Abstract

Abstract. Changes in Arctic sea ice affect atmospheric circulation, ocean current, and polar ecosystems. There have been unprecedented decreases in the amount of Arctic sea ice due to global warming. In this study, a novel 1-month sea ice concentration (SIC) prediction model is proposed, with eight predictors using a deep-learning approach, convolutional neural networks (CNNs). This monthly SIC prediction model based on CNNs is shown to perform better predictions (mean absolute error – MAE – of 2.28 %, anomaly correlation coefficient – ACC – of 0.98, root-mean-square error – RMSE – of 5.76 %, normalized RMSE – nRMSE – of 16.15 %, and NSE – Nash–Sutcliffe efficiency – of 0.97) than a random-forest-based (RF-based) model (MAE of 2.45 %, ACC of 0.98, RMSE of 6.61 %, nRMSE of 18.64 %, and NSE of 0.96) and the persistence model based on the monthly trend (MAE of 4.31 %, ACC of 0.95, RMSE of 10.54 %, nRMSE of 29.17 %, and NSE of 0.89) through hindcast validations. The spatio-temporal analysis also confirmed the superiority of the CNN model. The CNN model showed good SIC prediction results in extreme cases that recorded unforeseen sea ice plummets in 2007 and 2012 with RMSEs of less than 5.0 %. This study also examined the importance of the input variables through a sensitivity analysis. In both the CNN and RF models, the variables of past SICs were identified as the most sensitive factor in predicting SICs. For both models, the SIC-related variables generally contributed more to predict SICs over ice-covered areas, while other meteorological and oceanographic variables were more sensitive to the prediction of SICs in marginal ice zones. The proposed 1-month SIC prediction model provides valuable information which can be used in various applications, such as Arctic shipping-route planning, management of the fishing industry, and long-term sea ice forecasting and dynamics.

Highlights

  • Sea ice refers to the frozen seawater that covers approximately 15 % of the oceans in the world (National Snow and Ice Data Center, 2018)

  • This study firstly evaluated the model performance by quantitatively comparing the prediction results of the three models based on five accuracy metrics: the mean absolute error (MAE; Eq 1), anomaly correlation coefficient (ACC; Eq 2), root-mean-square error (RMSE; Eq 3), nRMSE (Eq 4), and Nash–Sutcliffe efficiency (NSE; Eq 5)

  • The convolutional neural networks (CNNs) model showed higher performance than the persistence model as well as RF models in all accuracy metrics. When it comes to considering the whole range of sea ice concentration (SIC) (0 %–100 %), the persistence model resulted in the lowest prediction performance (MAE of 4.31 %, ACC of 0.95, rootmean-square error (RMSE) of 10.54 %, nRMSE of 29.17 %, and NSE of 0.89)

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Summary

Introduction

Sea ice refers to the frozen seawater that covers approximately 15 % of the oceans in the world (National Snow and Ice Data Center, 2018). Sea ice reflects more solar radiation than the water’s surface, which makes the polar regions relatively cool. Sea ice shrinks in summer due to the warmer climate and expands in the winter season. Many studies on Arctic sea ice monitoring and dynamics have been conducted because it plays a significant role in the energy and water balance of global climate systems (Ledley, 1988; Guemas et al, 2016). The change in sea ice is an important indicator that shows the degree of ongoing climate change (Johannessen et al, 2004). Global warming causes a decrease in sea ice that worsens the arctic amplification, which in turn accelerates global warming itself (Cohen et al, 2014; Francis and Vavrus, 2015). Sea ice affects various oceanic characteristics and societal issues, such as ocean current circulation, by changing salinity and temperature gradation (Timmermann et al, 2009); polar ecosystems, by affecting key parts of the Arctic food web like sea ice algae (Doney et al, 2012); and economic industries, e.g., Arctic shipping routes (Melia et al, 2016)

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