Prediction of subglacial lake melt source regions from site characteristics

Subglacial melt has important implications for ice-sheet dynamics. Locating and identifying subglacial lakes are expensive and time-consuming, requiring radar surveys or satellite methods. We explore three methods to identify source regions for lakes using seven continent-wide environmental characte...

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Published in:Antarctic Science
Main Authors: Willcocks, S., Hasterok, D.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2023
Subjects:
Online Access:https://hdl.handle.net/2440/138522
https://doi.org/10.1017/s0954102023000032
id ftunivadelaidedl:oai:digital.library.adelaide.edu.au:2440/138522
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spelling ftunivadelaidedl:oai:digital.library.adelaide.edu.au:2440/138522 2023-12-17T10:22:31+01:00 Prediction of subglacial lake melt source regions from site characteristics Willcocks, S. Hasterok, D. 2023 https://hdl.handle.net/2440/138522 https://doi.org/10.1017/s0954102023000032 en eng Cambridge University Press (CUP) http://purl.org/au-research/grants/arc/DP180104074 Antarctic Science, 2023; 35(2):127-140 0954-1020 1365-2079 https://hdl.handle.net/2440/138522 doi:10.1017/s0954102023000032 Hasterok, D. [0000-0002-8257-7975] © The Author(s), 2023. Published by Cambridge University Press on behalf of Antarctic Science Ltd http://dx.doi.org/10.1017/s0954102023000032 active lakes machine learning principal component analysis subglacial lakes Journal article 2023 ftunivadelaidedl https://doi.org/10.1017/s0954102023000032 2023-11-20T23:15:49Z Subglacial melt has important implications for ice-sheet dynamics. Locating and identifying subglacial lakes are expensive and time-consuming, requiring radar surveys or satellite methods. We explore three methods to identify source regions for lakes using seven continent-wide environmental characteristics that are sensitive to or influenced by ice-sheet temperature. A simple comparison of environmental properties at lake locations with their continent-wide distributions suggests a statistical relationship (high Kolmogorov-Smirnov statistic) between stable lake locations and ice thickness and surface temperatures, indicating melting under passive conditions. Active lakes, in contrast, show little correlation with direct thermally influenced parameters, instead exhibiting large statistical differences with horizontal velocity and bedrock elevation. More sophisticated techniques, including principal component analysis (PCA) and machine learning (ML) classification, provide better spatial identification of lake types. Positive PCA scores derived from the environmental characteristics correlate with stable lakes, whereas negative values correspond to active lakes. ML methods can also identify regions where subglacial lake melt sources are probable. While ML provides the most accurate classification maps, the combination of approaches adds deeper knowledge of the primary controls on lake formation and the environmental settings in which they are likely to be found. Simon Willcocks and Derrick Hasterok Article in Journal/Newspaper Antarctic Science Ice Sheet The University of Adelaide: Digital Library Antarctic Science 35 2 127 140
institution Open Polar
collection The University of Adelaide: Digital Library
op_collection_id ftunivadelaidedl
language English
topic active lakes
machine learning
principal component analysis
subglacial lakes
spellingShingle active lakes
machine learning
principal component analysis
subglacial lakes
Willcocks, S.
Hasterok, D.
Prediction of subglacial lake melt source regions from site characteristics
topic_facet active lakes
machine learning
principal component analysis
subglacial lakes
description Subglacial melt has important implications for ice-sheet dynamics. Locating and identifying subglacial lakes are expensive and time-consuming, requiring radar surveys or satellite methods. We explore three methods to identify source regions for lakes using seven continent-wide environmental characteristics that are sensitive to or influenced by ice-sheet temperature. A simple comparison of environmental properties at lake locations with their continent-wide distributions suggests a statistical relationship (high Kolmogorov-Smirnov statistic) between stable lake locations and ice thickness and surface temperatures, indicating melting under passive conditions. Active lakes, in contrast, show little correlation with direct thermally influenced parameters, instead exhibiting large statistical differences with horizontal velocity and bedrock elevation. More sophisticated techniques, including principal component analysis (PCA) and machine learning (ML) classification, provide better spatial identification of lake types. Positive PCA scores derived from the environmental characteristics correlate with stable lakes, whereas negative values correspond to active lakes. ML methods can also identify regions where subglacial lake melt sources are probable. While ML provides the most accurate classification maps, the combination of approaches adds deeper knowledge of the primary controls on lake formation and the environmental settings in which they are likely to be found. Simon Willcocks and Derrick Hasterok
format Article in Journal/Newspaper
author Willcocks, S.
Hasterok, D.
author_facet Willcocks, S.
Hasterok, D.
author_sort Willcocks, S.
title Prediction of subglacial lake melt source regions from site characteristics
title_short Prediction of subglacial lake melt source regions from site characteristics
title_full Prediction of subglacial lake melt source regions from site characteristics
title_fullStr Prediction of subglacial lake melt source regions from site characteristics
title_full_unstemmed Prediction of subglacial lake melt source regions from site characteristics
title_sort prediction of subglacial lake melt source regions from site characteristics
publisher Cambridge University Press (CUP)
publishDate 2023
url https://hdl.handle.net/2440/138522
https://doi.org/10.1017/s0954102023000032
genre Antarctic Science
Ice Sheet
genre_facet Antarctic Science
Ice Sheet
op_source http://dx.doi.org/10.1017/s0954102023000032
op_relation http://purl.org/au-research/grants/arc/DP180104074
Antarctic Science, 2023; 35(2):127-140
0954-1020
1365-2079
https://hdl.handle.net/2440/138522
doi:10.1017/s0954102023000032
Hasterok, D. [0000-0002-8257-7975]
op_rights © The Author(s), 2023. Published by Cambridge University Press on behalf of Antarctic Science Ltd
op_doi https://doi.org/10.1017/s0954102023000032
container_title Antarctic Science
container_volume 35
container_issue 2
container_start_page 127
op_container_end_page 140
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