@article {334, title = {Spatio-temporal variations in seasonal ice tongue submarine melt rate at a tidewater glacier in southwest Greenland}, journal = {J. Glaciol.}, year = {2019}, pages = {1{\textendash}8}, keywords = {glacier calving, ice, ocean interactions, Remote sensing, subglacial processes}, doi = {10.1017/jog.2019.27}, author = {Moyer, A N and Nienow, P W and Gourmelen, N and Sole, A J and Truffer, M and Fahnestock, M and Slater, D A} } @article {351, title = {Dynamic jamming of iceberg-choked fjords}, journal = {Geophys. Res. Lett.}, volume = {42}, year = {2015}, pages = {1122{\textendash}1129}, keywords = {10.1002/2014GL062715 and glaciers, calving, icebergs, jamming}, issn = {00948276}, doi = {10.1002/2014GL062715}, author = {Peters, I and Amundson, J. M. and Cassotto, R and Fahnestock, M and Darnell, K and Truffer, M. and Zhang, W.} } @article {Fahnestock2001a, title = {{High geothermal heat flow, Basal melt, and the origin of rapid ice flow in central Greenland.}}, journal = {Science (New York, N.Y.)}, volume = {294}, number = {5550}, year = {2001}, month = {dec}, pages = {2338{\textendash}42}, abstract = {Age-depth relations from internal layering reveal a large region of rapid basal melting in Greenland. Melt is localized at the onset of rapid ice flow in the large ice stream that drains north off the summit dome and other areas in the northeast quadrant of the ice sheet. Locally, high melt rates indicate geothermal fluxes 15 to 30 times continental background. The southern limit of melt coincides with magnetic anomalies and topography that suggest a volcanic origin.}, issn = {0036-8075}, doi = {10.1126/science.1065370}, url = {http://www.ncbi.nlm.nih.gov/pubmed/11743197}, author = {Fahnestock, M and Abdalati, W and Joughin, Ian and Brozena, J and Gogineni, P} }