Quantifying Surface Water Dynamics at 30 Meter Spatial Resolution in the North American High Northern Latitudes 1991–2011

The availability of a dense time series of satellite observations at moderate (30 m) spatial resolution is enabling unprecedented opportunities for understanding ecosystems around the world. A time series of data from Landsat was used to generate a series of three maps at decadal time step to show h...

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Published in:Remote Sensing
Main Authors: Mark Carroll, Margaret Wooten, Charlene DiMiceli, Robert Sohlberg, Maureen Kelly
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2016
Subjects:
Online Access:https://doi.org/10.3390/rs8080622
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spelling ftmdpi:oai:mdpi.com:/2072-4292/8/8/622/ 2023-08-20T04:04:42+02:00 Quantifying Surface Water Dynamics at 30 Meter Spatial Resolution in the North American High Northern Latitudes 1991–2011 Mark Carroll Margaret Wooten Charlene DiMiceli Robert Sohlberg Maureen Kelly agris 2016-07-28 application/pdf https://doi.org/10.3390/rs8080622 EN eng Multidisciplinary Digital Publishing Institute https://dx.doi.org/10.3390/rs8080622 https://creativecommons.org/licenses/by/4.0/ Remote Sensing; Volume 8; Issue 8; Pages: 622 remote sensing inland water land cover Landsat ABoVE Text 2016 ftmdpi https://doi.org/10.3390/rs8080622 2023-07-31T20:55:37Z The availability of a dense time series of satellite observations at moderate (30 m) spatial resolution is enabling unprecedented opportunities for understanding ecosystems around the world. A time series of data from Landsat was used to generate a series of three maps at decadal time step to show how surface water has changed from 1991 to 2011 in the high northern latitudes of North America. Previous attempts to characterize the change in surface water in this region have been limited in either spatial or temporal resolution, or both. This series of maps was generated for the NASA Arctic and Boreal Vulnerability Experiment (ABoVE), which began in fall 2015. These maps show a “nominal” extent of surface water by using multiple observations to make a single map for each time step. This increases the confidence that any detected changes are related to climate or ecosystem changes not simply caused by short duration weather events such as flood or drought. The methods and comparison to other contemporary maps of the region are presented here. Initial verification results indicate 96% producer accuracy and 54% user accuracy when compared to 2-m resolution WorldView-2 data. All water bodies that were omitted were one Landsat pixel or smaller, hence below detection limits of the instrument. Text Arctic MDPI Open Access Publishing Arctic Remote Sensing 8 8 622
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic remote sensing
inland water
land cover
Landsat
ABoVE
spellingShingle remote sensing
inland water
land cover
Landsat
ABoVE
Mark Carroll
Margaret Wooten
Charlene DiMiceli
Robert Sohlberg
Maureen Kelly
Quantifying Surface Water Dynamics at 30 Meter Spatial Resolution in the North American High Northern Latitudes 1991–2011
topic_facet remote sensing
inland water
land cover
Landsat
ABoVE
description The availability of a dense time series of satellite observations at moderate (30 m) spatial resolution is enabling unprecedented opportunities for understanding ecosystems around the world. A time series of data from Landsat was used to generate a series of three maps at decadal time step to show how surface water has changed from 1991 to 2011 in the high northern latitudes of North America. Previous attempts to characterize the change in surface water in this region have been limited in either spatial or temporal resolution, or both. This series of maps was generated for the NASA Arctic and Boreal Vulnerability Experiment (ABoVE), which began in fall 2015. These maps show a “nominal” extent of surface water by using multiple observations to make a single map for each time step. This increases the confidence that any detected changes are related to climate or ecosystem changes not simply caused by short duration weather events such as flood or drought. The methods and comparison to other contemporary maps of the region are presented here. Initial verification results indicate 96% producer accuracy and 54% user accuracy when compared to 2-m resolution WorldView-2 data. All water bodies that were omitted were one Landsat pixel or smaller, hence below detection limits of the instrument.
format Text
author Mark Carroll
Margaret Wooten
Charlene DiMiceli
Robert Sohlberg
Maureen Kelly
author_facet Mark Carroll
Margaret Wooten
Charlene DiMiceli
Robert Sohlberg
Maureen Kelly
author_sort Mark Carroll
title Quantifying Surface Water Dynamics at 30 Meter Spatial Resolution in the North American High Northern Latitudes 1991–2011
title_short Quantifying Surface Water Dynamics at 30 Meter Spatial Resolution in the North American High Northern Latitudes 1991–2011
title_full Quantifying Surface Water Dynamics at 30 Meter Spatial Resolution in the North American High Northern Latitudes 1991–2011
title_fullStr Quantifying Surface Water Dynamics at 30 Meter Spatial Resolution in the North American High Northern Latitudes 1991–2011
title_full_unstemmed Quantifying Surface Water Dynamics at 30 Meter Spatial Resolution in the North American High Northern Latitudes 1991–2011
title_sort quantifying surface water dynamics at 30 meter spatial resolution in the north american high northern latitudes 1991–2011
publisher Multidisciplinary Digital Publishing Institute
publishDate 2016
url https://doi.org/10.3390/rs8080622
op_coverage agris
geographic Arctic
geographic_facet Arctic
genre Arctic
genre_facet Arctic
op_source Remote Sensing; Volume 8; Issue 8; Pages: 622
op_relation https://dx.doi.org/10.3390/rs8080622
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/rs8080622
container_title Remote Sensing
container_volume 8
container_issue 8
container_start_page 622
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