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2“...<p>Calving is an important mechanism that controls the dynamics of marine terminating glaciers...”
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3by M. O'Regan, M. O'Regan, T. M. Cronin, B. Reilly, A. K. O. Alstrup, L. Gemery, A. Golub, L. A. Mayer, M. Morlighem, M. Moros, O. L. Munk, J. Nilsson, J. Nilsson, C. Pearce, H. Detlef, C. Stranne, C. Stranne, F. Vermassen, F. Vermassen, G. West, G. West, M. Jakobsson, M. Jakobsson“... to ice mass loss arising from increased glacier discharge in the coming decades. However, the past extent...”
Published 2021-08-01
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4by C. Zhao, C. Zhao, R. M. Gladstone, R. C. Warner, M. A. King, T. Zwinger, M. Morlighem“...<p>The Wordie Ice Shelf–Fleming Glacier system in the southern Antarctic Peninsula has experienced...”
Published 2018-08-01
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5by C. Zhao, C. Zhao, R. M. Gladstone, R. C. Warner, M. A. King, T. Zwinger, M. Morlighem“...<p>Many glaciers in the Antarctic Peninsula are now rapidly losing mass. Understanding...”
Published 2018-08-01
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6by H. Seroussi, M. Morlighem, E. Rignot, J. Mouginot, E. Larour, M. Schodlok, A. Khazendar“...Pine Island Glacier, a major contributor to sea level rise in West Antarctica, has been undergoing...”
Published 2014-09-01
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7“...Thwaites Glacier (TG), West Antarctica, has been losing mass and retreating rapidly in the past...”
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8by D. Farinotti, D. J. Brinkerhoff, G. K. C. Clarke, J. J. Fürst, H. Frey, P. Gantayat, F. Gillet-Chaulet, C. Girard, M. Huss, P. W. Leclercq, A. Linsbauer, H. Machguth, C. Martin, F. Maussion, M. Morlighem, C. Mosbeux, A. Pandit, A. Portmann, A. Rabatel, R. Ramsankaran, T. J. Reerink, O. Sanchez, P. A. Stentoft, S. Singh Kumari, W. J. J. van Pelt, B. Anderson, T. Benham, D. Binder, J. A. Dowdeswell, A. Fischer, K. Helfricht, S. Kutuzov, I. Lavrentiev, R. McNabb, G. H. Gudmundsson, H. Li, L. M. Andreassen“...Knowledge of the ice thickness distribution of glaciers and ice caps is an important prerequisite...”
Published 2017-04-01
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9by J. M. Lea, D. W. F. Mair, F. M. Nick, B. R. Rea, D. van As, M. Morlighem, P. W. Nienow, A. Weidick“...Many tidewater glaciers in Greenland are known to have undergone significant retreat during...”
Published 2014-11-01
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10“...<p>Thwaites Glacier (TG), West Antarctica, has experienced rapid, potentially irreversible...”
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11“...Understanding of long-term dynamics of glaciers and ice caps is vital to assess their recent...”
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12by M. Morlighem, M. Morlighem, M. Wood, H. Seroussi, Y. Choi, E. Rignot, E. Rignot“... retreat of marine-terminating glaciers may, for example, lead to a loss in resistive stress, which...”
Published 2019-03-01
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13by J. Schaffer, R. Timmermann, J. E. Arndt, S. S. Kristensen, C. Mayer, M. Morlighem, D. Steinhage“... by interacting with the ice shelves in Antarctica and with the marine-terminating outlet glaciers in Greenland...”
Published 2016-10-01
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14by J. H. Bondzio, H. Seroussi, M. Morlighem, T. Kleiner, M. Rückamp, A. Humbert, E. Y. Larour“... change in calving front position affects the entire stress regime of marine terminating glaciers...”
Published 2016-03-01
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15by D. A. Slater, D. Felikson, F. Straneo, H. Goelzer, H. Goelzer, C. M. Little, M. Morlighem, X. Fettweis, S. Nowicki“...” implementations. The retreat implementation parameterises glacier retreat as a function of projected subglacial...”
Published 2020-03-01
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16by K. Haubner, K. Haubner, J. E. Box, N. J. Schlegel, E. Y. Larour, M. Morlighem, A. M. Solgaard, K. K. Kjeldsen, K. K. Kjeldsen, K. K. Kjeldsen, S. H. Larsen, S. H. Larsen, E. Rignot, E. Rignot, T. K. Dupont, K. H. Kjær“...Tidewater glacier velocity and mass balance are known to be highly responsive to terminus position...”
Published 2018-04-01
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17“...<p>Subglacial hydrology has a strong influence on glacier and ice sheet dynamics, particularly...”
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18by L. A. Stevens, F. Straneo, S. B. Das, A. J. Plueddemann, A. L. Kukulya, M. Morlighem“... are lacking, due in large part to the difficulty in working at the margin of calving glaciers. Here we pair...”
Published 2016-02-01
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19“... to observed records of surface velocities on Upernavik Glacier, central West Greenland. We also provide...”
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20“...<p>Basal melting at the bottom of Antarctic ice shelves is a major control on glacier dynamics...”
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