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

The PlanetScope constellation consists of ∼150 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 m. Subsequent cubesats on each of the orbital planes image t...

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Main Authors: Kääb, Andreas, Altena, B., Mascaro, Joseph
Other Authors: Sub Dynamics Meteorology, Marine and Atmospheric Research
Format: Article in Journal/Newspaper
Language:English
Published: 2019
Subjects:
Online Access:https://dspace.library.uu.nl/handle/1874/408376
id ftunivutrecht:oai:dspace.library.uu.nl:1874/408376
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spelling ftunivutrecht:oai:dspace.library.uu.nl:1874/408376 2023-12-03T10:31:44+01:00 River-ice and water velocities using the Planet optical cubesat constellation Kääb, Andreas Altena, B. Mascaro, Joseph Sub Dynamics Meteorology Marine and Atmospheric Research 2019-10-22 application/pdf https://dspace.library.uu.nl/handle/1874/408376 en eng 1027-5606 https://dspace.library.uu.nl/handle/1874/408376 info:eu-repo/semantics/OpenAccess Article 2019 ftunivutrecht 2023-11-08T23:18:49Z The PlanetScope constellation consists of ∼150 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 m. Subsequent cubesats on each of the orbital planes image the Earth surface with a nominal time lag of approximately 90 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 km long reach of the Amur River in Siberia, and a 200 km long reach of the Yukon River in Alaska. The accuracy of the estimated horizontal surface velocities is of the order of ±0.01 m s−1. 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. Article in Journal/Newspaper Yukon river Alaska Siberia Yukon Utrecht University Repository Yukon
institution Open Polar
collection Utrecht University Repository
op_collection_id ftunivutrecht
language English
description The PlanetScope constellation consists of ∼150 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 m. Subsequent cubesats on each of the orbital planes image the Earth surface with a nominal time lag of approximately 90 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 km long reach of the Amur River in Siberia, and a 200 km long reach of the Yukon River in Alaska. The accuracy of the estimated horizontal surface velocities is of the order of ±0.01 m s−1. 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.
author2 Sub Dynamics Meteorology
Marine and Atmospheric Research
format Article in Journal/Newspaper
author Kääb, Andreas
Altena, B.
Mascaro, Joseph
spellingShingle Kääb, Andreas
Altena, B.
Mascaro, Joseph
River-ice and water velocities using the Planet optical cubesat constellation
author_facet Kääb, Andreas
Altena, B.
Mascaro, Joseph
author_sort Kääb, Andreas
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
publishDate 2019
url https://dspace.library.uu.nl/handle/1874/408376
geographic Yukon
geographic_facet Yukon
genre Yukon river
Alaska
Siberia
Yukon
genre_facet Yukon river
Alaska
Siberia
Yukon
op_relation 1027-5606
https://dspace.library.uu.nl/handle/1874/408376
op_rights info:eu-repo/semantics/OpenAccess
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