Detecting Landscape Changes in High Latitude Environments Using Landsat Trend Analysis: 2. Classification

Mapping landscape dynamics is necessary to assess cumulative impacts due to climate change and development in Arctic regions. Landscape changes produce a range of temporal reflectance trajectories that can be obtained from remote sensing image time-series. Mapping these changes assumes that their tr...

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Published in:Remote Sensing
Main Authors: Ian Olthof, Robert Fraser
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2014
Subjects:
Online Access:https://doi.org/10.3390/rs61111558
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spelling ftmdpi:oai:mdpi.com:/2072-4292/6/11/11558/ 2023-08-20T04:04:17+02:00 Detecting Landscape Changes in High Latitude Environments Using Landsat Trend Analysis: 2. Classification Ian Olthof Robert Fraser agris 2014-11-20 application/pdf https://doi.org/10.3390/rs61111558 EN eng Multidisciplinary Digital Publishing Institute https://dx.doi.org/10.3390/rs61111558 https://creativecommons.org/licenses/by/4.0/ Remote Sensing; Volume 6; Issue 11; Pages: 11558-11578 Landsat arctic time-series change profile matching trend regression Text 2014 ftmdpi https://doi.org/10.3390/rs61111558 2023-07-31T20:40:21Z Mapping landscape dynamics is necessary to assess cumulative impacts due to climate change and development in Arctic regions. Landscape changes produce a range of temporal reflectance trajectories that can be obtained from remote sensing image time-series. Mapping these changes assumes that their trajectories are unique and can be characterized by magnitude and shape. A companion paper in this issue describes a trajectory visualization method for assessing a range of landscape disturbances. This paper focusses on generating a change map using a time-series of calibrated Landsat Tasseled Cap indices from 1985 to 2011. A reference change database covering the Mackenzie Delta region was created using a number of ancillary datasets to delineate polygons describing 21 natural and human-induced disturbances. Two approaches were tested to classify the Landsat time-series and generate change maps. The first involved profile matching based on trajectory shape and distance, while the second quantified profile shape with regression coefficients that were input to a decision tree classifier. Results indicate that classification of robust linear trend coefficients performed best. A final change map was assessed using bootstrapping and cross-validation, producing an overall accuracy of 82.8% at the level of 21 change classes and 87.3% when collapsed to eight underlying change processes. Text Arctic Climate change Mackenzie Delta MDPI Open Access Publishing Arctic Mackenzie Delta ENVELOPE(-136.672,-136.672,68.833,68.833) Remote Sensing 6 11 11558 11578
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic Landsat
arctic
time-series
change
profile matching
trend
regression
spellingShingle Landsat
arctic
time-series
change
profile matching
trend
regression
Ian Olthof
Robert Fraser
Detecting Landscape Changes in High Latitude Environments Using Landsat Trend Analysis: 2. Classification
topic_facet Landsat
arctic
time-series
change
profile matching
trend
regression
description Mapping landscape dynamics is necessary to assess cumulative impacts due to climate change and development in Arctic regions. Landscape changes produce a range of temporal reflectance trajectories that can be obtained from remote sensing image time-series. Mapping these changes assumes that their trajectories are unique and can be characterized by magnitude and shape. A companion paper in this issue describes a trajectory visualization method for assessing a range of landscape disturbances. This paper focusses on generating a change map using a time-series of calibrated Landsat Tasseled Cap indices from 1985 to 2011. A reference change database covering the Mackenzie Delta region was created using a number of ancillary datasets to delineate polygons describing 21 natural and human-induced disturbances. Two approaches were tested to classify the Landsat time-series and generate change maps. The first involved profile matching based on trajectory shape and distance, while the second quantified profile shape with regression coefficients that were input to a decision tree classifier. Results indicate that classification of robust linear trend coefficients performed best. A final change map was assessed using bootstrapping and cross-validation, producing an overall accuracy of 82.8% at the level of 21 change classes and 87.3% when collapsed to eight underlying change processes.
format Text
author Ian Olthof
Robert Fraser
author_facet Ian Olthof
Robert Fraser
author_sort Ian Olthof
title Detecting Landscape Changes in High Latitude Environments Using Landsat Trend Analysis: 2. Classification
title_short Detecting Landscape Changes in High Latitude Environments Using Landsat Trend Analysis: 2. Classification
title_full Detecting Landscape Changes in High Latitude Environments Using Landsat Trend Analysis: 2. Classification
title_fullStr Detecting Landscape Changes in High Latitude Environments Using Landsat Trend Analysis: 2. Classification
title_full_unstemmed Detecting Landscape Changes in High Latitude Environments Using Landsat Trend Analysis: 2. Classification
title_sort detecting landscape changes in high latitude environments using landsat trend analysis: 2. classification
publisher Multidisciplinary Digital Publishing Institute
publishDate 2014
url https://doi.org/10.3390/rs61111558
op_coverage agris
long_lat ENVELOPE(-136.672,-136.672,68.833,68.833)
geographic Arctic
Mackenzie Delta
geographic_facet Arctic
Mackenzie Delta
genre Arctic
Climate change
Mackenzie Delta
genre_facet Arctic
Climate change
Mackenzie Delta
op_source Remote Sensing; Volume 6; Issue 11; Pages: 11558-11578
op_relation https://dx.doi.org/10.3390/rs61111558
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/rs61111558
container_title Remote Sensing
container_volume 6
container_issue 11
container_start_page 11558
op_container_end_page 11578
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