4.3 Article

Field-based research directions for investigating the interior of high-elevation debris-covered glaciers

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ANNALS OF GLACIOLOGY
卷 -, 期 -, 页码 -

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CAMBRIDGE UNIV PRESS
DOI: 10.1017/aog.2023.21

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Debris-covered glaciers; glacier hydrology; ice thickness measurements; ice temperature; ice velocity

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The debris on high-elevation debris-covered glaciers plays a significant role in shaping their features and processes. However, our understanding of the subsurface environments of these glaciers is still very limited. More field-based studies are needed to improve numerical models and enhance predictions.
The debris that covers the ablation areas of high-elevation debris-covered glaciers contributes to the distinctive features and processes occurring both on and within such glaciers. Despite recent advances, knowledge of the subsurface environments of high-elevation debris-covered glaciers is still extremely limited. In particular, targeted field-based data are needed to parameterise and refine the projections of these glaciers in numerical models. Here, we outline the current understanding of the internal properties of high-elevation debris-covered glaciers based on direct field-based methods and suggest future research directions for field-based studies.

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