Surface morphology and backscattering of ice-ridge sails in the Baltic Sea

Abstract The triangular shape of an ice-ridge sail in the Baltic Sea was studied statistically. The dimensions and orientation of individual ice blocks were measured in several ridges. All measurements were carried out from the standpoint of backscattering research. The results confirm that given ge...

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Published in:Journal of Glaciology
Main Author: Manninen, A. T.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1996
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000030604
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000030604
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spelling crcambridgeupr:10.1017/s0022143000030604 2024-06-23T07:54:15+00:00 Surface morphology and backscattering of ice-ridge sails in the Baltic Sea Manninen, A. T. 1996 http://dx.doi.org/10.1017/s0022143000030604 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000030604 en eng Cambridge University Press (CUP) Journal of Glaciology volume 42, issue 140, page 141-156 ISSN 0022-1430 1727-5652 journal-article 1996 crcambridgeupr https://doi.org/10.1017/s0022143000030604 2024-06-12T04:04:33Z Abstract The triangular shape of an ice-ridge sail in the Baltic Sea was studied statistically. The dimensions and orientation of individual ice blocks were measured in several ridges. All measurements were carried out from the standpoint of backscattering research. The results confirm that given geometrical properties of the two sides of ice ridges are in general not equal. A slight negative correlation was found between the slope angle and width of the sail. All three orientations and all three size parameters of ice blocks on both sides of the ridges studied can be considered as normally distributed. A log-normal distribution, however, fits slightly better the dimensions of the orientationally best rectangular approximations of the polygonal main facets of flat ice blocks. Three-dimensional modelling of ice ridges is essential, since the total side-facet area visible is typically at least as large as the total main-facet area. Calculated incidence-angle distrubutions show that the broad distributions of orientations and dimensions make different redges appear very similar on radar images. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 42 140 141 156
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description Abstract The triangular shape of an ice-ridge sail in the Baltic Sea was studied statistically. The dimensions and orientation of individual ice blocks were measured in several ridges. All measurements were carried out from the standpoint of backscattering research. The results confirm that given geometrical properties of the two sides of ice ridges are in general not equal. A slight negative correlation was found between the slope angle and width of the sail. All three orientations and all three size parameters of ice blocks on both sides of the ridges studied can be considered as normally distributed. A log-normal distribution, however, fits slightly better the dimensions of the orientationally best rectangular approximations of the polygonal main facets of flat ice blocks. Three-dimensional modelling of ice ridges is essential, since the total side-facet area visible is typically at least as large as the total main-facet area. Calculated incidence-angle distrubutions show that the broad distributions of orientations and dimensions make different redges appear very similar on radar images.
format Article in Journal/Newspaper
author Manninen, A. T.
spellingShingle Manninen, A. T.
Surface morphology and backscattering of ice-ridge sails in the Baltic Sea
author_facet Manninen, A. T.
author_sort Manninen, A. T.
title Surface morphology and backscattering of ice-ridge sails in the Baltic Sea
title_short Surface morphology and backscattering of ice-ridge sails in the Baltic Sea
title_full Surface morphology and backscattering of ice-ridge sails in the Baltic Sea
title_fullStr Surface morphology and backscattering of ice-ridge sails in the Baltic Sea
title_full_unstemmed Surface morphology and backscattering of ice-ridge sails in the Baltic Sea
title_sort surface morphology and backscattering of ice-ridge sails in the baltic sea
publisher Cambridge University Press (CUP)
publishDate 1996
url http://dx.doi.org/10.1017/s0022143000030604
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000030604
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 42, issue 140, page 141-156
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000030604
container_title Journal of Glaciology
container_volume 42
container_issue 140
container_start_page 141
op_container_end_page 156
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