Over the past four decades, the increased heat gain in the southwestern Barents Sea through AW inflow was not compensated by surface heat loss, which had a negative trend (Fig. 1c ), resulting in a strong ocean warming trend (Fig. 3a ).
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Over the past four decades, the increased heat gain in the southwestern Barents Sea through AW inflow was not compensated by surface heat loss, which had a negative trend (Fig. 1c ), resulting in a strong ocean warming trend (Fig. 3a ).