Pan-arctic river bank erosion and accretion, and planform metrics measured over intervals ranging from 1973 to 2016
This dataset provides the tabular summary of analysis of 14 reaches of 13 Arctic rivers for river bank erosion and accretion rates, as well as, river channel properties such as channel width, bank curvature, and the aspect/orientation of the river banks. These rivers include the: Colville River, Ala...
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ESS-DIVE: Deep Insight for Earth Science Data
2019
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Online Access: | https://search.dataone.org/view/ess-dive-79ea27d111c1adb-20210430T025619850563 |
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dataone:ess-dive-79ea27d111c1adb-20210430T025619850563 |
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record_format |
openpolar |
institution |
Open Polar |
collection |
ESS-DIVE: Deep Insight for Earth Science Data (via DataONE) |
op_collection_id |
dataone:urn:node:ESS_DIVE |
language |
unknown |
topic |
EARTH SCIENCE > LAND SURFACE > GEOMORPHIC LANDFORMS/PROCESSES EARTH SCIENCE > CRYOSPHERE > FROZEN GROUND EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > SURFACE WATER EARTH SCIENCE > LAND SURFACE > GEOMORPHIC LANDFORMS/PROCESSES > FLUVIAL LANDFORMS > RIVER EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > EROSION EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > SEDIMENT TRANSPORT EARTH SCIENCE > LAND SURFACE > FROZEN GROUND > PERMAFROST EARTH SCIENCE > LAND SURFACE > GEOMORPHIC LANDFORMS/PROCESSES > FLUVIAL LANDFORMS > CUTBANK EARTH SCIENCE > LAND SURFACE > GEOMORPHIC LANDFORMS/PROCESSES > FLUVIAL LANDFORMS > FLOOD PLAIN EARTH SCIENCE > LAND SURFACE > GEOMORPHIC LANDFORMS/PROCESSES > FLUVIAL LANDFORMS > MEANDER EARTH SCIENCE > LAND SURFACE > GEOMORPHIC LANDFORMS/PROCESSES > FLUVIAL LANDFORMS > POINT BAR EARTH SCIENCE > LAND SURFACE > GEOMORPHIC LANDFORMS/PROCESSES > FLUVIAL PROCESSES > SEDIMENT TRANSPORT EARTH SCIENCE > LAND SURFACE > GEOMORPHIC LANDFORMS/PROCESSES > FLUVIAL PROCESSES EARTH SCIENCE > LAND SURFACE > LANDSCAPE > LANDSCAPE PATTERNS EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > SURFACE WATER > SURFACE WATER FEATURES > RIVERS/STREAMS |
spellingShingle |
EARTH SCIENCE > LAND SURFACE > GEOMORPHIC LANDFORMS/PROCESSES EARTH SCIENCE > CRYOSPHERE > FROZEN GROUND EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > SURFACE WATER EARTH SCIENCE > LAND SURFACE > GEOMORPHIC LANDFORMS/PROCESSES > FLUVIAL LANDFORMS > RIVER EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > EROSION EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > SEDIMENT TRANSPORT EARTH SCIENCE > LAND SURFACE > FROZEN GROUND > PERMAFROST EARTH SCIENCE > LAND SURFACE > GEOMORPHIC LANDFORMS/PROCESSES > FLUVIAL LANDFORMS > CUTBANK EARTH SCIENCE > LAND SURFACE > GEOMORPHIC LANDFORMS/PROCESSES > FLUVIAL LANDFORMS > FLOOD PLAIN EARTH SCIENCE > LAND SURFACE > GEOMORPHIC LANDFORMS/PROCESSES > FLUVIAL LANDFORMS > MEANDER EARTH SCIENCE > LAND SURFACE > GEOMORPHIC LANDFORMS/PROCESSES > FLUVIAL LANDFORMS > POINT BAR EARTH SCIENCE > LAND SURFACE > GEOMORPHIC LANDFORMS/PROCESSES > FLUVIAL PROCESSES > SEDIMENT TRANSPORT EARTH SCIENCE > LAND SURFACE > GEOMORPHIC LANDFORMS/PROCESSES > FLUVIAL PROCESSES EARTH SCIENCE > LAND SURFACE > LANDSCAPE > LANDSCAPE PATTERNS EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > SURFACE WATER > SURFACE WATER FEATURES > RIVERS/STREAMS Joel Rowland Sophie Stauffer Pan-arctic river bank erosion and accretion, and planform metrics measured over intervals ranging from 1973 to 2016 |
topic_facet |
EARTH SCIENCE > LAND SURFACE > GEOMORPHIC LANDFORMS/PROCESSES EARTH SCIENCE > CRYOSPHERE > FROZEN GROUND EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > SURFACE WATER EARTH SCIENCE > LAND SURFACE > GEOMORPHIC LANDFORMS/PROCESSES > FLUVIAL LANDFORMS > RIVER EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > EROSION EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > SEDIMENT TRANSPORT EARTH SCIENCE > LAND SURFACE > FROZEN GROUND > PERMAFROST EARTH SCIENCE > LAND SURFACE > GEOMORPHIC LANDFORMS/PROCESSES > FLUVIAL LANDFORMS > CUTBANK EARTH SCIENCE > LAND SURFACE > GEOMORPHIC LANDFORMS/PROCESSES > FLUVIAL LANDFORMS > FLOOD PLAIN EARTH SCIENCE > LAND SURFACE > GEOMORPHIC LANDFORMS/PROCESSES > FLUVIAL LANDFORMS > MEANDER EARTH SCIENCE > LAND SURFACE > GEOMORPHIC LANDFORMS/PROCESSES > FLUVIAL LANDFORMS > POINT BAR EARTH SCIENCE > LAND SURFACE > GEOMORPHIC LANDFORMS/PROCESSES > FLUVIAL PROCESSES > SEDIMENT TRANSPORT EARTH SCIENCE > LAND SURFACE > GEOMORPHIC LANDFORMS/PROCESSES > FLUVIAL PROCESSES EARTH SCIENCE > LAND SURFACE > LANDSCAPE > LANDSCAPE PATTERNS EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > SURFACE WATER > SURFACE WATER FEATURES > RIVERS/STREAMS |
description |
This dataset provides the tabular summary of analysis of 14 reaches of 13 Arctic rivers for river bank erosion and accretion rates, as well as, river channel properties such as channel width, bank curvature, and the aspect/orientation of the river banks. These rivers include the: Colville River, Alaska; Indigirka River, Russia; Kolyma River, Russia; Koyukuk River, Alaska; Lena River, Alaska; Noatak River, Alaska; Ob River, Russia; Pechora River, Russia; Selawik River, Alaska; Taz River, Russia; Yana River, Russia; Yenisei River, Russia;, and the Yukon River, Alaska. The dataset was generated from a total of 114 images including: Landsat, higher resolution satellite imagery, and aerial photography over time periods ranging from the 1970s and 2016. A full list of the image dates, row and path (for Landsat), and pixel resolutions is provided in the dataset. The masks were analyzed using the Spatially Continuous Riverbank Erosion and Accretion Measurements (SCREAM) software detailed in Rowland et al. 2016. The masks used in this analysis can be found an accompanying dataset (DOI: doi:10.15485/1571525). In files with "summary" in the name, the data is provided at a pixel level, where each mapped bank pixel has an associated erosion or accretion value, a channel width, a curvature value, and an aspect each river and time period will have an individual file. Files with "Segments" in name provide data that is averaged along segments of the rivers. These data are consolidated into a single file each for the erosion and accretion measurements. These segments are approximately 10 channel widths in length. In addition to erosion and accretion rates, the segment-based results include area measurements of erosion and accretion, islands, and channels. The number of islands is also included. Rowland JC, et al. (2016) A morphology independent methodology for quantifying planview river change and characteristics from remotely sensed imagery. Remote Sens Environ 184. doi:10.1016/j.rse.2016.07.005. |
format |
Dataset |
author |
Joel Rowland Sophie Stauffer |
author_facet |
Joel Rowland Sophie Stauffer |
author_sort |
Joel Rowland |
title |
Pan-arctic river bank erosion and accretion, and planform metrics measured over intervals ranging from 1973 to 2016 |
title_short |
Pan-arctic river bank erosion and accretion, and planform metrics measured over intervals ranging from 1973 to 2016 |
title_full |
Pan-arctic river bank erosion and accretion, and planform metrics measured over intervals ranging from 1973 to 2016 |
title_fullStr |
Pan-arctic river bank erosion and accretion, and planform metrics measured over intervals ranging from 1973 to 2016 |
title_full_unstemmed |
Pan-arctic river bank erosion and accretion, and planform metrics measured over intervals ranging from 1973 to 2016 |
title_sort |
pan-arctic river bank erosion and accretion, and planform metrics measured over intervals ranging from 1973 to 2016 |
publisher |
ESS-DIVE: Deep Insight for Earth Science Data |
publishDate |
2019 |
url |
https://search.dataone.org/view/ess-dive-79ea27d111c1adb-20210430T025619850563 |
op_coverage |
Colville River, downstream of Umiat, Alaska USA Indigirka River, upstream of Chokurdakh, Russia Kolyma River, upstream of Srednekolymsk, Russia Lena River, downstream of Yakutsk, Russia Noatak River, near Noatak Village, Alaska USA Ob River, near Kolpashevo, Russia Pechora River, near Oksino, Russia Pechora River, downstream of Ust-Tsilma Selawik River, northwest Alaska Taz River, upstream of Sidorovsk, Russia Yana River, Russia Lower Yenisei River, Russia Yukon River, Yukon Flats, Alaska USA ENVELOPE(-155.1909,-150.95447,70.18678,68.941216) BEGINDATE: 1973-07-18T00:00:00Z ENDDATE: 2019-09-16T00:00:00Z |
long_lat |
ENVELOPE(161.000,161.000,69.500,69.500) ENVELOPE(84.738,84.738,69.718,69.718) ENVELOPE(149.609,149.609,70.929,70.929) ENVELOPE(161.700,161.700,-77.213,-77.213) ENVELOPE(134.625,134.625,67.662,67.662) ENVELOPE(153.702,153.702,67.457,67.457) ENVELOPE(82.283,82.283,66.607,66.607) ENVELOPE(-155.1909,-150.95447,70.18678,68.941216) |
geographic |
Arctic Yukon Yakutsk Kolyma Yenisei River Indigirka Rowland Yana River Srednekolymsk Sidorovsk |
geographic_facet |
Arctic Yukon Yakutsk Kolyma Yenisei River Indigirka Rowland Yana River Srednekolymsk Sidorovsk |
genre |
Arctic kolyma river lena river ob river Pechora permafrost Yakutsk Yukon river Alaska Yukon |
genre_facet |
Arctic kolyma river lena river ob river Pechora permafrost Yakutsk Yukon river Alaska Yukon |
_version_ |
1811922267065548800 |
spelling |
dataone:ess-dive-79ea27d111c1adb-20210430T025619850563 2024-10-03T18:45:55+00:00 Pan-arctic river bank erosion and accretion, and planform metrics measured over intervals ranging from 1973 to 2016 Joel Rowland Sophie Stauffer Colville River, downstream of Umiat, Alaska USA Indigirka River, upstream of Chokurdakh, Russia Kolyma River, upstream of Srednekolymsk, Russia Lena River, downstream of Yakutsk, Russia Noatak River, near Noatak Village, Alaska USA Ob River, near Kolpashevo, Russia Pechora River, near Oksino, Russia Pechora River, downstream of Ust-Tsilma Selawik River, northwest Alaska Taz River, upstream of Sidorovsk, Russia Yana River, Russia Lower Yenisei River, Russia Yukon River, Yukon Flats, Alaska USA ENVELOPE(-155.1909,-150.95447,70.18678,68.941216) BEGINDATE: 1973-07-18T00:00:00Z ENDDATE: 2019-09-16T00:00:00Z 2019-10-15T00:00:00Z https://search.dataone.org/view/ess-dive-79ea27d111c1adb-20210430T025619850563 unknown ESS-DIVE: Deep Insight for Earth Science Data EARTH SCIENCE > LAND SURFACE > GEOMORPHIC LANDFORMS/PROCESSES EARTH SCIENCE > CRYOSPHERE > FROZEN GROUND EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > SURFACE WATER EARTH SCIENCE > LAND SURFACE > GEOMORPHIC LANDFORMS/PROCESSES > FLUVIAL LANDFORMS > RIVER EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > EROSION EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > SEDIMENT TRANSPORT EARTH SCIENCE > LAND SURFACE > FROZEN GROUND > PERMAFROST EARTH SCIENCE > LAND SURFACE > GEOMORPHIC LANDFORMS/PROCESSES > FLUVIAL LANDFORMS > CUTBANK EARTH SCIENCE > LAND SURFACE > GEOMORPHIC LANDFORMS/PROCESSES > FLUVIAL LANDFORMS > FLOOD PLAIN EARTH SCIENCE > LAND SURFACE > GEOMORPHIC LANDFORMS/PROCESSES > FLUVIAL LANDFORMS > MEANDER EARTH SCIENCE > LAND SURFACE > GEOMORPHIC LANDFORMS/PROCESSES > FLUVIAL LANDFORMS > POINT BAR EARTH SCIENCE > LAND SURFACE > GEOMORPHIC LANDFORMS/PROCESSES > FLUVIAL PROCESSES > SEDIMENT TRANSPORT EARTH SCIENCE > LAND SURFACE > GEOMORPHIC LANDFORMS/PROCESSES > FLUVIAL PROCESSES EARTH SCIENCE > LAND SURFACE > LANDSCAPE > LANDSCAPE PATTERNS EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > SURFACE WATER > SURFACE WATER FEATURES > RIVERS/STREAMS Dataset 2019 dataone:urn:node:ESS_DIVE 2024-10-03T18:17:06Z This dataset provides the tabular summary of analysis of 14 reaches of 13 Arctic rivers for river bank erosion and accretion rates, as well as, river channel properties such as channel width, bank curvature, and the aspect/orientation of the river banks. These rivers include the: Colville River, Alaska; Indigirka River, Russia; Kolyma River, Russia; Koyukuk River, Alaska; Lena River, Alaska; Noatak River, Alaska; Ob River, Russia; Pechora River, Russia; Selawik River, Alaska; Taz River, Russia; Yana River, Russia; Yenisei River, Russia;, and the Yukon River, Alaska. The dataset was generated from a total of 114 images including: Landsat, higher resolution satellite imagery, and aerial photography over time periods ranging from the 1970s and 2016. A full list of the image dates, row and path (for Landsat), and pixel resolutions is provided in the dataset. The masks were analyzed using the Spatially Continuous Riverbank Erosion and Accretion Measurements (SCREAM) software detailed in Rowland et al. 2016. The masks used in this analysis can be found an accompanying dataset (DOI: doi:10.15485/1571525). In files with "summary" in the name, the data is provided at a pixel level, where each mapped bank pixel has an associated erosion or accretion value, a channel width, a curvature value, and an aspect each river and time period will have an individual file. Files with "Segments" in name provide data that is averaged along segments of the rivers. These data are consolidated into a single file each for the erosion and accretion measurements. These segments are approximately 10 channel widths in length. In addition to erosion and accretion rates, the segment-based results include area measurements of erosion and accretion, islands, and channels. The number of islands is also included. Rowland JC, et al. (2016) A morphology independent methodology for quantifying planview river change and characteristics from remotely sensed imagery. Remote Sens Environ 184. doi:10.1016/j.rse.2016.07.005. Dataset Arctic kolyma river lena river ob river Pechora permafrost Yakutsk Yukon river Alaska Yukon ESS-DIVE: Deep Insight for Earth Science Data (via DataONE) Arctic Yukon Yakutsk Kolyma ENVELOPE(161.000,161.000,69.500,69.500) Yenisei River ENVELOPE(84.738,84.738,69.718,69.718) Indigirka ENVELOPE(149.609,149.609,70.929,70.929) Rowland ENVELOPE(161.700,161.700,-77.213,-77.213) Yana River ENVELOPE(134.625,134.625,67.662,67.662) Srednekolymsk ENVELOPE(153.702,153.702,67.457,67.457) Sidorovsk ENVELOPE(82.283,82.283,66.607,66.607) ENVELOPE(-155.1909,-150.95447,70.18678,68.941216) |