A review of the use of radio-echo sounding in glaciology
LA Plewes, B Hubbard - Progress in physical geography, 2001 - journals.sagepub.com
Radio-echo sounding (RES), or radar, is an established geophysical technique that has
been, and continues to be, applied to investigate a variety of ice-mass properties. This …
been, and continues to be, applied to investigate a variety of ice-mass properties. This …
Distributed ice thickness and volume of all glaciers around the globe
A new physically based approach for calculating glacier ice thickness distribution and
volume is presented and applied to all glaciers and ice caps worldwide. Combining glacier …
volume is presented and applied to all glaciers and ice caps worldwide. Combining glacier …
Greenland freshwater runoff. Part I: A runoff routing model for glaciated and nonglaciated landscapes (HydroFlow)
GE Liston, SH Mernild - Journal of Climate, 2012 - journals.ametsoc.org
A gridded linear-reservoir runoff routing model (HydroFlow) was developed to simulate the
linkages between runoff production from land-based snowmelt and icemelt processes and …
linkages between runoff production from land-based snowmelt and icemelt processes and …
Identification of snow ablation rate, ELA, AAR and net mass balance using transient snowline variations on two Arctic glaciers
Identification of the transient snowline (TSL) from high spatial resolution Landsat imagery on
Lemon Creek Glacier (LCG), southeast Alaska, USA, and Mittivakkat Gletscher (MG) …
Lemon Creek Glacier (LCG), southeast Alaska, USA, and Mittivakkat Gletscher (MG) …
Snow distribution and melt modeling for Mittivakkat Glacier, Ammassalik Island, southeast Greenland
SH Mernild, GE Liston, B Hasholt… - Journal of …, 2006 - journals.ametsoc.org
A physically based snow-evolution modeling system (SnowModel) that includes four
submodels—the Micrometeorological Model (MicroMet), EnBal, SnowPack, and SnowTran …
submodels—the Micrometeorological Model (MicroMet), EnBal, SnowPack, and SnowTran …
The future sea-level rise contribution of Greenland's glaciers and ice caps
We calculate the future sea-level rise contribution from the surface mass balance of all of
Greenland's glaciers and ice caps (GICs,∼ 90 000 km 2) using a simplified energy balance …
Greenland's glaciers and ice caps (GICs,∼ 90 000 km 2) using a simplified energy balance …
Three decades of volume change of a small Greenlandic glacier using ground penetrating radar, Structure from Motion, and aerial photogrammetry
Glaciers in the Arctic are losing mass at an increasing rate. Here we use surface topography
derived from Structure from Motion (SfM) and ice volume from ground penetrating radar …
derived from Structure from Motion (SfM) and ice volume from ground penetrating radar …
Increasing mass loss from Greenland's Mittivakkat Gletscher
Warming in the Arctic during the past several decades has caused glaciers to thin and
retreat, and recent mass loss from the Greenland Ice Sheet is well documented. Local …
retreat, and recent mass loss from the Greenland Ice Sheet is well documented. Local …
Ice geometry and thermal regime of Lyngmarksbræen Ice Cap, West Greenland
Observations remain sparse for peripheral glaciers and ice caps in Greenland. Here, we
present the results of a multi-frequency radar survey of Lyngmarksbræen Ice Cap in West …
present the results of a multi-frequency radar survey of Lyngmarksbræen Ice Cap in West …
Geochemistry of groundwater in front of a warm‐based glacier in Southeast Greenland
Groundwater in front of warm‐based glaciers is likely to become a more integrated part of
the future proglacial hydrological system at high latitudes due to global warming. Here, we …
the future proglacial hydrological system at high latitudes due to global warming. Here, we …