@article {Goelzer2018,
	title = {{Design and results of the ice sheet model initialisation experiments initMIP-Greenland: an ISMIP6 intercomparison}},
	journal = {The Cryosphere},
	volume = {12},
	number = {4},
	year = {2018},
	month = {apr},
	pages = {1433{\textendash}1460},
	abstract = {Abstract. Earlier large-scale Greenland ice sheet sea-level projections (e.g. those run during the ice2sea and SeaRISE initiatives) have shown that ice sheet initial conditions have a large effect on the projections and give rise to important uncertainties. The goal of this initMIP-Greenland intercomparison exercise is to compare, evaluate, and improve the initialisation techniques used in the ice sheet modelling community and to estimate the associated uncertainties in modelled mass changes. initMIP-Greenland is the first in a series of ice sheet model intercomparison activities within ISMIP6 (the Ice Sheet Model Intercomparison Project for CMIP6), which is the primary activity within the Coupled Model Intercomparison Project Phase 6 (CMIP6) focusing on the ice sheets. Two experiments for the large-scale Greenland ice sheet have been designed to allow intercomparison between participating models of (1) the initial present-day state of the ice sheet and (2) the response in two idealised forward experiments. The forward experiments serve to evaluate the initialisation in terms of model drift (forward run without additional forcing) and in response to a large perturbation (prescribed surface mass balance anomaly); they should not be interpreted as sea-level projections. We present and discuss results that highlight the diversity of data sets, boundary conditions, and initialisation techniques used in the community to generate initial states of the Greenland ice sheet. We find good agreement across the ensemble for the dynamic response to surface mass balance changes in areas where the simulated ice sheets overlap but differences arising from the initial size of the ice sheet. The model drift in the control experiment is reduced for models that participated in earlier intercomparison exercises.},
	issn = {1994-0424},
	doi = {10.5194/tc-12-1433-2018},
	url = {https://www.the-cryosphere.net/12/1433/2018/},
	author = {Goelzer, Heiko and Nowicki, Sophie and Edwards, Tamsin and Beckley, Matthew and Abe-Ouchi, Ayako and Aschwanden, Andy and Calov, Reinhard and Gagliardini, Olivier and Gillet-Chaulet, Fabien and Golledge, Nicholas R. and Gregory, Jonathan and Greve, Ralf and Humbert, Angelika and Huybrechts, Philippe and Kennedy, Joseph H. and Larour, Eric and Lipscomb, William H. and Le clec\&apos;h, S{\'e}bastien and Lee, Victoria and Morlighem, Mathieu and Pattyn, Frank and Payne, Antony J. and Rodehacke, Christian and R{\"u}ckamp, Martin and Saito, Fuyuki and Schlegel, Nicole and Seroussi, Helene and Shepherd, Andrew and Sun, Sainan and van de Wal, Roderik and Ziemen, Florian A.}
}
@article {Roth2018,
	title = {{Modeling Winter Precipitation Over the Juneau Icefield, Alaska, Using a Linear Model of Orographic Precipitation}},
	journal = {Frontiers in Earth Science},
	volume = {6},
	number = {March},
	year = {2018},
	month = {mar},
	pages = {1{\textendash}19},
	keywords = {Alaska, downscaling, glacier mass balance, Juneau Icefield, Modeling, orographic precipitation, snow accumulation},
	issn = {2296-6463},
	doi = {10.3389/feart.2018.00020},
	url = {http://journal.frontiersin.org/article/10.3389/feart.2018.00020/full},
	author = {Roth, Aurora and Hock, Regine and Schuler, Thomas V. and Bieniek, Peter A. and Pelto, Mauri and Aschwanden, Andy}
}
@article {apr,
	title = {Asynchronous behavior of outlet glaciers feeding Godth{\aa}bsfjord (Nuup Kangerlua) and the triggering of Narsap Sermia{\textquoteright}s retreat in SW Greenland},
	journal = {J. Glaciol.},
	volume = {63},
	year = {2017},
	month = {apr},
	pages = {288{\textendash}308},
	abstract = {We assess ice loss and velocity changes between 1985 and 2014 of three tidewater and five-land terminating glaciers in Godth{\aa}bsfjord (Nuup Kangerlua), Greenland. Glacier thinning accounted for 43.8 {\textpm} 0.2 km 3 of ice loss, equivalent to 0.10 mm eustatic sea-level rise. An additional 3.5 {\textpm} 0.3 km 3 was lost to the calving retreats of Kangiata Nunaata Sermia (KNS) and Narsap Sermia (NS), two tidewater glaciers that exhibited asynchronous behavior over the study period. KNS has retreated 22 km from its Little Ice Age (LIA) maximum (1761 AD), of which 0.8 km since 1985. KNS has stabilized in shallow water, but seasonally advects a 2 km long floating tongue. In contrast, NS began retreating from its LIA moraine in 2004{\textendash}06 (0.6 km), re-stabilized, then retreated 3.3 km during 2010{\textendash}14 into an over-deepened basin. Velocities at KNS ranged 5{\textendash}6 km a -1 , while at NS they increased from 1.5 to 5.5 km a -1 between 2004 and 2014. We present comprehensive analyses of glacier thinning, runoff, surface mass balance, ocean conditions, submarine melting, bed topography, ice m{\'e}lange and conclude that the 2010{\textendash}14 NS retreat was triggered by a combination of factors but primarily by an increase in submarine melting.},
	keywords = {glacier calving, glacier discharge, glacier mass balance, ice/atmosphere interactions, ice/ocean interactions, tidewater glaciers},
	issn = {0022-1430},
	doi = {10.1017/jog.2016.138},
	author = {Motyka, Roman J. and Cassotto, Ryan and Truffer, Martin and Kjeldsen, Kristian K. and Van As, Dirk and Korsgaard, Niels J. and Fahnestock, Mark and Howat, Ian and Langen, Peter L. and Mortensen, John and Lennert, Kunuk and Rysgaard, S{\o}ren}
}
@article {313,
	title = {Diagnosing the decline in climatic mass balance of glaciers in Svalbard over 1957{\textendash}2014},
	journal = {The Cryosphere},
	volume = {11},
	year = {2017},
	pages = {191{\textendash}215},
	doi = {10.5194/tc-11-191-2017},
	url = {https://www.the-cryosphere.net/11/191/2017/},
	author = {{\O}stby, T. I. and Schuler, T. V. and Hagen, J. O. and Hock, R. and Kohler, J. and Reijmer, C. H.}
}
@article {283,
	title = {Derivation and analysis of a complete modern-date glacier inventory for Alaska and northwest Canada},
	journal = {Journal of Glaciology},
	volume = {61},
	year = {2015},
	pages = {403},
	author = {Kienholz, Christian and Herreid, Sam and Rich, J and Arendt, A and Hock, R and Burgess, E}
}
@article {MacGregor2015,
	title = {{Radiostratigraphy and age structure of the Greenland Ice Sheet}},
	journal = {Journal of Geophysical Research: Earth Surface},
	volume = {120},
	year = {2015},
	pages = {212{\textendash}241},
	keywords = {10.1002/2014JF003215 and Greenland Ice Sheet, ice core, ice-penetrating dynamics, ice-sheet dynamics},
	issn = {21699003},
	doi = {10.1002/2014JF003215},
	url = {http://doi.wiley.com/10.1002/2014JF003215},
	author = {MacGregor, Joseph A. and Fahnestock, Mark A. and Catania, Ginny A. and Paden, John D and Prasad Gogineni, S. and Young, S Keith and Rybarski, Susan C and Mabrey, Alexandria N and Wagman, Benjamin M and Morlighem, Mathieu}
}
@article {275,
	title = {Alaska National Park glaciers: what do they tell us about climate change?},
	journal = {Alaska Park Science},
	volume = {12},
	year = {2014},
	pages = {18{\textendash}25},
	author = {Loso, M.G. and Arendt, A. and Chris F. Larsen and Murphy, N. and Rich, J.}
}
@article {rebesco2014boundary,
	title = {Boundary condition of grounding lines prior to collapse, Larsen-B Ice Shelf, Antarctica},
	journal = {Science},
	volume = {345},
	number = {6202},
	year = {2014},
	pages = {1354{\textendash}1358},
	publisher = {American Association for the Advancement of Science},
	author = {Rebesco, M and Domack, E and Zgur, F and Lavoie, C and Leventer, A and Brachfeld, S and Willmott, V and Halverson, G and Truffer, M and Scambos, T and Pettit, Erin C}
}
@article {205,
	title = {Coupled ice sheet{\textendash}climate modeling under glacial and pre-industrial boundary conditions},
	journal = {Climate of the Past},
	volume = {10},
	year = {2014},
	pages = {1817-1836},
	chapter = {1817},
	abstract = {In the standard Paleoclimate Modelling Intercomparison Project (PMIP) experiments, the Last Glacial Maximum (LGM) is modeled in quasi-equilibrium with atmosphere{\textendash}ocean{\textendash}vegetation general circulation models (AOVGCMs) with prescribed ice sheets. This can lead to inconsistencies between the modeled climate and ice sheets. One way to avoid this problem would be to model the ice sheets explicitly. Here, we present the first results from coupled ice sheet{\textendash}climate simulations for the pre-industrial times and the LGM. 

Our setup consists of the AOVGCM ECHAM5/MPIOM/LPJ bidirectionally coupled with the Parallel Ice Sheet Model (PISM) covering the Northern Hemisphere. The results of the pre-industrial and LGM simulations agree reasonably well with reconstructions and observations. This shows that the model system adequately represents large, non-linear climate perturbations. 

A large part of the drainage of the ice sheets occurs in ice streams. Most modeled ice stream systems show recurring surges as internal oscillations. The Hudson Strait Ice Stream surges with an ice volume equivalent to about 5 m sea level and a recurrence interval of about 7000 yr. This is in agreement with basic expectations for Heinrich events. Under LGM boundary conditions, different ice sheet configurations imply different locations of deep water formation.
},
	doi = {10.5194/cp-10-1817-2014},
	url = {http://www.clim-past.net/10/1817/2014/cp-10-1817-2014.html},
	author = {Ziemen, F. A. and Rodehacke, C. B. and Mikolajewicz, U.}
}
@article {248,
	title = {The effect of climate forcing on numerical simulations of the Cordilleran ice sheet at the Last Glacial Maximum},
	journal = {The Cryosphere},
	volume = {8},
	year = {2014},
	pages = {1087{\textendash}1103},
	doi = {10.5194/tc-8-1087-2014},
	url = {http://www.the-cryosphere.net/8/1087/2014/},
	author = {Seguinot, J. and Khroulev, C. and Rogozhina, I. and Stroeven, A. P. and Zhang, Q.}
}
@article {280,
	title = {Glacier changes in the Karakoram region mapped by multimission satellite imagery},
	journal = {The Cryosphere},
	volume = {8},
	year = {2014},
	pages = {977{\textendash}989},
	author = {Rankl, Melanie and Kienholz, C and Braun, M}
}
@article {259,
	title = {Glaciers in the Earth{\textquoteright}s Hydrological Cycle: Assessments of Glacier Mass and Runoff Changes on Global and Regional Scales},
	journal = {Surveys in Geophysics},
	volume = {35},
	year = {2014},
	pages = {813-837},
	keywords = {Glacier projections, glacier runoff, glaciers, mass balance, Mass-balance observations, Modeling, Sea-level rise},
	issn = {0169-3298},
	doi = {10.1007/s10712-013-9262-y},
	url = {http://dx.doi.org/10.1007/s10712-013-9262-y},
	author = {Radi{\'c}, Valentina and Hock, Regine}
}
@article {257,
	title = {Global response of glacier runoff to twenty-first century climate change},
	journal = {Journal of Geophysical Research: Earth Surface},
	volume = {119},
	year = {2014},
	pages = {717{\textendash}730},
	keywords = {climate change, glacier mass balance, glacier runoff},
	issn = {2169-9011},
	doi = {10.1002/2013JF002931},
	url = {http://dx.doi.org/10.1002/2013JF002931},
	author = {Bliss, Andrew and Hock, Regine and Radi{\'c}, Valentina}
}
@article {220,
	title = {A new method for deriving glacier centerlines applied to glaciers in Alaska and northwest Canada},
	journal = {The Cryosphere},
	volume = {8},
	year = {2014},
	pages = {503{\textendash}519},
	doi = {10.5194/tc-8-503-2014},
	url = {http://www.the-cryosphere.net/8/503/2014/},
	author = {Kienholz, C. and Rich, J. L. and Arendt, A. A. and Hock, R.}
}
@article {240,
	title = {The Randolph Glacier Inventory: a globally complete inventory of glaciers},
	volume = {60},
	year = {2014},
	pages = {537 - 552},
	doi = {10.3189/2014JoG13J176},
	author = {Pfeffer, W.T. and Arendt, A. and Bliss, A. and Bolch, T. and Cogley, G. and Gardner, A. and Hagen, J-O., and Hock, R. and Kaser, G and Kienholz, C. and Miles, E. and Moholdt, G. and M{\"o}lg, N. and Paul, F. and Radi{\'c}, V. and Rastner, P. and Raup, B. and Rich, J. and Sharp, M.}
}
@article {2013/08/01,
	title = {Challenges to Understanding the Dynamic Response of Greenland{\textquoteright}s Marine Terminating Glaciers to Oceanic and Atmospheric Forcing},
	journal = {Bulletin of the American Meteorological Society},
	volume = {94},
	year = {2013},
	month = {2013/08/01},
	pages = {1131 - 1144},
	doi = {10.1175/BAMS-D-12-00100.1},
	url = {http://dx.doi.org/10.1175/BAMS-D-12-00100.1},
	author = {Straneo, Fiammetta and Heimbach, Patrick and Sergienko, Olga and Hamilton, Gordon and Catania, Ginny and Griffies, Stephen and Hallberg, Robert and Jenkins, Adrian and Joughin, Ian and Motyka, Roman and Pfeffer, W. Tad and Stephen F. Price and Eric Rignot and Scambos, Ted and Martin Truffer and Vieli, Andreas}
}
@article {sep,
	title = {Channelized ice melting in the ocean boundary layer beneath Pine Island Glacier, Antarctica.},
	journal = {Science (New York, N.Y.)},
	volume = {341},
	year = {2013},
	month = {sep},
	pages = {1236{\textendash}9},
	abstract = {Ice shelves play a key role in the mass balance of the Antarctic ice sheets by buttressing their seaward-flowing outlet glaciers; however, they are exposed to the underlying ocean and may weaken if ocean thermal forcing increases. An expedition to the ice shelf of the remote Pine Island Glacier, a major outlet of the West Antarctic Ice Sheet that has rapidly thinned and accelerated in recent decades, has been completed. Observations from geophysical surveys and long-term oceanographic instruments deployed down bore holes into the ocean cavity reveal a buoyancy-driven boundary layer within a basal channel that melts the channel apex by 0.06 meter per day, with near-zero melt rates along the flanks of the channel. A complex pattern of such channels is visible throughout the Pine Island Glacier shelf.},
	keywords = {Antarctic Regions, Freezing, Ice Cover, Oceans and Seas},
	issn = {1095-9203},
	doi = {10.1126/science.1239373},
	url = {http://www.ncbi.nlm.nih.gov/pubmed/24031016},
	author = {Stanton, T P and Shaw, W J and Truffer, M. and Corr, H F J and Peters, L E and Riverman, K L and Bindschadler, R and Holland, D M and Anandakrishnan, S}
}
@article {SeariseGreenland2013,
	title = {{Insights into spatial sensitivities of ice mass response to environmental change from the SeaRISE ice sheet modeling project II: Greenland}},
	journal = {J. Geophys. Res.},
	volume = {118},
	number = {2},
	year = {2013},
	month = {jun},
	pages = {1025{\textendash}1044},
	issn = {21699003},
	doi = {10.1002/jgrf.20076},
	url = {http://doi.wiley.com/10.1002/jgrf.20076},
	author = {Nowicki, Sophie and Robert A. Bindschadler and Abe-Ouchi, Ayako and Andy Aschwanden and E. Bueler and Choi, Hyeungu and Fastook, Jim and Granzow, Glen and Greve, Ralf and Gutowski, Gail and Herzfeld, Ute and Jackson, Charles and Jesse V Johnson and Constantine Khroulev and Larour, Eric and Anders Levermann and Lipscomb, William H. and Maria A. Martin and Morlighem, Mathieu and Parizek, Byron R. and David Pollard and Stephen F. Price and Ren, Diandong and Eric Rignot and Fuyuki Saito and Tatsuru Sato and Seddik, Hakime and Seroussi, Helene and Takahashi, Kunio and Walker, Ryan and Wang, Wei Li}
}
@article {SeariseAntarctica2013,
	title = {{Insights into spatial sensitivities of ice mass response to environmental change from the SeaRISE ice sheet modeling project I: Antarctica}},
	journal = {J. Geophys. Res.},
	volume = {118},
	number = {2},
	year = {2013},
	pages = {1002{\textendash}1024},
	issn = {21699003},
	doi = {10.1002/jgrf.20081},
	url = {http://doi.wiley.com/10.1002/jgrf.20081},
	author = {Nowicki, Sophie and Robert A. Bindschadler and Abe-Ouchi, Ayako and Andy Aschwanden and E. Bueler and Choi, Hyeungu and Fastook, Jim and Granzow, Glen and Greve, Ralf and Gutowski, Gail and Herzfeld, Ute and Jackson, Charles and Jesse V Johnson and Constantine Khroulev and Larour, Eric and Anders Levermann and Lipscomb, William H. and Maria A. Martin and Morlighem, Mathieu and Parizek, Byron R. and David Pollard and Stephen F. Price and Ren, Diandong and Eric Rignot and Fuyuki Saito and Tatsuru Sato and Seddik, Hakime and Seroussi, Helene and Takahashi, Kunio and Walker, Ryan and Wang, Wei Li}
}
@article {167,
	title = {Low-frequency radar sounding of temperate ice masses in Southern Alaska},
	journal = {Geophysical Research Letters},
	year = {2013},
	pages = {n/a{\textendash}n/a},
	abstract = {We present the Warm Ice Sounding Explorer (WISE), a low-frequency (2.5 MHz) radar for the sounding of temperate ice. WISE deployment in southern Alaska in 2008 and 2012 provides comprehensive measurements of glacier thickness, reveals deep valleys beneath glaciers and the full extent of zones grounded below sea level. The east branch of Columbia Glacier is deeper that its main branch and remains below sea level 20 km farther inland. Ice is 1000 m deep on Tazlina Glacier. On Bering glacier, two sills separate three deep bed depressions (>1200 m) that coincide with the dynamic balance lines during surges. The piedmont lobe of Malaspina Glacier and the lower reaches of Hubbard Glacier are entirely grounded below sea level 40 and 10 km, respectively, from their termini. Knowledge of ice thickness in these regions helps better understand their glacier dynamics, mass balance, and impact on sea level.},
	keywords = {Alaska, bed topography, glaciology, mass balance, radar, thickness},
	issn = {1944-8007},
	doi = {10.1002/2013GL057452},
	url = {http://dx.doi.org/10.1002/2013GL057452},
	author = {Eric Rignot and Mouginot, J. and Chris F. Larsen and Gim, Y. and Kirchner, D.}
}
@article {207,
	title = {An open ocean region in Neoproterozoic glaciations would have to be narrow to allow equatorial ice sheets},
	journal = {Geophysical Research Letters},
	volume = {40},
	year = {2013},
	pages = {5503{\textendash}5507},
	abstract = {A major goal of understanding Neoproterozoic glaciations and determining their effect on the evolution of life and Earth{\textquoteright}s atmosphere is establishing whether and how much open ocean there was during them. Geological evidence tells us that continental ice sheets had to flow into the ocean near the equator during these glaciations. Here we drive the Parallel Ice Sheet Model with output from four simulations of the ECHAM5/Max Planck Institute Ocean Model atmosphere-ocean general circulation model with successively narrower open ocean regions. We find that extensive equatorial ice sheets form on marine margins if sea ice extends to within about 20{\textdegree} latitude of the equator or less (Jormungand-like and hard snowball states), but do not form if there is more open ocean than this. Given uncertainty in topographical reconstruction and ice sheet ablation parameterizations, we perform extensive sensitivity tests to confirm the robustness of our main conclusions.},
	keywords = {ice sheet modeling, Neoproterozoic glaciations, snowball Earth},
	issn = {1944-8007},
	doi = {10.1002/2013GL057582},
	url = {http://dx.doi.org/10.1002/2013GL057582},
	author = {Rodehacke, Christian B. and Voigt, Aiko and Ziemen, Florian and Abbot, Dorian S.}
}
@article {127,
	title = {Regional and global projections of twenty-first century glacier mass changes in response to climate scenarios from global climate models},
	journal = {Climate Dynamics},
	year = {2013},
	pages = {1-22},
	keywords = {Global climate models, Projections of sea level rise, Regional and global glacier mass changes},
	issn = {0930-7575},
	doi = {10.1007/s00382-013-1719-7},
	url = {http://dx.doi.org/10.1007/s00382-013-1719-7},
	author = {Valentina Radi{\'c} and Andrew Bliss and Beedlow, A.Cody and Regine Hock and Miles, Evan and J. Graham Cogley}
}
@article {86,
	title = {The role of subsurface heat exchange: energy partitioning at Austfonna ice cap, Svalbard, over 2004-2008},
	journal = {Annals of Glaciology},
	volume = {54},
	year = {2013},
	pages = {229-240},
	doi = {10.3189/2013AoG63A280},
	author = {Torbj{\o}rn I. {\O}STBY and Schuler, T.V. and Jon Ove Hagen and Regine Hock and C H Reijmer}
}
@article {153,
	title = {On the seasonal freshwater stratification in the proximity of fast-flowing tidewater outlet glaciers in a sub-Arctic sill fjord},
	journal = {Journal of Geophysical Research: Oceans},
	volume = {118},
	year = {2013},
	pages = {1382{\textendash}1395},
	abstract = {The Greenland Ice Sheet releases large amounts of freshwater into the fjords around Greenland and many fjords are in direct contact with the ice sheet through tidewater outlet glaciers. Here we present the first seasonal hydrographic observations from the inner part of a sub-Arctic fjord, relatively close to and within 4{\textendash}50 km of a fast-flowing tidewater outlet glacier. This region is characterized by a dense glacial and sea ice cover. Freshwater from runoff, subglacial freshwater (SgFW) discharge, glacial, and sea ice melt are observed above 50{\textendash}90 m depth. During summer, SgFW and subsurface glacial melt mixed with ambient water are observed as a layered structure in the temperature profiles below the low-saline summer surface layer (<7 m). During winter, the upper water column is characterized by stepwise halo- and thermoclines formed by mixing between deeper layers and the surface layer influenced by ice melt. The warm (T > 1{\textdegree}C) intermediate water mass is a significant subsurface heat source for ice melt. We analyze the temperature and salinity profiles observed in late summer with a thermodynamic mixing model and determine the total freshwater content in the layer below the summer surface layer to be between 5\% and 11\%. The total freshwater contribution in this layer from melted glacial ice was estimated to be 1{\textendash}2\%, while the corresponding SgFW was estimated to be 3{\textendash}10\%. The winter measurements in the subsurface halocline layer showed a total freshwater content of about 1\% and no significant contribution from SgFW.},
	keywords = {fjord, freshwater sources and their distribution, Greenland Ice Sheet, subglacial freshwater fraction model, subsurface heat sources for glacial ice melt, tidewater outlet glaciers},
	issn = {2169-9291},
	doi = {10.1002/jgrc.20134},
	url = {http://dx.doi.org/10.1002/jgrc.20134},
	author = {Mortensen, J. and Bendtsen, J. and Roman J. Motyka and Lennert, K. and Martin Truffer and Mark Fahnestock and Rysgaard, S.}
}
@article {gusmeroli2012crystal,
	title = {The crystal fabric of ice from full-waveform borehole sonic logging},
	journal = {Journal of Geophysical Research: Earth Surface (2003{\textendash}2012)},
	volume = {117},
	number = {F3},
	year = {2012},
	publisher = {Wiley Online Library},
	author = {Alessio Gusmeroli and Erin C Pettit and Joseph H Kennedy and Ritz, Catherine}
}
@article {199,
	title = {Plate margin deformation and active tectonics along the northern edge of the Yakutat Terrane in the Saint Elias Orogen, Alaska, and Yukon, Canada},
	journal = {Geosphere},
	volume = {8},
	year = {2012},
	pages = {1384-1407},
	url = {http://www.scopus.com/inward/record.url?eid=2-s2.0-84873486244\&partnerID=40\&md5=6b0147233ff3aeb0e48bf9b253b6c6ec},
	author = {Bruhn, R.L. and Sauber, J. and Cotton, M.M. and Pavlis, T.L. and Evan W. Burgess and Ruppert, N. and Richard R. Forster}
}
@article {76,
	title = {{Using surface velocities to calculate ice thickness and bed topography: a case study at Columbia Glacier, Alaska, USA}},
	journal = {Journal of Glaciology},
	volume = {58},
	year = {2012},
	pages = {1151-1164},
	doi = {10.3189/2012JoG11J249},
	author = {R ~W McNabb and Regine Hock and Shad O'Neel and L ~A Rasmussen and Ahn, Y. and M Braun and H Conway and Herreid, S. and Ian Joughin and W. Tad Pfeffer and B ~E Smith and Martin Truffer}
}
@article {61,
	title = {Analysis of seasonal variations in mass balance and meltwater discharge of the tropical Zongo Glacier by application of a distributed energy balance model},
	journal = {Journal of Geophysical Research},
	volume = {116},
	year = {2011},
	pages = {D13105},
	doi = {10.1029/2010JD015105},
	author = {Sicart, JE and Regine Hock and Ribstein, P. and Litt, M. and Ramirez, E.}
}
@article {70,
	title = {Existence and stability of steady-state solutions of the shallow-ice-sheet equation by an energy-minimization approach},
	journal = {Journal of Glaciology},
	volume = {57},
	year = {2011},
	pages = {345{\textendash}354},
	url = {http://www.ingentaconnect.com/content/igsoc/jog/2011/00000057/00000202/art00016},
	author = {Guillaume Jouvet and Rappaz, J. and E. Bueler and Blatter, H.}
}
@article {64,
	title = {Glossary of glacier mass balance and related terms},
	journal = {IHP-VII Technical Documents in Hydrology},
	volume = {86},
	year = {2011},
	author = {J. Graham Cogley and Regine Hock and L ~A Rasmussen and Anthony A. Arendt and Bauder, A. and Braithwaite, RJ and Jansson, P. and Georg Kaser and M{\"o}ller, M. and Nicholson, L. and others}
}
@article {155,
	title = {An increase in crevasse extent, West Greenland: Hydrologic implications},
	journal = {Geophysical Research Letters},
	volume = {38},
	year = {2011},
	pages = {n/a{\textendash}n/a},
	abstract = {We compare high-resolution 1985 and 2009 imagery to assess changes in crevasse extent in the Sermeq Avannarleq ablation zone, West Greenland. The area occupied by crevasses >2 m wide significantly increased (13 {\textpm} 4\%) over the 24-year period. This increase consists of an expansion of existing crevasse fields, and is accompanied by widespread changes in crevasse orientation (up to 45{\textdegree}). We suggest that a combination of ice sheet thinning and steepening are responsible for the increase in crevasse extent. We examine the potential impact of this change on the hydrology of the ice sheet. We provide a first-order demonstration that moulin-type drainage is more efficient in transferring meltwater fluctuations to the subglacial system than crevasse-type drainage. As enhanced basal sliding is associated with meltwater {\textquotedblleft}pulses{\textquotedblright}, an increase in crevasse extent can therefore be expected to result in a net decrease in basal sliding sensitivity. An increase in crevasse extent may also accelerate cryo-hydrologic warming and enhance surface ablation.},
	keywords = {crevasses, Greenland, mass balance, velocity},
	issn = {1944-8007},
	doi = {10.1029/2011GL048491},
	url = {http://dx.doi.org/10.1029/2011GL048491},
	author = {Colgan, William and Steffen, Konrad and McLamb, W. Scott and Waleed Abdalati and Rajaram, Harihar and Roman J. Motyka and Phillips, Thomas and Robert S Anderson}
}
@article {67,
	title = {Observed glacial changes on the King George Island ice cap, Antarctica, in the last decade},
	journal = {Global and Planetary Change},
	volume = {79},
	year = {2011},
	pages = {99 - 109},
	keywords = {climate change},
	issn = {0921-8181},
	doi = {10.1016/j.gloplacha.2011.06.009},
	url = {http://www.sciencedirect.com/science/article/pii/S0921818111001111},
	author = {M R{\"u}ckamp and M Braun and S. Suckro and N. Blindow}
}
@article {62,
	title = {Regionally differentiated contribution of mountain glaciers and ice caps to future sea-level rise},
	journal = {Nature Geoscience},
	volume = {4},
	year = {2011},
	pages = {91{\textendash}94},
	doi = {10.1038/NGEO1052},
	author = {Valentina Radi{\'c} and Regine Hock}
}
@article {60,
	title = {Submarine melting of the 1985 Jakobshavn Isbr{\ae} floating tongue and the triggering of the current retreat},
	journal = {Journal of Geophysical Research},
	volume = {116},
	year = {2011},
	pages = {F01007},
	doi = {10.1029/2009JF001632},
	author = {Roman J. Motyka and Martin Truffer and Mark Fahnestock and Mortensen, J. and Rysgaard, S. and I M Howat}
}
@article {65,
	title = {Surface mass balance, thinning and iceberg production, Columbia Glacier, Alaska, 19482007},
	journal = {Journal of Glaciology},
	volume = {57},
	year = {2011},
	pages = {431{\textendash}440},
	author = {L ~A Rasmussen and H Conway and Krimmel, RM and Regine Hock}
}
@article {48,
	title = {Iceberg calving as a primary source of regional-scale glacier-generated seismicity in the St. Elias Mountains, Alaska},
	journal = {Journal of Geophysical Research},
	volume = {115},
	year = {2010},
	pages = {F04034},
	doi = {10.1029/2009JF001598},
	author = {Shad O'Neel and Chris F. Larsen and Rupert, N. and Hansen, R.}
}
@article {47,
	title = {Regional and global volumes of glaciers derived from statistical upscaling of glacier inventory data},
	journal = {Journal of Geophysical Research},
	volume = {115},
	year = {2010},
	pages = {F01010},
	doi = {10.1029/2009JF001373},
	author = {Valentina Radi{\'c} and Regine Hock}
}
@article {54,
	title = {Results from the Ice-Sheet Model Intercomparison ProjectHeinrich Event INtercOmparison (ISMIP HEINO)},
	journal = {Journal of Glaciology},
	volume = {56},
	year = {2010},
	pages = {371-383},
	abstract = {Results from the Heinrich Event INtercOmparison (HEINO) topic of the Ice-Sheet Model Intercomparison Project (ISMIP) are presented. ISMIP HEINO was designed to explore internal large-scale ice-sheet instabilities in different contemporary ice-sheet models. These instabilities are of interest because they are a possible cause of Heinrich events. A simplified geometry experiment reproduces the main characteristics of the Laurentide ice sheet, including the sedimented region over Hudson Bay and Hudson Strait. The model experiments include a standard run plus seven variations. Nine dynamic/thermodynamic ice-sheet models were investigated; one of these models contains a combination of the shallow-shelf (SSA) and shallow-ice approximation (SIA), while the remaining eight models are of SIA type only. Seven models, including the SIA-SSA model, exhibit oscillatory surges with a period of \&$\#$8764;1000 years for a broad range of parameters, while two models remain in a permanent state of streaming for most parameter settings. In a number of models, the oscillations disappear for high surface temperatures, strong snowfall and small sediment sliding parameters. In turn, low surface temperatures and low snowfall are favourable for the ice-surge cycles. We conclude that further improvement of ice-sheet models is crucial for adequate, robust simulations of cyclic large-scale instabilities.},
	doi = {doi:10.3189/002214310792447789},
	url = {http://www.ingentaconnect.com/content/igsoc/jog/2010/00000056/00000197/art00001},
	author = {Calov, Reinhard and Greve, Ralf and Abe-Ouchi, Ayako and E. Bueler and Huybrechts, Philippe and Jesse V Johnson and Frank Pattyn and David Pollard and Ritz, Catherine and Fuyuki Saito and Tarasov, Lev}
}
@article {57,
	title = {Sky longwave radiation on tropical Andean glaciers: parameterization and sensitivity to atmospheric variables},
	journal = {Journal of Glaciology},
	volume = {56},
	year = {2010},
	pages = {854{\textendash}860},
	author = {Sicart, JE and Regine Hock and Ribstein, P. and Chazarin, J.P.}
}
@article {36,
	title = {Mountain glaciers and ice caps around Antarctica make a large sea-level rise contribution},
	journal = {Geophysical Research Letters},
	volume = {36},
	year = {2009},
	pages = {L07501},
	author = {Regine Hock and de Woul, M. and Valentina Radi{\'c} and Dyurgerov, M.}
}
@article {22,
	title = {Analysis of scaling methods in deriving future volume evolutions of valley glaciers},
	journal = {Journal of Glaciology},
	volume = {54},
	year = {2008},
	pages = {601{\textendash}612},
	author = {Valentina Radi{\'c} and Regine Hock and Oerlemans, J.}
}
@article {Pattyn2008,
	title = {{Benchmark experiments for higher-order and full Stokes ice sheet models (ISMIP-HOM)}},
	journal = {The Cryosphere},
	volume = {2},
	year = {2008},
	pages = {95{\textendash}108},
	author = {Frank Pattyn and Perichon, L. and Andy Aschwanden and Breuer, B. and de Smedt, B. and Gagliardini, O. and Gudmundsson, G. H. and Hindmarsh, R. C. A. and Hubbard, A. L. and Jesse V Johnson and Kleiner, T. and Konovalov, Y. and Martin, C. and Payne, A. J. and David Pollard and Stephen F. Price and M R{\"u}ckamp and Fuyuki Saito and Sou{\v c}ek, O. and Sugiyama, S. and Zwinger, T.}
}
@article {21,
	title = {Internal accumulation on Storglaciaren, Sweden, in a multi-layer snow model coupled to a distributed energy-and mass-balance model},
	journal = {Journal of Glaciology},
	volume = {54},
	year = {2008},
	pages = {61{\textendash}72},
	author = {C H Reijmer and Regine Hock}
}
@article {200,
	title = {Mass balance of the Greenland ice sheet from 1958 to 2007},
	journal = {Geophysical Research Letters},
	volume = {35},
	year = {2008},
	url = {http://www.scopus.com/inward/record.url?eid=2-s2.0-58249086581\&partnerID=40\&md5=f29d2f8e4a2c1845220d5fc846c65f0a},
	author = {Eric Rignot and Box, J.E. and Evan W. Burgess and Hanna, E.}
}
@article {26,
	title = {Recent glacier mass changes in the Gulf of Alaska region from GRACE mascon solutions},
	journal = {Journal of Glaciology},
	volume = {54},
	year = {2008},
	pages = {767{\textendash}777},
	author = {Scott B Luthcke and Anthony A. Arendt and Rowlands, D.D. and J J McCarthy and Chris F. Larsen}
}
@article {20,
	title = {Seasonal fluctuations in the advance of a tidewater glacier and potential causes: Hubbard Glacier, Alaska, USA},
	journal = {Journal of Glaciology},
	volume = {54},
	year = {2008},
	pages = {401{\textendash}411},
	url = {http://openurl.ingenta.com/content/xref?genre=article\&issn=0022-1430\&volume=54\&issue=186\&spage=401},
	author = {Ritchie, J.B. and C S Lingle and Roman J. Motyka and Martin Truffer}
}
@article {11,
	title = {Climate sensitivity of Storglaciaren, Sweden: an intercomparison of mass-balance models using ERA-40 re-analysis and regional climate model data},
	journal = {Annals of glaciology},
	volume = {46},
	year = {2007},
	pages = {342{\textendash}348},
	author = {Regine Hock and Valentina Radi{\'c} and de Woul, M.}
}
@conference {10,
	title = {Deriving glacier mass balance from accumulation area ratio on Storglaci{\"a}ren, Sweden.},
	booktitle = {Proceedings of a workshop on Andean Glaciology and a symposium on the Contribution from Glaciers and Snow Cover to Runoff from Mountains in Different Climates during the 7th Scientific Assembly of the IAHS, Foz do Iguacu, Brazil, 4-9 April 2005.},
	year = {2007},
	publisher = {IAHS Press},
	organization = {IAHS Press},
	author = {Regine Hock and Kootstra, D.S. and C H Reijmer and Ginot, P. and Sicart, JE and others}
}
@article {4,
	title = {Volumearea scaling vs flowline modelling in glacier volume projections},
	journal = {Annals of Glaciology},
	volume = {46},
	year = {2007},
	pages = {234{\textendash}240},
	author = {Valentina Radi{\'c} and Regine Hock and Oerlemans, J.}
}
@article {366,
	title = {Probing the till beneath Black Rapids Glacier, Alaska, USA},
	journal = {J. Glaciol.},
	volume = {50},
	year = {2004},
	pages = {608{\textendash}614},
	issn = {00221430},
	doi = {10.3189/172756504781829693},
	url = {http://openurl.ingenta.com/content/xref?genre=article{\&}issn=0022-1430{\&}volume=50{\&}issue=171{\&}spage=608},
	author = {Harrison, W.D. and Truffer, M. and Echelmeyer, K. A. and Pomraning, D. A. and Abnett, K. A. and Ruhkick, R. H.}
}
