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pro vyhledávání: '"C. Rosie Williams"'
Autor:
Alexander T. Bradley, David T. Bett, Paul R. Holland, C. Rosie Williams, Robert J. Arthern, Jan De Rydt
Publikováno v:
Communications Earth & Environment, Vol 5, Iss 1, Pp 1-12 (2024)
Abstract The relative contributions of anthropogenic climate change and internal variability in sea level rise from the West Antarctic Ice Sheet are yet to be determined. Even the way to address this question is not yet clear, since these two are lin
Externí odkaz:
https://doaj.org/article/29e35d56250b45e09e541fd94b414b0e
Autor:
Alexander T. Bradley, David T. Bett, Paul R. Holland, C. Rosie Williams, Robert J. Arthern, Jan De Rydt
Publikováno v:
Communications Earth & Environment, Vol 5, Iss 1, Pp 1-1 (2024)
Externí odkaz:
https://doaj.org/article/61f04e9fd3c74cf39c7d0a295bfbf0f6
The West Antarctic Ice Sheet is thinning and losing mass at an accelerating rate. However these changes have yet to be formally attributed to anthropogenic climate change, primarily because of the potential for positive feedbacks on ice sheet mass lo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0913e6ba5823939dc22015fd8c8e2719
https://doi.org/10.5194/egusphere-egu23-8309
https://doi.org/10.5194/egusphere-egu23-8309
Publikováno v:
Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences. 478
Accurate predictions of basal melt rates on ice shelves are necessary for precise projections of the future behaviour of ice sheets. The computational expense associated with completely resolving the cavity circulation using an ocean model makes this
Autor:
C. Rosie Williams, Robert J. Arthern, Kelly A. Hogan, Andrew Smith, Alex Brisbourne, Tom A. Jordan
We consider a variety of ways that the basal drag that acts to resist the sliding of an ice sheet can be inferred from satellite observations, or from in situ observations. Three approaches are considered here. (1) use of inverse methods combined wit
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cce979e43f122bdf0acc4881c62defb6
https://doi.org/10.5194/egusphere-egu2020-10035
https://doi.org/10.5194/egusphere-egu2020-10035
Publikováno v:
Journal of Geophysical Research: Earth Surface. 120:1171-1188
Accurate dynamical models of the Antarctic ice sheet with carefully specified initial conditions and well-calibrated rheological parameters are needed to forecast global sea level. By adapting an inverse method previously used in electric impedance t
Autor:
C. Rosie Williams, Robert J. Arthern
We use an ice sheet model with realistic initial conditions to forecast how the Amundsen Sea sector of West Antarctica responds to recently observed rates of submarine melting. In these simulations, we isolate the effects of a positive feedback, driv
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ef703bd29fef8c047df861ddf6d093bb
Publikováno v:
Journal of Glaciology. 60:294-304
Inverse methods, where surface data are ‘inverted’ in order to quantify basal properties of ice sheets, play a major role in initializations. The balance-velocity method is a unique linear initialization, in which accumulation, surface elevation
Autor:
C. Rosie Williams, Martin A. Bees
Publikováno v:
The Journal of experimental biology. 214(Pt 14)
SUMMARYThe term bioconvection encapsulates the intricate patterns in concentration, due to hydrodynamic instabilities, that may arise in suspensions of non-neutrally buoyant, biased swimming microorganisms. The directional bias may be due to light (p
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