Found: 11
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Analysis of Snow Microstructure by Means of X-Ray Diffraction Contrast Tomography.
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- Advanced Engineering Materials, 2011, v. 13, n. 3, p. 128, doi. 10.1002/adem.201000221
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- Article
Unraveling the optical shape of snow.
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- Nature Communications, 2023, v. 14, n. 1, p. 1, doi. 10.1038/s41467-023-39671-3
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- Article
Effective coefficient of diffusion and permeability of firn at Dome C and Lock In, Antarctica, and of various snow types – estimates over the 100–850 kg m-3 density range.
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- Cryosphere, 2022, v. 16, n. 3, p. 967, doi. 10.5194/tc-16-967-2022
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- Article
Orientation selective grain sublimation–deposition in snow under temperature gradient metamorphism observed with diffraction contrast tomography.
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- Cryosphere, 2021, v. 15, n. 9, p. 4381, doi. 10.5194/tc-15-4381-2021
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- Article
Multiscale modeling of heat and mass transfer in dry snow: influence of the condensation coefficient and comparison with experiments.
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- Cryosphere Discussions, 2023, p. 1, doi. 10.5194/tc-2023-148
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- Article
Heterogeneous grain growth and vertical mass transfer within a snow layer under temperature gradient.
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- Cryosphere Discussions, 2023, p. 1, doi. 10.5194/tc-2022-255
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- Article
Effective coefficient of diffusion and permeability of firn at Dome C and Lock In, Antarctica - Estimates over the 100-850kgm<sup>-3</sup> density range.
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- Cryosphere Discussions, 2021, p. 1, doi. 10.5194/tc-2021-196
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- Article
Snow as a granular material: assessment of a new grain segmentation algorithm.
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- Granular Matter, 2014, v. 16, n. 4, p. 421, doi. 10.1007/s10035-014-0503-7
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- Article
Three-dimensional measurements of the deformation of snow induced by a cone penetration test.
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- Geophysical Research Abstracts, 2018, v. 20, p. 4746
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- Article
Orientation selective grain sublimation-deposition in snow under temperature gradient metamorphism observed with Diffraction Contrast Tomography.
- Published in:
- Cryosphere Discussions, 2021, p. 1, doi. 10.5194/tc-2021-22
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- Publication type:
- Article
Heterogeneous grain growth and vertical mass transfer within a snow layer under a temperature gradient.
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- Cryosphere, 2023, v. 17, n. 8, p. 3553, doi. 10.5194/tc-17-3553-2023
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- Article