@article {336,
	title = {Circumpolar Deep Water Impacts Glacial Meltwater Export and Coastal Biogeochemical Cycling Along the West Antarctic Peninsula},
	journal = {Frontiers in Marine Science},
	volume = {6},
	year = {2019},
	pages = {1{\textendash}23},
	keywords = {Antarctic Peninsula, ice, meltwater, phytoplankton},
	issn = {2296-7745},
	doi = {10.3389/fmars.2019.00144},
	url = {https://www.frontiersin.org/article/10.3389/fmars.2019.00144/full},
	author = {Cape, Mattias R. and Vernet, Maria and Pettit, Erin C. and Wellner, Julia and Truffer, Martin and Akie, Garrett and Domack, Eugene and Leventer, Amy and Smith, Craig R. and Huber, Bruce A.}
}
@article {333,
	title = {The Larsen Ice Shelf System, Antarctica (LARISSA): Polar Systems Bound Together, Changing Fast},
	journal = {GSA Today},
	volume = {29},
	year = {2019},
	pages = {4{\textendash}10},
	abstract = {Climatic, cryospheric, and biologic changes taking place in the northern Antarctic Peninsula provide examples for how ongoing systemic change may pro- gress through the entire Antarctic system. A large, interdisciplinary research project focused on the Larsen Ice Shelf system, synthesized here, has documented dramatic ice cover, oceanographic, and ecosystem changes in the Antarctic Peninsula during the Holocene and the present period of rapid regional warming. The responsive- ness of the region results from its position in the climate and ocean system, in which a narrow continental block extends across zonal atmospheric and ocean flow, creating high snow accumulation, strong gradients and gyres, dynamic oceanography, outlet glaciers feeding into many fjords and bays having steep topography, and a continental shelf that contains many glacially carved troughs separated by areas of glacial sedi- ment accumulation. The microcosm of the northern Antarctic Peninsula has a ten- dency to change rapidly{\textemdash}rapid relative not just to Antarctica{\textquoteright}s mainland but compared to the rest of the planet as well{\textemdash}and it is generally warmer than the rest of Antarctica. Both its Holocene and modern glaciological retreats offer a picture of how larger areas of Antarctica farther south might change under future warming.},
	issn = {10525173},
	doi = {10.1130/gsatg382a.1},
	author = {Wellner, Julia and Scambos, Ted and Domack, Eugene and Vernet, Maria and Leventer, Amy and Balco, Greg and Brachfeld, Stefanie and Cape, Mattias and Huber, Bruce and Ishman, Scott and McCormick, Michael and Mosley-Thompson, Ellen and Pettit, Erin and Smith, Craig and Truffer, Martin and Van Dover, Cindy and Yoo, Kyu-Cheul}
}
@article {335,
	title = {Tracking icebergs with time-lapse photography and sparse optical flow , LeConte Bay , Alaska , 2016 {\textendash} 2017},
	journal = {J. Glaciol.},
	volume = {65},
	year = {2019},
	pages = {195{\textendash}211},
	keywords = {glaciological instruments and methods, ice, icebergs, ocean interactions, Remote sensing},
	doi = {10.1017/jog.2018.105},
	author = {Kienholz, Christian and Amundson, Jason M and Motyka, Roman J and Jackson, Rebecca H and Mickett, John B and Sutherland, David A and Nash, Jonathan D and Winters, Dylan S and Dryer, William P and Truffer, Martin}
}
@article {Kiaer2018,
	title = {{A large impact crater beneath Hiawatha Glacier in northwest Greenland}},
	journal = {Science Advances},
	volume = {4},
	number = {11},
	year = {2018},
	month = {nov},
	pages = {eaar8173},
	abstract = {We report the discovery of a large impact crater beneath Hiawatha Glacier in northwest Greenland. From airborne radar surveys, we identify a 31-kilometer-wide, circular bedrock depression beneath up to a kilometer of ice. This depression has an elevated rim that cross-cuts tributary subglacial channels and a subdued central uplift that appears to be actively eroding. From ground investigations of the deglaciated foreland, we identify overprinted structures within Precambrian bedrock along the ice margin that strike tangent to the subglacial rim. Glaciofluvial sediment from the largest river draining the crater contains shocked quartz and other impact-related grains. Geochemical analysis of this sediment indicates that the impactor was a fractionated iron asteroid, which must have been more than a kilometer wide to produce the identified crater. Radiostratigraphy of the ice in the crater shows that the Holocene ice is continuous and conformable, but all deeper and older ice appears to be debris rich or heavily disturbed. The age of this impact crater is presently unknown, but from our geological and geophysical evidence, we conclude that it is unlikely to predate the Pleistocene inception of the Greenland Ice Sheet.},
	issn = {23752548},
	doi = {10.1126/sciadv.aar8173},
	url = {http://advances.sciencemag.org/ http://advances.sciencemag.org/lookup/doi/10.1126/sciadv.aar8173},
	author = {Kj{\ae}r, Kurt H. and Larsen, Nicolaj K and Binder, Tobias and Bj{\o}rk, Anders A and Eisen, Olaf and Fahnestock, Mark A and Funder, Svend and Garde, Adam A and Haack, Henning and Helm, Veit and Houmark-Nielsen, Michael and Kjeldsen, Kristian K and Khan, Shfaqat A and Machguth, Horst and McDonald, Iain and Morlighem, Mathieu and Mouginot, J{\'e}r{\'e}mie and Paden, John D and Waight, Tod E and Weikusat, Christian and Willerslev, Eske and MacGregor, Joseph A.}
}
@article {312,
	title = {Glacier Changes in the Susitna Basin, Alaska, USA,(1951{\textendash}2015) using GIS and Remote Sensing Methods},
	journal = {Remote Sensing},
	volume = {9},
	year = {2017},
	pages = {478},
	author = {Wastlhuber, Roland and Hock, Regine and Kienholz, Christian and Braun, Matthias}
}
@article {Khan2016,
	title = {{Geodetic measurements reveal similarities between post-Last Glacial Maximum and present-day mass loss from the Greenland ice sheet}},
	journal = {Science Advances},
	volume = {2},
	number = {9},
	year = {2016},
	month = {sep},
	pages = {e1600931{\textendash}e1600931},
	issn = {2375-2548},
	doi = {10.1126/sciadv.1600931},
	url = {http://advances.sciencemag.org/cgi/doi/10.1126/sciadv.1600931},
	author = {Khan, Shfaqat A and Sasgen, Ingo and Bevis, Michael and van Dam, T. and Bamber, Jonathan L and Wahr, John and Willis, Michael and Kjaer, K. H. and Wouters, Bert and Helm, Veit and Csatho, Beata and Fleming, Kevin and Bjork, A. A. and Aschwanden, Andy and Knudsen, Per and Munneke, Peter Kuipers}
}
@article {Muresan2016,
	title = {{Modelled glacier dynamics over the last quarter of a century at Jakobshavn Isbr{\ae}}},
	journal = {The Cryosphere},
	volume = {10},
	number = {2},
	year = {2016},
	month = {mar},
	pages = {597{\textendash}611},
	issn = {1994-0424},
	doi = {10.5194/tc-10-597-2016},
	url = {http://www.the-cryosphere.net/10/597/2016/},
	author = {Muresan, Ioana S. and Khan, Shfaqat A. and Aschwanden, Andy and Khroulev, Constantine and Van Dam, Tonie and Bamber, Jonathan and van den Broeke, Michiel R. and Wouters, Bert and Kuipers Munneke, Peter and Kj{\ae}r, Kurt H.}
}
@article {oct,
	title = {Sensitivity of Pine Island Glacier to observed ocean forcing},
	journal = {Geophysical Research Letters},
	volume = {43},
	year = {2016},
	month = {oct},
	pages = {10,817{\textendash}10,825},
	abstract = {{\textcopyright}2016. American Geophysical Union. All Rights Reserved.We present subannual observations (2009{\textendash}2014) of a major West Antarctic glacier (Pine Island Glacier) and the neighboring ocean. Ongoing glacier retreat and accelerated ice flow were likely triggered a few decades ago by increased ocean-induced thinning, which may have initiated marine ice sheet instability. Following a subsequent 60{\%} drop in ocean heat content from early 2012 to late 2013, ice flow slowed, but by {\textless} 4{\%}, with flow recovering as the ocean warmed to prior temperatures. During this cold-ocean period, the evolving glacier-bed/ice shelf system was also in a geometry favorable to stabilization. However, despite a minor, temporary decrease in ice discharge, the basin-wide thinning signal did not change. Thus, as predicted by theory, once marine ice sheet instability is underway, a single transient high-amplitude ocean cooling has only a relatively minor effect on ice flow. The long-term effects of ocean temperature variability on ice flow, however, are not yet known.},
	keywords = {glacier-ocean interactions, Ice Dynamics, ice shelves, ice streams, marine ice sheet instability},
	issn = {00948276},
	doi = {10.1002/2016GL070500},
	url = {http://doi.wiley.com/10.1002/2016GL070500},
	author = {Christianson, Knut and Bushuk, Mitchell and Dutrieux, Pierre and Parizek, Byron R. and Joughin, Ian R. and Alley, Richard B. and Shean, David E. and Abrahamsen, E. Povl and Anandakrishnan, Sridhar and Heywood, Karen J. and Kim, Tae-Wan and Lee, Sang Hoon and Nicholls, Keith and Stanton, Tim and Truffer, Martin and Webber, Benjamin G. M. and Jenkins, Adrian and Jacobs, Stan and Bindschadler, Robert and Holland, David M.}
}
@article {282,
	title = {End-of-winter snow depth variability on glaciers in Alaska},
	journal = {Journal of Geophysical Research: Earth Surface},
	volume = {120},
	year = {2015},
	pages = {1530{\textendash}1550},
	author = {McGrath, Daniel and Sass, Louis and O{\textquoteright}Neel, Shad and Arendt, Anthony and Wolken, Gabriel and Gusmeroli, Alessio and Kienholz, Christian and McNeil, Christopher}
}
@article {Khan2015,
	title = {{Greenland ice sheet mass balance}},
	journal = {Reports on Progress in Physics},
	volume = {78},
	number = {46801},
	year = {2015},
	pages = {26},
	publisher = {IOP Publishing},
	abstract = {Mass balance equation for glaciers; areal distribution and ice volumes; estimates of actual mass balance; loss by calving of icebergs; hydrological budget for Greenland; and temporal variations of Greenland mass balance are examined.},
	doi = {10.1088/0034-4885/78/4/046801},
	url = {http://dx.doi.org/10.1088/0034-4885/78/4/046801},
	author = {Khan, Shfaqat A. and Aschwanden, Andy and Bj{\o}rk, Anders A and Whar, John and Kjeldsen, Kristian K. and Kj{\ae}r, Kurt H.}
}
@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 {274,
	title = {Subglacial discharge at tidewater glaciers revealed by seismic tremor},
	journal = {Geophysical Research Letters},
	year = {2015},
	author = {Bartholomaus, Timothy C and Amundson, Jason M and Walter, Jacob I and O{\textquoteright}Neel, Shad and West, Michael E and Chris F. Larsen}
}
@article {289,
	title = {Tidal and seasonal variations in calving flux observed with passive seismology},
	journal = {Journal of Geophysical Research: Earth Surface},
	year = {2015},
	author = {Bartholomaus, Timothy C and Larsen, Christopher F and West, Michael E and O{\textquoteright}Neel, Shad and Pettit, Erin C and Truffer, Martin}
}
@article {05/2015,
	title = {Triggered Seismic Events along the Eastern Denali Fault in Northwest Canada Following the 2012 Mw 7.8 Haida Gwaii, 2013 Mw 7.5 Craig, and Two Mw>8.5 Teleseismic Earthquakes},
	journal = {Bulletin of the Seismological Society of America},
	volume = {105},
	year = {2015},
	month = {05/2015},
	chapter = {1165},
	abstract = {We conduct a systematic search for remotely triggered seismic activity along the eastern Denali fault (EDF) in northwest Canada, an intraplate strike-slip region. We examine 19 distant earthquakes recorded by nine broadband stations in the Canadian National Seismograph Network and find that the 2012 Mw 7.8 Haida Gwaii and 2013 Mw 7.5 Craig, Alaska, earthquakes triggered long duration (>10  s), emergent tremor-like signals near the southeastern portion of the EDF. In both cases, tremor coincides with the peak transverse velocities, consistent with Love-wave triggering on right-lateral strike-slip faults. The 2011 Mw 9.0 Tohoku-Oki and 2012 Mw 8.6 Indian Ocean earthquakes possibly triggered tremor signals, although we were unable to locate those sources. In addition, we also identify many short-duration (<5  s) bursts that were repeatedly triggered by the Rayleigh waves of the 2012 Mw 7.8 Haida Gwaii earthquake. Although we were unable to precisely locate the short-duration (<5  s) events, they appear to be radiating from the direction of the Klutlan Glacier and from a belt of shallow historical seismicity at the eastern flank of the Wrangell{\textendash}St. Elias mountain range. The fact that these events were triggered solely by the Rayleigh waves suggests a different source mechanism as compared with triggered tremor observed along the EDF and other plate boundary regions. },
	doi = {10.1785/0120140156},
	url = {http://www.bssaonline.org/content/early/2015/04/08/0120140156.abstract},
	author = {Chastity Aiken and Jessica Zimmerman Mejia}
}
@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 {279,
	title = {Glacier area and length changes in Norway from repeat inventories},
	journal = {The Cryosphere},
	volume = {8},
	year = {2014},
	pages = {1885{\textendash}1903},
	author = {Winsvold, S. H. and Andreassen, L. M. and Kienholz, C.}
}
@article {239,
	title = {Helicopter borne radar imaging of snow cover on and around glaciers in {A}laska},
	journal = {Annals of Glaciology},
	volume = {55},
	year = {2014},
	pages = {78-88},
	doi = {10.3189/2014AoG67A029},
	author = {Gusmeroli, A. and Wolken, G. and Arendt, A.}
}
@article {pettit2014influence,
	title = {Influence of debris-rich basal ice on flow of a polar glacier},
	journal = {Journal of Glaciology},
	volume = {60},
	number = {223},
	year = {2014},
	pages = {989{\textendash}1006},
	publisher = {International Glaciological Society},
	author = {Pettit, Erin C and Whorton, Erin N and Waddington, Edwin D and Sletten, Ronald S}
}
@article {354,
	title = {Surface Drifters Track the Fate of Greenland Ice Sheet Meltwater},
	journal = {Eos Trans. AGU},
	volume = {95},
	year = {2014},
	pages = {237{\textendash}239},
	doi = {10.1002/2014EO260002},
	author = {Hauri, C. and Truffer, M. and Winsor, P. and Lennert, K.}
}
@article {125,
	title = {Glaciers and ice caps (outside Greenland)},
	year = {2013},
	institution = { Bull. Amer. Meteor. Soc. 94(7), S143},
	author = {G. J. Wolken and Martin J. Sharp and M-L. Geai and D. Burges and Anthony A. Arendt and Bert Wouters}
}
@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 {132,
	title = {A Reconciled Estimate of Glacier Contributions to Sea Level Rise: 2003 to 2009},
	journal = {Science},
	volume = {340},
	year = {2013},
	pages = {852-857},
	abstract = {Glaciers distinct from the Greenland and Antarctic Ice Sheets are losing large amounts of water to the world{\textquoteright}s oceans. However, estimates of their contribution to sea level rise disagree. We provide a consensus estimate by standardizing existing, and creating new, mass-budget estimates from satellite gravimetry and altimetry and from local glaciological records. In many regions, local measurements are more negative than satellite-based estimates. All regions lost mass during 2003{\textendash}2009, with the largest losses from Arctic Canada, Alaska, coastal Greenland, the southern Andes, and high-mountain Asia, but there was little loss from glaciers in Antarctica. Over this period, the global mass budget was {\textendash}259 {\textpm} 28 gigatons per year, equivalent to the combined loss from both ice sheets and accounting for 29 {\textpm} 13\% of the observed sea level rise.},
	doi = {10.1126/science.1234532},
	url = {http://www.sciencemag.org/content/340/6134/852.abstract},
	author = {Alex S. Gardner and Geir Moholdt and J. Graham Cogley and Bert Wouters and Anthony A. Arendt and Wahr, John and Berthier, Etienne and Regine Hock and W. Tad Pfeffer and Georg Kaser and Ligtenberg, Stefan R. M. and Bolch, Tobias and Martin J. Sharp and Jon Ove Hagen and van den Broeke, Michiel R. and Paul, Frank}
}
@article {lee2013underwater,
	title = {Underwater sound radiated by bubbles released by melting glacier ice},
	journal = {The Journal of the Acoustical Society of America},
	volume = {134},
	number = {5},
	year = {2013},
	pages = {4172{\textendash}4172},
	publisher = {Acoustical Society of America},
	author = {Lee, Kevin M and Wilson, Preston S and Pettit, Erin C}
}
@article {121,
	title = {Accelerated contributions of Canada{\textquoteright}s Baffin and Bylot Island glaciers to sea level rise over the past half century},
	journal = {The Cryosphere},
	volume = {6},
	year = {2012},
	pages = {1103{\textendash}1125},
	doi = {10.5194/tc-6-1103-2012},
	author = {Alex S. Gardner and Geir Moholdt and Anthony A. Arendt and Bert Wouters}
}
@article {mar,
	title = {Analysis of low-frequency seismic signals generated during a multiple-iceberg calving event at Jakobshavn Isbr{\ae}, Greenland},
	journal = {Journal of Geophysical Research},
	volume = {117},
	year = {2012},
	month = {mar},
	pages = {1{\textendash}11},
	keywords = {calving, glacier, iceberg, seismology},
	issn = {0148-0227},
	doi = {10.1029/2011JF002132},
	url = {http://www.agu.org/pubs/crossref/2012/2011JF002132.shtml},
	author = {Walter, F. and Amundson, J. M. and O{\textquoteright}Neel, S. and Truffer, M. and Fahnestock, M.A. and Fricker, H. A.}
}
@article {80,
	title = {Calving seismicity from iceberg{\textendash}sea surface interactions},
	journal = {Journal of Geophysical Research},
	volume = {117},
	year = {2012},
	pages = {F04029},
	doi = {10.1029/2012JF002513},
	author = {Timothy C. Bartholomaus and Chris F. Larsen and Shad O'Neel and West, M.}
}
@article {11/2011,
	title = {Mountain Glaciers and ice caps},
	number = {xii},
	year = {2012},
	month = {11/2011},
	pages = {538},
	institution = {Arctic Monitoring and Assessment Programme (AMAP)},
	address = {Oslo, Norway},
	isbn = {978-82-7971-071-4},
	author = {Martin J. Sharp and M. Ananicheva and Anthony A. Arendt and Jon Ove Hagen and Regine Hock and E. Josberger and R. D. Moore and W. Tad Pfeffer and G. J. Wolken}
}
@article {pettit2011crossover,
	title = {The crossover stress, anisotropy and the ice flow law at Siple Dome, West Antarctica},
	journal = {Journal of Glaciology},
	volume = {57},
	number = {201},
	year = {2011},
	pages = {39{\textendash}52},
	publisher = {International Glaciological Society},
	author = {Erin C Pettit and Waddington, Edwin D and Harrison, William D and Thorsteinsson, Throstur and Elsberg, Daniel and Morack, John and Zumberge, Mark A}
}
@article {198,
	title = {Greenland Ice Sheet surface mass balance 1870 to 2010 based on Twentieth Century Reanalysis, and links with global climate forcing},
	journal = {Journal of Geophysical Research D: Atmospheres},
	volume = {116},
	year = {2011},
	url = {http://www.scopus.com/inward/record.url?eid=2-s2.0-84855336557\&partnerID=40\&md5=9239bc453a5004bd7a1258a2aaa14f07},
	author = {Hanna, E. and Huybrechts, P. and Cappelen, J. and Steffen, K. and Bales, R.C. and Evan W. Burgess and McConnell, J.R. and Steffensen, J.P. and Van Den Broeke, M. and Wake, L. and Bigg, G. and Griffiths, M. and Savas, D.}
}
@article {72,
	title = {The Potsdam Parallel Ice Sheet Model (PISM-PIK)-Part 2: Dynamic equilibrium simulation of the Antarctic ice sheet},
	journal = {The Cryosphere},
	volume = {5},
	year = {2011},
	pages = {727-740},
	doi = {10.5194/tc-5-727-2011},
	url = {http://www.the-cryosphere.net/5/727/2011/tc-5-727-2011.html},
	author = {Maria A. Martin and Winkelmann, R. and Haseloff, M. and Albrecht, T. and E. Bueler and Constantine Khroulev and Anders Levermann}
}
@article {71,
	title = {The Potsdam Parallel Ice Sheet Model (PISM-PIK){\textendash}Part 1: Model description},
	journal = {The Cryosphere},
	volume = {5},
	year = {2011},
	pages = {715{\textendash}726},
	doi = {10.5194/tc-5-715-2011},
	url = {http://www.the-cryosphere.net/5/715/2011/tc-5-715-2011.html},
	author = {Winkelmann, R. and Maria A. Martin and Haseloff, M. and Albrecht, T. and E. Bueler and Constantine Khroulev and Anders Levermann}
}
@article {44,
	title = {Glacier microseismicity},
	journal = {Geology},
	volume = {38},
	year = {2010},
	pages = {319-322},
	abstract = {We present a framework for interpreting small glacier seismic events based on data collected near the center of Bering Glacier, Alaska, in spring 2007. We find extremely high microseismicity rates (as many as tens of events per minute) occurring largely within a few kilometers of the receivers. A high-frequency class of seismicity is distinguished by dominant frequencies of 20{\textendash}35 Hz and impulsive arrivals. A low-frequency class has dominant frequencies of 6{\textendash}15 Hz, emergent onsets, and longer, more monotonic codas. A bimodal distribution of 160,000 seismic events over two months demonstrates that the classes represent two distinct populations. This is further supported by the presence of hybrid waveforms that contain elements of both event types. The high-low-hybrid paradigm is well established in volcano seismology and is demonstrated by a comparison to earthquakes from Augustine Volcano. We build on these parallels to suggest that fluid-induced resonance is likely responsible for the low-frequency glacier events and that the hybrid glacier events may be caused by the rush of water into newly opening pathways.},
	doi = {10.1130/G30606.1},
	url = {http://geology.gsapubs.org/content/38/4/319.abstract},
	author = {West, M. and Chris F. Larsen and Martin Truffer and Shad O'Neel and LeBlanc, Laura}
}
@article {51,
	title = {Recent and future warm extreme events and high-mountain slope stability},
	journal = {Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences},
	volume = {368},
	year = {2010},
	pages = {2435{\textendash}2459},
	doi = {10.1098/rsta.2010.0078},
	author = {Huggel, C. and Salzmann, N. and Allen, S. and Caplan-Auerbach, J. and L Fischer  and Haeberli, W. and Chris F. Larsen and Schneider, D. and Wessels, R.}
}
@article {42,
	title = {Changes of glaciers and climate in northwestern North America during the late twentieth century},
	journal = {Journal of Climate},
	volume = {22},
	year = {2009},
	pages = {4117{\textendash}4134},
	author = {Anthony A. Arendt and Walsh, J. and Harrison, W.}
}
@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 {32,
	title = {Glacier, fjord, and seismic response to recent large calving events, Jakobshavn Isbr{\ae}, Greenland},
	journal = {Geophysical Research Letters},
	volume = {35},
	year = {2008},
	pages = {L22501},
	url = {http://www.agu.org/pubs/crossref/2008/2008GL035281.shtml},
	author = {Jason M Amundson and Martin Truffer and M P L{\"u}thi and Mark Fahnestock and West, M. and Roman J. Motyka}
}
@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.}
}
@article {9,
	title = {Glacier-dammed lake outburst events of Gornersee, Switzerland},
	journal = {Journal of Glaciology},
	volume = {53},
	year = {2007},
	pages = {189{\textendash}200},
	author = {Huss, M. and Bauder, A. and Werder, M. and Funk, M. and Regine Hock}
}
@article {pettit2007role,
	title = {The role of crystal fabric in flow near an ice divide},
	journal = {Journal of Glaciology},
	volume = {53},
	number = {181},
	year = {2007},
	pages = {277{\textendash}288},
	publisher = {International Glaciological Society},
	author = {Erin C Pettit and Thorsteinsson, Throstur and Jacobson, H Paul and Waddington, Edwin D}
}
@article {conway2005candidate,
	title = {Candidate drill site near the Ross-Amundsen ice divide, West Antarctica},
	journal = {DRAFT, Mar},
	year = {2005},
	author = {Conway, H and Neumann, TA and Stephen F. Price and Waddington, ED and Morse, D and Taylor, K and Mayewski, PA and Dixon, D and Erin C Pettit and Steig, EJ}
}
@article {conway2005proposed,
	title = {Proposed drill site near the Ross{\textendash}Amundsen ice divide, West Antarctica},
	journal = {White Paper for the US Ice Core Working Group},
	year = {2005},
	author = {Conway, H and Neumann, TA and Stephen F. Price and Waddington, ED and Morse, D and Taylor, K and Mayewski, PA and Dixon, D and Erin C Pettit and Steig, EJ}
}
@article {elsberg2004depth,
	title = {Depth-and time-dependent vertical strain rates at Siple Dome, Antarctica},
	journal = {Journal of Glaciology},
	volume = {50},
	number = {171},
	year = {2004},
	pages = {511{\textendash}521},
	publisher = {International Glaciological Society},
	author = {Elsberg, Daniel H and Harrison, William D and Zumberge, Mark A and Morack, John L and Erin C Pettit and Waddington, Edward D and Husmann, Eric}
}
@article {pettit2003effects,
	title = {Effects of basal sliding on isochrones and flow near an ice divide},
	journal = {Annals of Glaciology},
	volume = {37},
	number = {1},
	year = {2003},
	pages = {370{\textendash}376},
	publisher = {International Glaciological Society},
	author = {Erin C Pettit and Jacobson, H Paul and Waddington, Edwin D}
}
@article {pettit2003ice,
	title = {Ice flow at low deviatoric stress},
	journal = {Journal of Glaciology},
	volume = {49},
	number = {166},
	year = {2003},
	pages = {359{\textendash}369},
	publisher = {International Glaciological Society},
	author = {Erin C Pettit and Waddington, Edwin D}
}
@article {zumberge2002measurement,
	title = {Measurement of vertical strain and velocity at Siple Dome, Antarctica, with optical sensors},
	journal = {Journal of Glaciology},
	volume = {48},
	number = {161},
	year = {2002},
	pages = {217{\textendash}225},
	publisher = {International Glaciological Society},
	author = {Zumberge, Mark A and Elsberg, Daniel H and Harrison, William D and Husmann, Eric and Morack, John L and Erin C Pettit and Waddington, Edwin D}
}
@article {383,
	title = {Glaciers and Climate of the Upper Susitna Basin, Alaska},
	author = {Bliss, Andrew and Hock, Regine and Wolken, Gabriel and Whorton, Erin and Aubry-Wake, Caroline and Braun, Juliana and Gusmeroli, Alessio and Harrison, Will and Hoffman, Andrew and Liljedahl, Anna and others}
}
@article {156,
	title = {Hazard assessment of the Tidal Inlet landslide and potential subsequent tsunami, Glacier Bay National Park, Alaska},
	journal = {Landslides},
	volume = {4},
	pages = {205-215},
	abstract = {An unstable rock slump, estimated at 5 to 10\&$\#$8201;{\texttimes}\&$\#$8201;10<sup xmlns="http://pub2web.metastore.ingenta.com/ns/">6</sup> m<sup xmlns="http://pub2web.metastore.ingenta.com/ns/">3</sup>, lies perched above the northern shore of Tidal Inlet in Glacier Bay National Park, Alaska. This landslide mass has the potential to rapidly move into Tidal Inlet and generate large, long-period-impulse tsunami waves. Field and photographic examination revealed that the landslide moved between 1892 and 1919 after the retreat of the Little Ice Age glaciers from Tidal Inlet in 1890. Global positioning system measurements over a 2-year period show that the perched mass is presently moving at 3\&$\#$8211;4 cm annually indicating the landslide remains unstable. Numerical simulations of landslide-generated waves suggest that in the western arm of Glacier Bay, wave amplitudes would be greatest near the mouth of Tidal Inlet and slightly decrease with water depth according to Green\&$\#$8217;s law. As a function of time, wave amplitude would be greatest within approximately 40 min of the landslide entering water, with significant wave activity continuing for potentially several hours.},
	doi = {doi:10.1007/s10346-007-0084-1},
	url = {http://www.ingentaconnect.com/content/klu/10346/2007/00000004/00000003/00000084},
	author = {Wieczorek, Gerald and Geist, Eric and Roman J. Motyka and Jakob, Matthias}
}
