes and rivers; Yukon Flats

资金

  1. NASA Terrestrial Ecology Program Arctic-Boreal Vulnerability Experiment (ABoVE) grant [NNX17AC60A]
  2. National Science Foundation Graduate Research Fellowship
  3. Polar Geospatial Center under NSF OPP [1043681, 1559691]
  4. NASA [NNX17AC60A, 1003117] Funding Source: Federal RePORTER

向作者/读者索取更多资源

Recent deployments of CubeSat imagers by companies such as Planet may advance hydrological remote sensing by providing an unprecedented combination of high temporal and high spatial resolution imagery at the global scale. With approximately 170 CubeSats orbiting at full operational capacity, the Planet CubeSat constellation currently offers an average revisit time of <1 day for the Arctic and near-daily revisit time globally at 3 m spatial resolution. Such data have numerous potential applications for water resource monitoring, hydrologic modeling and hydrologic research. Here we evaluate Planet CubeSat imaging capabilities and potential scientific utility for surface water studies in the Yukon Flats, a large sub-Arctic wetland in north central Alaska. We find that surface water areas delineated from Planet imagery have a normalized root mean square error (NRMSE) of <11% and geolocation accuracy of <10 m as compared with manual delineations from high resolution (0.3-0.5 m) WorldView-2/3 panchromatic satellite imagery. For a 625 km(2) subarea of the Yukon Flats, our time series analysis reveals that roughly one quarter of 268 lakes analyzed responded to changes in Yukon River discharge over the period 23 June-1 October 2016, one half steadily contracted, and one quarter remained unchanged. The spatial pattern of observed lake changes is heterogeneous. While connections to Yukon River control the hydrologically connected lakes, the behavior of other lakes is complex, likely driven by a combination of intricate flow paths, underlying geology and permafrost. Limitations of Planet CubeSat imagery include a lack of an automated cloud mask, geolocation inaccuracies, and inconsistent radiometric calibration across multiple platforms. Although these challenges must be addressed before Planet CubeSat imagery can achieve its full potential for large-scale hydrologic research, we conclude that CubeSat imagery offers a powerful new tool for the study and monitoring of dynamic surface water bodies.

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