Abstract

AbstractWhile hot-water drilling is a well-established technique used to access the subsurface of ice masses, drilling into high-elevation (≳ 4000 m a.s.l.) debris-covered glaciers faces specific challenges. First, restricted transport capacity limits individual equipment items to a volume and mass that can be slung by small helicopters. Second, low atmospheric oxygen and pressure reduces the effectiveness of combustion, limiting a system's ability to pump and heat water. Third, thick supraglacial debris, which is both highly uneven and unstable, inhibits direct access to the ice surface, hinders the manoeuvring of equipment and limits secure sites for equipment placement. Fourth, englacial debris can slow the drilling rate such that continued drilling becomes impracticable and/or boreholes deviate substantially from vertical. Because of these challenges, field-based englacial and subglacial data required to calibrate numerical models of high-elevation debris-covered glaciers are scarce or absent. Here, we summarise our experiences of hot-water drilling over two field seasons (2017–2018) at the debris-covered Khumbu Glacier, Nepal, where we melted 27 boreholes up to 192 m length, at elevations between 4900 and 5200 m a.s.l. We describe the drilling equipment and operation, evaluate the effectiveness of our approach and suggest equipment and methodological adaptations for future use.

Highlights

  • Hot-water drilling has long been used to study glaciers, ice sheets and ice shelves, providing a means to determine ice structure, debris content and hydrological features, as well as ice thickness if the bed is reached

  • We present our apparatus, method and experiences of hot-water drilling on the high-elevation debris-covered Khumbu Glacier, Nepal Himalaya, in 2017 and 2018

  • We suggest adaptations to the equipment and method to facilitate future hot-water drilling at high-elevation debris-covered glaciers, both at similar and higher elevations to those at which we drilled on Khumbu Glacier

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Summary

Introduction

Hot-water drilling has long been used to study glaciers, ice sheets and ice shelves, providing a means to determine ice structure, debris content and hydrological features, as well as ice thickness if the bed is reached. Such boreholes allow direct access to the ice-bed interface, from which sediment and water can be sampled. Viable drilling sites may be further restricted by hazards such as rockfall or avalanches from nearby mountain slopes Given these challenges, it is not surprising that hot-water drilling has rarely, if ever, been attempted at high-elevation debriscovered glaciers, resulting in a paucity of field-based data relating to the englacial and subglacial conditions at such glaciers. We suggest adaptations to the equipment and method to facilitate future hot-water drilling at high-elevation debris-covered glaciers, both at similar and higher elevations to those at which we drilled on Khumbu Glacier

Combustion engine power loss at high elevation
Equipment
Methods
System performance
Drilling
21–22 May 2017 10:54–15:31
Changes in surface topography
Methodological adaptations for future hot-water drilling
Conclusions
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