A SPATIO-TEMPORAL FRAMEWORK FOR MODELING ACTIVE LAYER THICKNESS

The Arctic is experiencing an unprecedented rate of environmental and climate change. The active layer (the uppermost layer of soil between the atmosphere and permafrost that freezes in winter and thaws in summer) is sensitive to both climatic and environmental changes, and plays an important role i...

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Published in:ISPRS Annals of the Photogrammetry, Remote Sensing and Spatial Information Sciences
Main Authors: Touyz, J., Streletskiy, D. A., Nelson, F. E., Apanasovich, T. V.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/isprsannals-II-4-W2-199-2015
https://www.isprs-ann-photogramm-remote-sens-spatial-inf-sci.net/II-4-W2/199/2015/
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spelling ftcopernicus:oai:publications.copernicus.org:isprsannals44086 2023-05-15T13:02:42+02:00 A SPATIO-TEMPORAL FRAMEWORK FOR MODELING ACTIVE LAYER THICKNESS Touyz, J. Streletskiy, D. A. Nelson, F. E. Apanasovich, T. V. 2018-01-15 application/pdf https://doi.org/10.5194/isprsannals-II-4-W2-199-2015 https://www.isprs-ann-photogramm-remote-sens-spatial-inf-sci.net/II-4-W2/199/2015/ eng eng doi:10.5194/isprsannals-II-4-W2-199-2015 https://www.isprs-ann-photogramm-remote-sens-spatial-inf-sci.net/II-4-W2/199/2015/ eISSN: 2194-9050 Text 2018 ftcopernicus https://doi.org/10.5194/isprsannals-II-4-W2-199-2015 2019-12-24T09:53:19Z The Arctic is experiencing an unprecedented rate of environmental and climate change. The active layer (the uppermost layer of soil between the atmosphere and permafrost that freezes in winter and thaws in summer) is sensitive to both climatic and environmental changes, and plays an important role in the functioning, planning, and economic activities of Arctic human and natural ecosystems. This study develops a methodology for modeling and estimating spatial-temporal variations in active layer thickness (ALT) using data from several sites of the Circumpolar Active Layer Monitoring network, and demonstrates its use in spatial-temporal interpolation. The simplest model’s stochastic component exhibits no spatial or spatio-temporal dependency and is referred to as the naïve model, against which we evaluate the performance of the other models, which assume that the stochastic component exhibits either spatial or spatio-temporal dependency. The methods used to fit the models are then discussed, along with point forecasting. We compare the predicted fit of the various models at key study sites located in the North Slope of Alaska and demonstrate the advantages of space-time models through a series of error statistics such as mean squared error, mean absolute and percent deviance from observed data. We find the difference in performance between the spatio-temporal and remaining models is significant for all three error statistics. The best stochastic spatio-temporal model increases predictive accuracy, compared to the naïve model, of 33.3%, 36.2% and 32.5% on average across the three error metrics at the key sites for a one-year hold out period. Text Active layer monitoring Active layer thickness Arctic Circumpolar Active Layer Monitoring Network Climate change north slope permafrost Alaska Copernicus Publications: E-Journals Arctic ISPRS Annals of the Photogrammetry, Remote Sensing and Spatial Information Sciences II-4/W2 199 206
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description The Arctic is experiencing an unprecedented rate of environmental and climate change. The active layer (the uppermost layer of soil between the atmosphere and permafrost that freezes in winter and thaws in summer) is sensitive to both climatic and environmental changes, and plays an important role in the functioning, planning, and economic activities of Arctic human and natural ecosystems. This study develops a methodology for modeling and estimating spatial-temporal variations in active layer thickness (ALT) using data from several sites of the Circumpolar Active Layer Monitoring network, and demonstrates its use in spatial-temporal interpolation. The simplest model’s stochastic component exhibits no spatial or spatio-temporal dependency and is referred to as the naïve model, against which we evaluate the performance of the other models, which assume that the stochastic component exhibits either spatial or spatio-temporal dependency. The methods used to fit the models are then discussed, along with point forecasting. We compare the predicted fit of the various models at key study sites located in the North Slope of Alaska and demonstrate the advantages of space-time models through a series of error statistics such as mean squared error, mean absolute and percent deviance from observed data. We find the difference in performance between the spatio-temporal and remaining models is significant for all three error statistics. The best stochastic spatio-temporal model increases predictive accuracy, compared to the naïve model, of 33.3%, 36.2% and 32.5% on average across the three error metrics at the key sites for a one-year hold out period.
format Text
author Touyz, J.
Streletskiy, D. A.
Nelson, F. E.
Apanasovich, T. V.
spellingShingle Touyz, J.
Streletskiy, D. A.
Nelson, F. E.
Apanasovich, T. V.
A SPATIO-TEMPORAL FRAMEWORK FOR MODELING ACTIVE LAYER THICKNESS
author_facet Touyz, J.
Streletskiy, D. A.
Nelson, F. E.
Apanasovich, T. V.
author_sort Touyz, J.
title A SPATIO-TEMPORAL FRAMEWORK FOR MODELING ACTIVE LAYER THICKNESS
title_short A SPATIO-TEMPORAL FRAMEWORK FOR MODELING ACTIVE LAYER THICKNESS
title_full A SPATIO-TEMPORAL FRAMEWORK FOR MODELING ACTIVE LAYER THICKNESS
title_fullStr A SPATIO-TEMPORAL FRAMEWORK FOR MODELING ACTIVE LAYER THICKNESS
title_full_unstemmed A SPATIO-TEMPORAL FRAMEWORK FOR MODELING ACTIVE LAYER THICKNESS
title_sort spatio-temporal framework for modeling active layer thickness
publishDate 2018
url https://doi.org/10.5194/isprsannals-II-4-W2-199-2015
https://www.isprs-ann-photogramm-remote-sens-spatial-inf-sci.net/II-4-W2/199/2015/
geographic Arctic
geographic_facet Arctic
genre Active layer monitoring
Active layer thickness
Arctic
Circumpolar Active Layer Monitoring Network
Climate change
north slope
permafrost
Alaska
genre_facet Active layer monitoring
Active layer thickness
Arctic
Circumpolar Active Layer Monitoring Network
Climate change
north slope
permafrost
Alaska
op_source eISSN: 2194-9050
op_relation doi:10.5194/isprsannals-II-4-W2-199-2015
https://www.isprs-ann-photogramm-remote-sens-spatial-inf-sci.net/II-4-W2/199/2015/
op_doi https://doi.org/10.5194/isprsannals-II-4-W2-199-2015
container_title ISPRS Annals of the Photogrammetry, Remote Sensing and Spatial Information Sciences
container_volume II-4/W2
container_start_page 199
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