On the estimation of physical roughness of a marginal sea ice zone using remote sensing

This thesis provides insight into techniques for the detection and classification of various marginal ice zone roughnesses in the southern Beaufort Sea using in situ and satellite-based microwave remote sensing. A proposed model of surface roughness shows the dependence of circular coherence, a disc...

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Main Author: Gupta, Mukesh
Other Authors: Barber, David (Environment and Geography)
Published: John Wiley and Sons, Ltd. 2014
Subjects:
Online Access:http://hdl.handle.net/1993/23836
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spelling ndltd-MANITOBA-oai-mspace.lib.umanitoba.ca-1993-238362014-10-22T03:53:07Z On the estimation of physical roughness of a marginal sea ice zone using remote sensing Gupta, Mukesh Barber, David (Environment and Geography) Doering, Jay (Civil Engineering) Ehn, Jens (Environment and Geography) Papakyriakou, Tim (Environment and Geography) Bernier, Monique (Institut National de la Recherche Scientifique) Arctic surface roughness marginal ice zone sea ice polarimetry passive microwave active microwave remote sensing This thesis provides insight into techniques for the detection and classification of various marginal ice zone roughnesses in the southern Beaufort Sea using in situ and satellite-based microwave remote sensing. A proposed model of surface roughness shows the dependence of circular coherence, a discriminator of roughness, on the roughness and dielectrics. A relationship between ice slopes in azimuth and range direction is derived. Microwave brightness temperature of open water is significantly correlated with wave height but not with the wind speed, having the strongest correlations for the H-polarization at both 37 and 89 GHz. A modified formula for the relationship between non-dimensional form of energy and wave age at wind speeds 0−10 m/s is obtained. The brightness temperature (April−June) of sea ice at H-polarization of 89 GHz is found to decrease with increasing roughness, and is attributed to the dominant contributions from rapidly varying thermodynamic properties of snow-covered sea ice. 2014-08-20T17:18:25Z 2014-08-20T17:18:25Z 2014-01-30 2013-04-26 2014-03-10 Gupta, M., Barber, D. G., Scharien, R. K., and Isleifson, D. (2014). Detection and classification of surface roughness in an Arctic marginal sea ice zone. Hydrological Processes, 28, 599−609, doi:10.1002/hyp.9593 Gupta, M., Scharien, R. K., and Barber, D. G. (2013). C-band polarimetric coherences and ratios for discriminating sea ice roughness. International Journal of Oceanography, 2013, Article ID 567182, 1−13, doi:10.1155/2013/567182 Gupta, M., Scharien, R. K., and Barber, D. G. (2014). Microwave emission and scattering from ocean surface waves in the southern Beaufort Sea. International Journal of Oceanography, 2014, Article ID 872342, 1−12, doi:10.1155/2014/872342 http://hdl.handle.net/1993/23836 John Wiley and Sons, Ltd. Hindawi Publishing Corporation Hindawi Publishing Corporation
collection NDLTD
sources NDLTD
topic Arctic
surface roughness
marginal ice zone
sea ice
polarimetry
passive microwave
active microwave
remote sensing
spellingShingle Arctic
surface roughness
marginal ice zone
sea ice
polarimetry
passive microwave
active microwave
remote sensing
Gupta, Mukesh
On the estimation of physical roughness of a marginal sea ice zone using remote sensing
description This thesis provides insight into techniques for the detection and classification of various marginal ice zone roughnesses in the southern Beaufort Sea using in situ and satellite-based microwave remote sensing. A proposed model of surface roughness shows the dependence of circular coherence, a discriminator of roughness, on the roughness and dielectrics. A relationship between ice slopes in azimuth and range direction is derived. Microwave brightness temperature of open water is significantly correlated with wave height but not with the wind speed, having the strongest correlations for the H-polarization at both 37 and 89 GHz. A modified formula for the relationship between non-dimensional form of energy and wave age at wind speeds 0−10 m/s is obtained. The brightness temperature (April−June) of sea ice at H-polarization of 89 GHz is found to decrease with increasing roughness, and is attributed to the dominant contributions from rapidly varying thermodynamic properties of snow-covered sea ice.
author2 Barber, David (Environment and Geography)
author_facet Barber, David (Environment and Geography)
Gupta, Mukesh
author Gupta, Mukesh
author_sort Gupta, Mukesh
title On the estimation of physical roughness of a marginal sea ice zone using remote sensing
title_short On the estimation of physical roughness of a marginal sea ice zone using remote sensing
title_full On the estimation of physical roughness of a marginal sea ice zone using remote sensing
title_fullStr On the estimation of physical roughness of a marginal sea ice zone using remote sensing
title_full_unstemmed On the estimation of physical roughness of a marginal sea ice zone using remote sensing
title_sort on the estimation of physical roughness of a marginal sea ice zone using remote sensing
publisher John Wiley and Sons, Ltd.
publishDate 2014
url http://hdl.handle.net/1993/23836
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