OceanRep
Items where Author is "Ahlkrona, Josefin"
Number of items: 10.
Articles in a Scientific Journal - peer-reviewed
Ahlkrona, J. and Braack, M.
(2019)
Equal-Order Stabilized Finite Element Approximation of the p-Stokes Equations on Anisotropic Cartesian Meshes.
Computational Methods in Applied Mathematics
.
DOI 10.1515/cmam-2018-0260.
Helanow, C. and Ahlkrona, J.
(2018)
Stabilized equal low-order finite elements in ice sheet modeling – accuracy and robustness.
Computational Geosciences, 22
.
DOI 10.1007/s10596-017-9713-5.
Ahlkrona, J. and Shcherbakov, V.
(2017)
A meshfree approach to non-Newtonian free surface ice flow: Application to the Haut Glacier d'Arolla.
Journal of Computational Physics, 330
.
pp. 633-649.
DOI 10.1016/j.jcp.2016.10.045.
Ahlkrona, J., Lötstedt, P., Kirchner, N. and Zwinger, T.
(2016)
Dynamically coupling the non-linear Stokes equations with the shallow ice approximation in glaciology: Description and first applications of the ISCAL method.
Journal of Computational Physics, 308
.
pp. 1-19.
DOI 10.1016/j.jcp.2015.12.025.
Kirchner, N., Ahlkrona, J., Gowan, E. J., Lötstedt, P., Lea, J. M., Noormets, R., von Sydow, L., Dowdeswell, J. A. and Benham, T.
(2016)
Shallow ice approximation, second order shallow ice approximation, and full Stokes models: A discussion of their roles in palaeo-ice sheet modelling and development.
Quaternary Science Reviews, 147
.
pp. 136-147.
DOI 10.1016/j.quascirev.2016.01.032.
Ahlkrona, J., Kirchner, N. and Lotstedt, P.
(2013)
A numerical study of scaling relations for non-newtonian thin-film flows with applications in ice sheet modelling.
The Quarterly Journal of Mechanics and Applied Mathematics, 66
(4).
pp. 417-435.
DOI 10.1093/qjmam/hbt009.
Ahlkrona, J., Kirchner, N. and Lötstedt, P.
(2013)
Accuracy of the zeroth- and second-order shallow-ice approximation – numerical and theoretical results.
Geoscientific Model Development, 6
(6).
pp. 2135-2152.
DOI 10.5194/gmd-6-2135-2013.
Articles in a Scientific Journal - without review
Theses - not published by a publisher
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