Assessment of Arctic sea ice dynamics and their impacts on precipitation moisture sources using deep learning approaches

Stable isotopes of water ( 18 O and 2 H) are essential for analyzing the Arctic water cycle and climate variations. However, the link between sea ice extent changes as an important factor influencing Arctic climate and the isotopic composition of Arctic precipitation remains unclear. This study examined how sea ice extent in different Arctic marine regions affects precipitation isotopes at stations belonging to the Global Network of Isotopes in Precipitation (GNIP) across the Arctic. The main objective of this study was to evaluate the influence of sea ice extent variability on moisture sources and the isotopic composition of precipitation, with a particular focus on d -excess. Advanced deep learning techniques, including Long Short-Term Memory (LSTM), Deep Neural Network (DNN), and Recurrent Neural Network (RNN), were employed to analyze how variations in sea ice coverage impact the isotopic content in Arctic precipitation. To enhance prediction accuracy, Entropy Model Averaging (EMA) was used to ensemble the outputs of the models. Interpolated maps of the simulated isotope values were generated using Inverse Distance Weighting (IDW) to visualize spatial patterns. This study demonstrated the influence of sea ice changes on the isotopic composition of Arctic precipitation and simulated d -excess values. The reduction in sea ice increased Arctic moisture proportion (AMP) in precipitation, altering its isotopic composition. Analysis of d -excess revealed lower values in locally sourced precipitation and higher values in precipitation from subtropical sources. These findings highlight the key role of sea ice extent changes in influencing moisture sources and the isotopic composition of Arctic precipitation. • The interplay between d -excess in Arctic precipitation and sea ice extent changes was investigated. • Deep learning models (DNN, LSTM, RNN) simulated d -excess in Arctic precipitation. • Ensemble model (EMA) improved accuracy of d -excess simulations in the Arctic. • Copula theory assessed relationships between d -excess and sea ice extent. • The study revealed spatial variability of d -excess related to Arctic moisture sources.

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Publication Details

Journal
Environmental Technology & Innovation
Published
2025-02-21
DOI
https://doi.org/10.1016/j.eti.2025.104088
Citations
2
Primary Topic
Arctic and Antarctic ice dynamics
Type
article
Field-Weighted Citation Impact
2.60

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article

Assessment of Arctic sea ice dynamics and their impacts on precipitation moisture sources using deep learning approaches

Mojtaba Heydarizad, Melanie Parker, Rogert Sorí, Zhongfang Liu et al.
2 citations
Environmental Technology & Innovation
Arctic and Antarctic ice dynamics
2.60
article

Assessment of Arctic sea ice dynamics and their impacts on precipitation moisture sources using deep learning approaches

Mojtaba Heydarizad, Melanie Parker, Rogert Sorí, Zhongfang Liu, Thiago Mora, Edward Thakur
article en
2 citations

Abstract

Stable isotopes of water ( 18 O and 2 H) are essential for analyzing the Arctic water cycle and climate variations. However, the link between sea ice extent changes as an important factor influencing Arctic climate and the isotopic composition of Arctic precipitation remains unclear. This study examined how sea ice extent in different Arctic marine regions affects precipitation isotopes at stations belonging to the Global Network of Isotopes in Precipitation (GNIP) across the Arctic. The main objective of this study was to evaluate the influence of sea ice extent variability on moisture sources and the isotopic composition of precipitation, with a particular focus on d -excess. Advanced deep learning techniques, including Long Short-Term Memory (LSTM), Deep Neural Network (DNN), and Recurrent Neural Network (RNN), were employed to analyze how variations in sea ice coverage impact the isotopic content in Arctic precipitation. To enhance prediction accuracy, Entropy Model Averaging (EMA) was used to ensemble the outputs of the models. Interpolated maps of the simulated isotope values were generated using Inverse Distance Weighting (IDW) to visualize spatial patterns. This study demonstrated the influence of sea ice changes on the isotopic composition of Arctic precipitation and simulated d -excess values. The reduction in sea ice increased Arctic moisture proportion (AMP) in precipitation, altering its isotopic composition. Analysis of d -excess revealed lower values in locally sourced precipitation and higher values in precipitation from subtropical sources. These findings highlight the key role of sea ice extent changes in influencing moisture sources and the isotopic composition of Arctic precipitation. • The interplay between d -excess in Arctic precipitation and sea ice extent changes was investigated. • Deep learning models (DNN, LSTM, RNN) simulated d -excess in Arctic precipitation. • Ensemble model (EMA) improved accuracy of d -excess simulations in the Arctic. • Copula theory assessed relationships between d -excess and sea ice extent. • The study revealed spatial variability of d -excess related to Arctic moisture sources.

Environmental Technology & InnovationVol. 38
Wesleyan University (US), Tongji University (CN), Simon Fraser University (CA), Universidad de Costa Rica (CR), Universidad Libre de Costa Rica (CR), Universidade de Vigo (ES)
National Natural Science Foundation of China
Life below water
Openalex Percentile: Top 14%
Arctic and Antarctic ice dynamics
2.60
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