南極の氷河湖形成を予測する数学モデルを開発(Future of Antarctic Ice: New Study Reveals the Mathematics of Meltwater Lakes)

2025-10-01 ジョージア工科大学

ジョージア工科大学の研究チームは、南極の氷床上に形成される融解湖の深さと広がりを予測する新たな数理モデルを開発した。氷床の地形的特徴(自己アフィン性)と衛星データを組み合わせ、湖の最大規模を簡易方程式で表現。これにより、気候モデルが氷床の安定性をより現実的に扱えるようになる。研究成果は『Nature Communications』に掲載され、NASAの気候モデリング計画にも統合が進められている。

南極の氷河湖形成を予測する数学モデルを開発(Future of Antarctic Ice: New Study Reveals the Mathematics of Meltwater Lakes)
A view of Greenland’s ice sheet from the NASA/USGS Landsat 8 satellite showing meltwater lakes on a glacier. (Credit: NASA)

<関連情報>

物理学に基づくパラメータ化による南極氷河融解湖の平均深度と面積率の予測 Predicting mean depth and area fraction of Antarctic supraglacial melt lakes with physics-based parameterizations

Danielle Grau,Azeez Hussain &Alexander A. Robel
Nature Communications  Published:15 July 2025
DOI:https://doi.org/10.1038/s41467-025-61798-8

Abstract

Despite the importance of supraglacial melt lakes to the future evolution of polar ice sheets, they are not represented in current large-scale climate and ice sheet models. In this study, we use ICESat-2 satellite surface elevation measurements to show that roughness on the Antarctic Ice Sheet surface is largely self-affine. Estimation of ice sheet surface roughness statistics then enables the development of a set of simple mathematical expressions parameterizing the average supraglacial melt lake area fraction and lake depth from statistical fitting of large simulation ensembles of water flow on random, self-affine surfaces. These parameterizations provide predictions that are generally consistent with observations, with some exceptions. Finally, we predict that on large portions of Antarctic ice shelves supraglacial lakes are likely to, on average, stay less than one meter deep and occupy less than 40% of the ice area, absent changes in ice shelf surface roughness.

1702地球物理及び地球化学
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