Search Results - "W. H. Lipscomb"

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    Global glacier changes: a revised assessment of committed mass losses and sampling uncertainties by Mernild, S. H, Lipscomb, W. H, Bahr, D. B, Radić, V, Zemp, M

    Published in The cryosphere (02-10-2013)
    “…Most glaciers and ice caps (GIC) are out of balance with the current climate. To return to equilibrium, GIC must thin and retreat, losing additional mass and…”
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    Journal Article
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    Parameterization of basal friction near grounding lines in a one-dimensional ice sheet model by Leguy, G. R, Asay-Davis, X. S, Lipscomb, W. H

    Published in The cryosphere (18-07-2014)
    “…Ice sheets and ice shelves are linked by the transition zone, the region where flow dominated by vertical shear stress makes a transition to flow dominated by…”
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    Journal Article
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    A High‐End Estimate of Sea Level Rise for Practitioners by Wal, R. S. W., Nicholls, R. J., Behar, D., McInnes, K., Stammer, D., Lowe, J. A., Church, J. A., DeConto, R., Fettweis, X., Goelzer, H., Haasnoot, M., Haigh, I. D., Hinkel, J., Horton, B. P., James, T. S., Jenkins, A., LeCozannet, G., Levermann, A., Lipscomb, W. H., Marzeion, B., Pattyn, F., Payne, A. J., Pfeffer, W. T., Price, S. F., Seroussi, H., Sun, S., Veatch, W., White, K.

    Published in Earth's future (01-11-2022)
    “…Sea level rise (SLR) is a long‐lasting consequence of climate change because global anthropogenic warming takes centuries to millennia to equilibrate for the…”
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    A technique for generating consistent ice sheet initial conditions for coupled ice sheet/climate models by Fyke, J. G, Sacks, W. J, Lipscomb, W. H

    Published in Geoscientific model development (23-06-2014)
    “…A transient technique for generating ice sheet preindustrial initial conditions for long-term coupled ice sheet/climate model simulations is developed and…”
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    Evaluation of the sea ice simulation in a new coupled atmosphere-ocean climate model (HadGEM1) by McLaren, A. J., Banks, H. T., Durman, C. F., Gregory, J. M., Johns, T. C., Keen, A. B., Ridley, J. K., Roberts, M. J., Lipscomb, W. H., Connolley, W. M., Laxon, S. W.

    Published in Journal of Geophysical Research - Oceans (01-12-2006)
    “…A rapid increase in the variety, quality, and quantity of observations in polar regions is leading to a significant improvement in the understanding of sea ice…”
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    An energy-conserving thermodynamic model of sea ice by Bitz, C. M., Lipscomb, William H.

    “…We introduce an energy‐conserving sea ice model for climate study that accounts for the effect of internal brine‐pocket melting on surface ablation. Sea ice…”
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    Increasing mass loss from Greenland's Mittivakkat Gletscher by Mernild, S. H., Knudsen, N. T., Lipscomb, W. H., Yde, J. C., Malmros, J. K., Hasholt, B., Jakobsen, B. H.

    Published in The cryosphere (01-01-2011)
    “…Warming in the Arctic during the past several decades has caused glaciers to thin and retreat, and recent mass loss from the Greenland Ice Sheet is well…”
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    CO2 Increase Experiments Using the CESM: Relationship to Climate Sensitivity and Comparison of CESM1 to CESM2 by Bacmeister, J. T., Hannay, C., Medeiros, B., Gettelman, A., Neale, R., Fredriksen, H. B., Lipscomb, W. H., Simpson, I., Bailey, D. A., Holland, M., Lindsay, K., Otto‐Bliesner, B.

    “…We examine the response of the Community Earth System Model Versions 1 and 2 (CESM1 and CESM2) to abrupt quadrupling of atmospheric CO2 concentrations (4xCO2)…”
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    CO 2 Increase Experiments Using the CESM: Relationship to Climate Sensitivity and Comparison of CESM1 to CESM2 by Bacmeister, J. T., Hannay, C., Medeiros, B., Gettelman, A., Neale, R., Fredriksen, H. B., Lipscomb, W. H., Simpson, I., Bailey, D. A., Holland, M., Lindsay, K., Otto‐Bliesner, B.

    “…Abstract We examine the response of the Community Earth System Model Versions 1 and 2 (CESM1 and CESM2) to abrupt quadrupling of atmospheric CO 2…”
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    Remapping the thickness distribution in sea ice models by Lipscomb, William H.

    Published in Journal of Geophysical Research: Oceans (15-07-2001)
    “…In sea ice models with multiple thickness categories the ice thickness distribution evolves in time. The evolution of the thickness distribution as ice grows…”
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    A comparison of the stability and performance of depth-integrated ice-dynamics solvers by Robinson, Alexander, Goldberg, Daniel, Lipscomb, William H

    Published in The cryosphere (25-02-2022)
    “…In the last decade, the number of ice-sheet models has increased substantially, in line with the growth of the glaciological community. These models use…”
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    Evaluating different geothermal heat-flow maps as basal boundary conditions during spin-up of the Greenland ice sheet by Zhang, Tong, Colgan, William, Wansing, Agnes, Løkkegaard, Anja, Leguy, Gunter, Lipscomb, William H, Xiao, Cunde

    Published in The cryosphere (26-01-2024)
    “…There is currently poor scientific agreement on whether the ice–bed interface is frozen or thawed beneath approximately one third of the Greenland ice sheet…”
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    Statistical emulation of a perturbed basal melt ensemble of an ice sheet model to better quantify Antarctic sea level rise uncertainties by Berdahl, Mira, Leguy, Gunter, Lipscomb, William H, Urban, Nathan M

    Published in The cryosphere (15-06-2021)
    “…Antarctic ice shelves are vulnerable to warming ocean temperatures, and some have already begun thinning in response to increased basal melt rates. Sea level…”
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    Exploring ice sheet model sensitivity to ocean thermal forcing and basal sliding using the Community Ice Sheet Model (CISM) by Berdahl, Mira, Leguy, Gunter, Lipscomb, William H, Urban, Nathan M, Hoffman, Matthew J

    Published in The cryosphere (06-04-2023)
    “…Multi-meter sea level rise (SLR) is thought to be possible within the next few centuries, with most of the uncertainty originating from the Antarctic land ice…”
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    Marine ice sheet experiments with the Community Ice Sheet Model by Leguy, Gunter R, Lipscomb, William H, Asay-Davis, Xylar S

    Published in The cryosphere (14-07-2021)
    “…Ice sheet models differ in their numerical treatment of dynamical processes. Simulations of marine-based ice are sensitive to the choice of Stokes flow…”
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