Search Results - "Riverman, K. L."

Channelized Ice Melting in the Ocean Boundary Layer Beneath Pine Island Glacier, Antarctica by Stanton, T. P., Shaw, W. J., Truffer, M., Corr, H. F. J., Peters, L. E., Riverman, K. L., Bindschadler, R., Holland, D. M., Anandakrishnan, S.

“…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…”
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Initial results from geophysical surveys and shallow coring of the Northeast Greenland Ice Stream (NEGIS) by Vallelonga, P, Christianson, K, Alley, R. B, Anandakrishnan, S, Christian, J. E. M, Dahl-Jensen, D, Gkinis, V, Holme, C, Jacobel, R. W, Karlsson, N. B, Keisling, B. A, Kipfstuhl, S, Kjær, H. A, Kristensen, M. E. L, Muto, A, Peters, L. E, Popp, T, Riverman, K. L, Svensson, A. M, Tibuleac, C, Vinther, B. M, Weng, Y, Winstrup, M

“…The Northeast Greenland Ice Stream (NEGIS) is the sole interior Greenlandic ice stream. Fast flow initiates near the summit dome, and the ice stream terminates…”
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Heterogeneous melting near the Thwaites Glacier grounding line by Schmidt, B. E., Washam, P., Davis, P. E. D., Nicholls, K. W., Holland, D. M., Lawrence, J. D., Riverman, K. L., Smith, J. A., Spears, A., Dichek, D. J. G., Mullen, A. D., Clyne, E., Yeager, B., Anker, P., Meister, M. R., Hurwitz, B. C., Quartini, E. S., Bryson, F. E., Basinski-Ferris, A., Thomas, C., Wake, J., Vaughan, D. G., Anandakrishnan, S., Rignot, E., Paden, J., Makinson, K.

“…Thwaites Glacier represents 15% of the ice discharge from the West Antarctic Ice Sheet and influences a wider catchment 1 – 3 . Because it is grounded below…”
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Publisher Correction: Heterogeneous melting near the Thwaites Glacier grounding line by Schmidt, B. E., Washam, P., Davis, P. E. D., Nicholls, K. W., Holland, D. M., Lawrence, J. D., Riverman, K. L., Smith, J. A., Spears, A., Dichek, D. J. G., Mullen, A. D., Clyne, E., Yeager, B., Anker, P., Meister, M. R., Hurwitz, B. C., Quartini, E. S., Bryson, F. E., Basinski-Ferris, A., Thomas, C., Wake, J., Vaughan, D. G., Anandakrishnan, S., Rignot, E., Paden, J., Makinson, K.

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Enhanced Firn Densification in High‐Accumulation Shear Margins of the NE Greenland Ice Stream by Riverman, K. L., Alley, R. B., Christianson, K., Holschuh, N. D., Medley, B., Muto, A., Peters, L. E.

“…Firn thickness across the NE Greenland Ice Stream is a function of accumulated strain, with thinner firn in the high‐strain margins of the ice stream. We…”
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Suppressed basal melting in the eastern Thwaites Glacier grounding zone by Davis, Peter E. D., Nicholls, Keith W., Holland, David M., Schmidt, Britney E., Washam, Peter, Riverman, Kiya L., Arthern, Robert J., Vaňková, Irena, Eayrs, Clare, Smith, James A., Anker, Paul G. D., Mullen, Andrew D., Dichek, Daniel, Lawrence, Justin D., Meister, Matthew M., Clyne, Elisabeth, Basinski-Ferris, Aurora, Rignot, Eric, Queste, Bastien Y., Boehme, Lars, Heywood, Karen J., Anandakrishnan, Sridhar, Makinson, Keith

“…Thwaites Glacier is one of the fastest-changing ice–ocean systems in Antarctica 1 – 3 . Much of the ice sheet within the catchment of Thwaites Glacier is…”
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