Roughness metrics of prismatic facets of ice. Issue 8 (30th April 2013)
- Record Type:
- Journal Article
- Title:
- Roughness metrics of prismatic facets of ice. Issue 8 (30th April 2013)
- Main Title:
- Roughness metrics of prismatic facets of ice
- Authors:
- Neshyba, S. P.
Lowen, B.
Benning, M.
Lawson, A.
Rowe, P. M. - Abstract:
- Abstract : [1] We define a surface normal roughness metric for mesoscopically rough ice facets and present methods for inferring its value from variable pressure scanning electron micrographs. The methods rely on the anisotropic morphology of roughening in the prismatic plane, in which nearly all the variation in surface height occurs in the direction of the main symmetry axis of hexagonal‐habit ice prisms. Because of this symmetry, roughening appears at boundaries between prismatic facets in a way that readily permits quantitative analysis. Prismatic surfaces of four ice crystals grown between −45 and −30°C are found to have mean surface normal roughness values of 0.04–0.1, a range that corresponds to Cox–Munk roughness scale parameters 0.3–0.5. The distribution of tilt angles also suggests a Weibull shape parameter smaller than unity, a result that compares favorably with field observations. Shortwave scattering calculations of hexagonal polyhedra with surface morphologies derived from these observations indicate substantial retention of the well‐known 22° halo, despite a large (4–6%) reduction in the asymmetry parameter compared to smooth‐surface counterparts. We argue that this signature is a generic outcome of the symmetry of the roughening, which in turn originates in the anisotropic surface self‐diffusivity of these facets. Key Points: Quantitative roughness information is derived from VPSEM observations. Roughness in VPSEM‐grown crystals is consistent with fieldAbstract : [1] We define a surface normal roughness metric for mesoscopically rough ice facets and present methods for inferring its value from variable pressure scanning electron micrographs. The methods rely on the anisotropic morphology of roughening in the prismatic plane, in which nearly all the variation in surface height occurs in the direction of the main symmetry axis of hexagonal‐habit ice prisms. Because of this symmetry, roughening appears at boundaries between prismatic facets in a way that readily permits quantitative analysis. Prismatic surfaces of four ice crystals grown between −45 and −30°C are found to have mean surface normal roughness values of 0.04–0.1, a range that corresponds to Cox–Munk roughness scale parameters 0.3–0.5. The distribution of tilt angles also suggests a Weibull shape parameter smaller than unity, a result that compares favorably with field observations. Shortwave scattering calculations of hexagonal polyhedra with surface morphologies derived from these observations indicate substantial retention of the well‐known 22° halo, despite a large (4–6%) reduction in the asymmetry parameter compared to smooth‐surface counterparts. We argue that this signature is a generic outcome of the symmetry of the roughening, which in turn originates in the anisotropic surface self‐diffusivity of these facets. Key Points: Quantitative roughness information is derived from VPSEM observations. Roughness in VPSEM‐grown crystals is consistent with field observations. Shortwave asymmetry parameter of 4‐6% relative to smooth‐surface counterparts … (more)
- Is Part Of:
- Journal of geophysical research. Volume 118:Issue 8(2013:Aug.)
- Journal:
- Journal of geophysical research
- Issue:
- Volume 118:Issue 8(2013:Aug.)
- Issue Display:
- Volume 118, Issue 8 (2013)
- Year:
- 2013
- Volume:
- 118
- Issue:
- 8
- Issue Sort Value:
- 2013-0118-0008-0000
- Page Start:
- 3309
- Page End:
- 3318
- Publication Date:
- 2013-04-30
- Subjects:
- ice -- cirrus -- mesoscopic -- roughness -- VPSEM -- prismatic
Atmospheric physics -- Periodicals
Geophysics -- Periodicals
551.5 - Journal URLs:
- http://onlinelibrary.wiley.com/journal/10.1002/(ISSN)2169-8996 ↗
http://www.agu.org/journals/jd/ ↗
http://onlinelibrary.wiley.com/ ↗ - DOI:
- 10.1002/jgrd.50357 ↗
- Languages:
- English
- ISSNs:
- 2169-897X
- Deposit Type:
- Legaldeposit
- View Content:
- Available online (eLD content is only available in our Reading Rooms) ↗
- Physical Locations:
- British Library DSC - 4995.001000
British Library DSC - BLDSS-3PM
British Library HMNTS - ELD Digital store - Ingest File:
- 360.xml