高山アジア地域における雪降比率の重要性を特定(Critical Snowfall-to-Precipitation Ratios Identified in High Mountain Asia Amid Global Warming)

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2025-02-25 中国科学院

中国科学院の研究チームは、ヒマラヤ山脈などの高山アジア(HMA)地域における降雪比率(S/P比)の臨界値を特定し、地球温暖化の影響を分析しました。過去の気候データとCMIP6モデルを用いた結果、S/P比の0.13~0.87の範囲が特に温暖化に敏感で、降雪率が3~5倍速く低下することが判明。SSP5-8.5シナリオによる予測では、雪主導地域が2100年までに冬で25.8%、春で54.1%縮小すると見込まれます。これにより水資源や生態系への影響が懸念されます。

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温暖化がアジア高山帯の降雪分画減少の閾値を引き起こす Warming triggers snowfall fraction loss Thresholds in High-Mountain Asia

Yupeng Li,Yaning Chen,Fan Sun,Zhi Li,Gonghuan Fang,Weili Duan,Xueqi Zhang & Baofu Li
npj Climate and Atmospheric Science  Published:17 February 2025
DOI:https://doi.org/10.1038/s41612-025-00935-y

高山アジア地域における雪降比率の重要性を特定(Critical Snowfall-to-Precipitation Ratios Identified in High Mountain Asia Amid Global Warming)

Abstract

Global warming is accelerating climate disasters by triggering tipping points in various Earth systems. Although changes in precipitation patterns in High-Mountain Asia (HMA) have been extensively studied, the specific thresholds that trigger rapid snowfall loss remain unclear. A continuous piecewise linear regression model was employed to classify HMA into four distinct precipitation regimes: insensitive snowfall-dominated areas, sensitive snowfall-dominated areas, sensitive rainfall-dominated areas, and insensitive rainfall-dominated areas. Our results show that future warming will increase the sensitivity of winter and spring snowfall to climate change, whereas summer and autumn snowfall will become less sensitive. All four precipitation regimes exhibit an upward shift to higher elevations, with varying rates of elevation gain across regions and seasons. Temperature is the primary driver of snowfall loss, whereas relative humidity mitigates it. This study identifies high-risk areas vulnerable to snowfall loss, to help guide the development of effective mitigation strategies.

1900環境一般
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