River-ice and water velocities using the Planet optical cubesat constellation

<p>The PlanetScope constellation consists of <span class="inline-formula">∼150</span> optical cubesats that are evenly distributed like strings of pearls on two orbital planes, scanning the Earth's land surface once per day with an approximate spatial image resolutio...

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Main Authors: A. Kääb, B. Altena, J. Mascaro
Format: Article
Language:English
Published: Copernicus Publications 2019-10-01
Series:Hydrology and Earth System Sciences
Online Access:https://www.hydrol-earth-syst-sci.net/23/4233/2019/hess-23-4233-2019.pdf
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spelling doaj-1289e585815141a0b34e3b8af2db29212020-11-25T01:16:36ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382019-10-01234233424710.5194/hess-23-4233-2019River-ice and water velocities using the Planet optical cubesat constellationA. Kääb0B. Altena1J. Mascaro2Department of Geosciences, University of Oslo, Oslo, 0316, NorwayDepartment of Geosciences, University of Oslo, Oslo, 0316, NorwayPlanet, San Francisco, 94103, USA<p>The PlanetScope constellation consists of <span class="inline-formula">∼150</span> optical cubesats that are evenly distributed like strings of pearls on two orbital planes, scanning the Earth's land surface once per day with an approximate spatial image resolution of 3&thinsp;m. Subsequent cubesats on each of the orbital planes image the Earth surface with a nominal time lag of approximately 90&thinsp;s between them, which produces near-simultaneous image pairs over the across-track overlaps of the cubesat swaths. We exploit this short time lag between subsequent Planet cubesat images to track river ice floes on northern rivers as indicators of water surface velocities. The method is demonstrated for a 60&thinsp;km long reach of the Amur River in Siberia, and a 200&thinsp;km long reach of the Yukon River in Alaska. The accuracy of the estimated horizontal surface velocities is of the order of <span class="inline-formula">±0.01</span>&thinsp;m&thinsp;s<span class="inline-formula"><sup>−1</sup></span>. The application of our approach is complicated by cloud cover and low sun angles at high latitudes during the periods where rivers typically carry ice floes, and by the fact that the near-simultaneous swath overlaps, by design, do not cover the complete Earth surface. Still, the approach enables direct remote sensing of river surface velocities for numerous cold-region rivers at a number of locations and occasionally several times per year – which is much more frequent and over much larger areas than currently feasible. We find that freeze-up conditions seem to offer ice floes that are generally more suitable for tracking, and over longer time periods, compared with typical ice break-up conditions. The coverage of river velocities obtained could be particularly useful in combination with satellite measurements of river area, and river surface height and slope.</p>https://www.hydrol-earth-syst-sci.net/23/4233/2019/hess-23-4233-2019.pdf
collection DOAJ
language English
format Article
sources DOAJ
author A. Kääb
B. Altena
J. Mascaro
spellingShingle A. Kääb
B. Altena
J. Mascaro
River-ice and water velocities using the Planet optical cubesat constellation
Hydrology and Earth System Sciences
author_facet A. Kääb
B. Altena
J. Mascaro
author_sort A. Kääb
title River-ice and water velocities using the Planet optical cubesat constellation
title_short River-ice and water velocities using the Planet optical cubesat constellation
title_full River-ice and water velocities using the Planet optical cubesat constellation
title_fullStr River-ice and water velocities using the Planet optical cubesat constellation
title_full_unstemmed River-ice and water velocities using the Planet optical cubesat constellation
title_sort river-ice and water velocities using the planet optical cubesat constellation
publisher Copernicus Publications
series Hydrology and Earth System Sciences
issn 1027-5606
1607-7938
publishDate 2019-10-01
description <p>The PlanetScope constellation consists of <span class="inline-formula">∼150</span> optical cubesats that are evenly distributed like strings of pearls on two orbital planes, scanning the Earth's land surface once per day with an approximate spatial image resolution of 3&thinsp;m. Subsequent cubesats on each of the orbital planes image the Earth surface with a nominal time lag of approximately 90&thinsp;s between them, which produces near-simultaneous image pairs over the across-track overlaps of the cubesat swaths. We exploit this short time lag between subsequent Planet cubesat images to track river ice floes on northern rivers as indicators of water surface velocities. The method is demonstrated for a 60&thinsp;km long reach of the Amur River in Siberia, and a 200&thinsp;km long reach of the Yukon River in Alaska. The accuracy of the estimated horizontal surface velocities is of the order of <span class="inline-formula">±0.01</span>&thinsp;m&thinsp;s<span class="inline-formula"><sup>−1</sup></span>. The application of our approach is complicated by cloud cover and low sun angles at high latitudes during the periods where rivers typically carry ice floes, and by the fact that the near-simultaneous swath overlaps, by design, do not cover the complete Earth surface. Still, the approach enables direct remote sensing of river surface velocities for numerous cold-region rivers at a number of locations and occasionally several times per year – which is much more frequent and over much larger areas than currently feasible. We find that freeze-up conditions seem to offer ice floes that are generally more suitable for tracking, and over longer time periods, compared with typical ice break-up conditions. The coverage of river velocities obtained could be particularly useful in combination with satellite measurements of river area, and river surface height and slope.</p>
url https://www.hydrol-earth-syst-sci.net/23/4233/2019/hess-23-4233-2019.pdf
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