@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 {Das2014,
	title = {{21st-century increase in glacier mass loss in the Wrangell Mountains, Alaska, USA, from airborne laser altimetry and satellite stereo imagery}},
	journal = {J. Glaciol.},
	volume = {60},
	number = {220},
	year = {2014},
	pages = {283{\textendash}293},
	keywords = {glacier mass balance, ice and climate},
	issn = {00221430},
	doi = {10.3189/2014JoG13J119},
	url = {http://www.igsoc.org/journal/60/220/j13J119.html},
	author = {Das, Indrani and Hock, Regine and Berthier, Etienne and Lingle, Craig S.}
}
@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}
}
