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&#xD;
The files contained in this collection present the outputs from three experiments carried out in Rowan et al. (2021; Journal of Geophysical Research-Earth Surface):&#xD;
1. Simulation with a continuous debris layer, where h0 = 0.23 m and dT = 1.5 degC, showing the effect of change in mean annual air temperature to the present day (2015 CE) from 1.5 degC relative to the Little Ice Age&#xD;
2. Simulation with a discontinuous debris layer, where h0 = 0.94 m and dT = 1.5 degC&#xD;
3. Simulation with a discontinuous debris layer of the active glacier, where h0 = 0.94 m and dT = 1.5 degC&#xD;
&#xD;
The subglacial DEMs used for the model domains for the entire glacier and the active glacier, and the present-day (2015 CE) ice thickness estimated by Rowan et al. (2015, EPSL) to create the subglacial topography are also included (3 files).&#xD;
&#xD;
Funded by NERC under grant: NE/P00265X/1 &amp;quot;EverDrill: Accessing the interior and bed of a Himalayan debris-covered glacier to forecast future mass loss&amp;quot; to Duncan Quincey (PI) and Ann Rowan (CoI).</gco:CharacterString>
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&#xD;
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1. Simulation with a continuous debris layer, where h0 = 0.23 m and dT = 1.5 degC, showing the effect of change in mean annual air temperature to the present day (2015 CE) from 1.5 degC relative to the Little Ice Age&#xD;
2. Simulation with a discontinuous debris layer, where h0 = 0.94 m and dT = 1.5 degC&#xD;
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&#xD;
The subglacial DEMs used for the model domains for the entire glacier and the active glacier, and the present-day (2015 CE) ice thickness estimated by Rowan et al. (2015, EPSL) to create the subglacial topography are also included (3 files).&#xD;
&#xD;
These results differ from those presented in Version 1 (GB/NERC/BAS/PDC/01435) in that here the h0 values were revised based on a maximum debris thickness of 2.0 m (compared to 4.0 m in v1) and the simulations of the active glacier extent were not part of v1.
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