北半球の湖氷減少の非線形過程を解明(Researchers Identify Nonlinear Process of Northern Hemisphere Lake Ice Loss)

2026-07-29 中国科学院(CAS)

中国科学院南京地理湖沼研究所(NIGLAS)などの国際研究チームは、北半球724湖(2000~2022年)の結氷・融氷記録と気温データを解析し、湖氷の減少が気温上昇に対して非線形に進行することを明らかにした。春の融氷時期は秋の結氷時期より気温変化への感度が高く、温暖化に伴い融解が急速に進む。また、冬季平均気温が約-13.7~-6.8℃の閾値を超えると、氷の減少速度が急激に増加し、氷況の気候感度は最大22倍に高まることが判明した。この閾値は湖の形状や水深よりも、冬季気温や地表アルベドといった広域気候条件に強く支配される。高排出シナリオでは、2100年頃までに北半球の湖の結氷期間は平均約40日短縮し、臨界閾値を超える湖の割合は現在の23%から70%へ増加すると予測された。研究は、湖氷の急激な減少が水質、水生生態系、冬季氷結に依存する地域社会へ深刻な影響を及ぼす可能性を示し、こうした非線形応答を気候モデルへ組み込む重要性を提唱している。

<関連情報>

北半球の湖沼における氷の消失は、気温が臨界閾値を超えると急速に加速する Rapid acceleration of ice-cover loss from Northern Hemisphere lakes above critical air temperature thresholds

Jian Zhou, Weijia Wang, Yaru Ma, +3 , and Peter R. Leavitt
Proceedings of the National Academy of Sciences  Published:July 27, 2026
DOI:https://doi.org/10.1073/pnas.2610752123

北半球の湖氷減少の非線形過程を解明(Researchers Identify Nonlinear Process of Northern Hemisphere Lake Ice Loss)

Abstract

Widespread declines in lake-ice cover are a hallmark of climate warming, yet the dynamic sensitivity of ice cover to thermal forcing remains poorly understood across broad climatic gradients. By analyzing an extensive dataset from 724 Northern Hemisphere lakes between 2000 and 2022, we quantify the responsiveness of lake-ice phenology to changes in air temperature and project their future trajectories. Our hemispheric analysis reveals a pronounced asymmetrical sensitivity where ice-decay processes are significantly more responsive to warming than ice-formation events. We identify critical thermal threshold of mean winter air temperature (AT) ranging from −13.7 to −6.8 °C, beyond which phenological sensitivity accelerates nonlinearly. Once these winter temperature breakpoints are surpassed, the sensitivity of ice loss increases by up to 22-fold, signaling a threshold-dependent collapse of the seasonal ice cycle. These threshold-dependent responses are primarily driven by broad-scale thermal and radiative regimes, particularly winter AT and surface albedo, rather than localized lake morphology. Future projections indicate that under high-emission scenarios, ice-cover duration will contract by approximately 40 d, and the proportion of lakes crossing critical thermal thresholds and entering a state of accelerated phenological sensitivity is expected to rise from 23 to 70% by the end of the century. These findings suggest that many temperate and southern boreal lakes are nearing a state of heightened vulnerability where marginal warming will trigger abrupt and potentially irreversible ecological shifts.

1702地球物理及び地球化学
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