Predicting regional and pan-Arctic sea ice anomalies with kernel analog forecasting

Predicting Arctic sea ice extent is a notoriously difficult forecasting problem, even for lead times as short as one month. Motivated by Arctic intraannual variability phenomena such as reemergence of sea surface temperature and sea ice anomalies, we use a prediction approach for sea ice anomalies b...

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Published in:Climate Dynamics
Main Authors: Comeau, Darin, Giannakis, Dimitrios, Zhao, Zhizhen, Majda, Andrew J.
Language:unknown
Published: 2023
Subjects:
Online Access:http://www.osti.gov/servlets/purl/1480002
https://www.osti.gov/biblio/1480002
https://doi.org/10.1007/s00382-018-4459-x
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spelling ftosti:oai:osti.gov:1480002 2023-07-30T04:00:30+02:00 Predicting regional and pan-Arctic sea ice anomalies with kernel analog forecasting Comeau, Darin Giannakis, Dimitrios Zhao, Zhizhen Majda, Andrew J. 2023-06-28 application/pdf http://www.osti.gov/servlets/purl/1480002 https://www.osti.gov/biblio/1480002 https://doi.org/10.1007/s00382-018-4459-x unknown http://www.osti.gov/servlets/purl/1480002 https://www.osti.gov/biblio/1480002 https://doi.org/10.1007/s00382-018-4459-x doi:10.1007/s00382-018-4459-x 54 ENVIRONMENTAL SCIENCES 2023 ftosti https://doi.org/10.1007/s00382-018-4459-x 2023-07-11T09:29:50Z Predicting Arctic sea ice extent is a notoriously difficult forecasting problem, even for lead times as short as one month. Motivated by Arctic intraannual variability phenomena such as reemergence of sea surface temperature and sea ice anomalies, we use a prediction approach for sea ice anomalies based on analog forecasting. Traditional analog forecasting relies on identifying a single analog in a historical record, usually by minimizing Euclidean distance, and forming a forecast from the analog’s historical trajectory. An ensemble of analogs is used to make forecasts, where the ensemble weights are determined by a dynamics-adapted similarity kernel, which takes into account the nonlinear geometry on the underlying data manifold. We apply this method for forecasting pan-Arctic and regional sea ice area and volume anomalies from multi-century climate model data, and in many cases find improvement over the benchmark damped persistence forecast. Examples of success include the 3–6 month lead time prediction of Arctic sea ice area, the winter sea ice area prediction of some marginal ice zone seas, and the 3–12 month lead time prediction of sea ice volume anomalies in many central Arctic basins. Finally, we discuss possible connections between KAF success and sea ice reemergence, and find KAF to be successful in regions and seasons exhibiting high interannual variability. Other/Unknown Material Arctic Sea ice SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy) Arctic Climate Dynamics 52 9-10 5507 5525
institution Open Polar
collection SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy)
op_collection_id ftosti
language unknown
topic 54 ENVIRONMENTAL SCIENCES
spellingShingle 54 ENVIRONMENTAL SCIENCES
Comeau, Darin
Giannakis, Dimitrios
Zhao, Zhizhen
Majda, Andrew J.
Predicting regional and pan-Arctic sea ice anomalies with kernel analog forecasting
topic_facet 54 ENVIRONMENTAL SCIENCES
description Predicting Arctic sea ice extent is a notoriously difficult forecasting problem, even for lead times as short as one month. Motivated by Arctic intraannual variability phenomena such as reemergence of sea surface temperature and sea ice anomalies, we use a prediction approach for sea ice anomalies based on analog forecasting. Traditional analog forecasting relies on identifying a single analog in a historical record, usually by minimizing Euclidean distance, and forming a forecast from the analog’s historical trajectory. An ensemble of analogs is used to make forecasts, where the ensemble weights are determined by a dynamics-adapted similarity kernel, which takes into account the nonlinear geometry on the underlying data manifold. We apply this method for forecasting pan-Arctic and regional sea ice area and volume anomalies from multi-century climate model data, and in many cases find improvement over the benchmark damped persistence forecast. Examples of success include the 3–6 month lead time prediction of Arctic sea ice area, the winter sea ice area prediction of some marginal ice zone seas, and the 3–12 month lead time prediction of sea ice volume anomalies in many central Arctic basins. Finally, we discuss possible connections between KAF success and sea ice reemergence, and find KAF to be successful in regions and seasons exhibiting high interannual variability.
author Comeau, Darin
Giannakis, Dimitrios
Zhao, Zhizhen
Majda, Andrew J.
author_facet Comeau, Darin
Giannakis, Dimitrios
Zhao, Zhizhen
Majda, Andrew J.
author_sort Comeau, Darin
title Predicting regional and pan-Arctic sea ice anomalies with kernel analog forecasting
title_short Predicting regional and pan-Arctic sea ice anomalies with kernel analog forecasting
title_full Predicting regional and pan-Arctic sea ice anomalies with kernel analog forecasting
title_fullStr Predicting regional and pan-Arctic sea ice anomalies with kernel analog forecasting
title_full_unstemmed Predicting regional and pan-Arctic sea ice anomalies with kernel analog forecasting
title_sort predicting regional and pan-arctic sea ice anomalies with kernel analog forecasting
publishDate 2023
url http://www.osti.gov/servlets/purl/1480002
https://www.osti.gov/biblio/1480002
https://doi.org/10.1007/s00382-018-4459-x
geographic Arctic
geographic_facet Arctic
genre Arctic
Sea ice
genre_facet Arctic
Sea ice
op_relation http://www.osti.gov/servlets/purl/1480002
https://www.osti.gov/biblio/1480002
https://doi.org/10.1007/s00382-018-4459-x
doi:10.1007/s00382-018-4459-x
op_doi https://doi.org/10.1007/s00382-018-4459-x
container_title Climate Dynamics
container_volume 52
container_issue 9-10
container_start_page 5507
op_container_end_page 5525
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