SEA ICE RADAR ALTIMETER SIGNATURE MODELLING EXPERIMENTS
Scattering at the large horizontal dielectric contrasts of the snow/sea ice system i.e. the snow and ice surface dominate the altimeter total backscatter coefficient. To investigate the temporal and seasonal altimeter backscatter signature variability a forward model is coupled to a thermodynamic an...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.535.2169 2023-05-15T18:16:33+02:00 SEA ICE RADAR ALTIMETER SIGNATURE MODELLING EXPERIMENTS Rasmus Tonboe Søren Andersen Leif Toudal Pedersen The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.535.2169 http://ocean.dmi.dk/staff/rtt/sea_ice_model.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.535.2169 http://ocean.dmi.dk/staff/rtt/sea_ice_model.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://ocean.dmi.dk/staff/rtt/sea_ice_model.pdf text ftciteseerx 2016-01-08T10:47:13Z Scattering at the large horizontal dielectric contrasts of the snow/sea ice system i.e. the snow and ice surface dominate the altimeter total backscatter coefficient. To investigate the temporal and seasonal altimeter backscatter signature variability a forward model is coupled to a thermodynamic and mass model for the snow and sea-ice temperature profile, accumulation, growth, melt and metamorphosis. The thermodynamic and mass model uses an initial snow and ice profile and meteorological data input. In situ data collected during the 2003 CRYOVEX joint Danish-German-ESA campaign and the 2004 GreenIce ice camp are used. Our results show that the snow cover is not only important for the microwave signature of sea ice but also the buoyant balance of ice floes as well as the heat-budget. These considerations are included in the discussion. 1 Text Sea ice Unknown |
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ftciteseerx |
language |
English |
description |
Scattering at the large horizontal dielectric contrasts of the snow/sea ice system i.e. the snow and ice surface dominate the altimeter total backscatter coefficient. To investigate the temporal and seasonal altimeter backscatter signature variability a forward model is coupled to a thermodynamic and mass model for the snow and sea-ice temperature profile, accumulation, growth, melt and metamorphosis. The thermodynamic and mass model uses an initial snow and ice profile and meteorological data input. In situ data collected during the 2003 CRYOVEX joint Danish-German-ESA campaign and the 2004 GreenIce ice camp are used. Our results show that the snow cover is not only important for the microwave signature of sea ice but also the buoyant balance of ice floes as well as the heat-budget. These considerations are included in the discussion. 1 |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Rasmus Tonboe Søren Andersen Leif Toudal Pedersen |
spellingShingle |
Rasmus Tonboe Søren Andersen Leif Toudal Pedersen SEA ICE RADAR ALTIMETER SIGNATURE MODELLING EXPERIMENTS |
author_facet |
Rasmus Tonboe Søren Andersen Leif Toudal Pedersen |
author_sort |
Rasmus Tonboe |
title |
SEA ICE RADAR ALTIMETER SIGNATURE MODELLING EXPERIMENTS |
title_short |
SEA ICE RADAR ALTIMETER SIGNATURE MODELLING EXPERIMENTS |
title_full |
SEA ICE RADAR ALTIMETER SIGNATURE MODELLING EXPERIMENTS |
title_fullStr |
SEA ICE RADAR ALTIMETER SIGNATURE MODELLING EXPERIMENTS |
title_full_unstemmed |
SEA ICE RADAR ALTIMETER SIGNATURE MODELLING EXPERIMENTS |
title_sort |
sea ice radar altimeter signature modelling experiments |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.535.2169 http://ocean.dmi.dk/staff/rtt/sea_ice_model.pdf |
genre |
Sea ice |
genre_facet |
Sea ice |
op_source |
http://ocean.dmi.dk/staff/rtt/sea_ice_model.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.535.2169 http://ocean.dmi.dk/staff/rtt/sea_ice_model.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766190228382416896 |