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The Nonlinear and Distinct Responses of Ocean Heat Content and Anthropogenic Carbon to Ice Sheet Freshwater Discharge in a Warming Climate. [PDF]
Earths FutureGorte T +4 more
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Annual Reports to the ESA Council ESA 110th Annual Meeting July, 2025
The Bulletin of the Ecological Society of America, EarlyView.
wiley +1 more source
Modelling transparent ice-sheet response to climate with a coupled 3D ice-sheet-earth model
, 1996 R. Greve, D. Wolf, Volker Klemann
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Science, 2012
Full-stress flow models for ice sheets promise improved projections of sea-level change.
Richard B. Alley, Ian Joughin
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Full-stress flow models for ice sheets promise improved projections of sea-level change.
Richard B. Alley, Ian Joughin
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1984
It is only in exceptional cases that the shape of an ice sheet can be calculated by analytical methods. Some examples of situations in which this is possible will be discussed in chapter 6. In most cases numerical methods have to be used, particularly when we are not only interested in steady states, but also want to compute the transient behaviour of ...
J. Oerlemans, C. J. van der Veen
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It is only in exceptional cases that the shape of an ice sheet can be calculated by analytical methods. Some examples of situations in which this is possible will be discussed in chapter 6. In most cases numerical methods have to be used, particularly when we are not only interested in steady states, but also want to compute the transient behaviour of ...
J. Oerlemans, C. J. van der Veen
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Geophysical & Astrophysical Fluid Dynamics, 1992
This paper surveys the problem of modelling the dynamics of large ice sheets. A simplified model for two-dimensional plane ice sheets is derived, and both isothermal and non-isothermal cases are co...
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This paper surveys the problem of modelling the dynamics of large ice sheets. A simplified model for two-dimensional plane ice sheets is derived, and both isothermal and non-isothermal cases are co...
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Antarctic ice-sheet hysteresis in a three-dimensional hybrid ice-sheet model
2020<p>Ice sheets, in particular the Antarctic Ice Sheet (AIS), are considered as potential tipping elements (TEs) of the Earth system. The mechanism underlying tipping is the existence of positive feedbacks leading to self-amplification processes that, once triggered, dominate the dynamics of the system.
Marisa Montoya +5 more
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2023
Glacier mass loss related to ice flow is a quantitative factor that controls sea level rise and global warming. Ice flow is attributed to the complicated interaction between grounding line migration, calving basal friction, and topography. Previous studies using massive geophysical observation, including IPR (Ice Penetrating Radar), InSAR ...
Yi-Jeong Baek, Byung-Dal So
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Glacier mass loss related to ice flow is a quantitative factor that controls sea level rise and global warming. Ice flow is attributed to the complicated interaction between grounding line migration, calving basal friction, and topography. Previous studies using massive geophysical observation, including IPR (Ice Penetrating Radar), InSAR ...
Yi-Jeong Baek, Byung-Dal So
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Historic simulations of the Antarctic Ice Sheet with the Parallel Ice Sheet Model
2021<p>Large uncertainties in Antarctic sea level projections are related to ocean-driven melting (Seroussi et al., 2020; Jourdain et al., 2020; Reese et al., 2020; Edwards et al., in press) and the marine ice sheet instability (Robel et al., 2019).
Ronja Reese +4 more
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