An Improved Backscattering Theoretical Model for Snow Area
Remote sensing has been studied for a long timeto monitor the earth terrain. Remote sensing technology has been used globally in many different fields and one of the most popular area of study that usesremotesensing technology is snow monitoring.In previous researches, remote sensing has been modell...
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ftdoajarticles:oai:doaj.org/article:b632aaedb2ea4788b52742fa7e2fd706 2023-05-15T15:55:49+02:00 An Improved Backscattering Theoretical Model for Snow Area Dina Naqiba Nur Ezzaty Abd Wahid Syabeela Syahali Muhamad Jalaluddin Jamri 2021-12-01T00:00:00Z https://doi.org/10.33093/jetap.2021.3.2.2 https://doaj.org/article/b632aaedb2ea4788b52742fa7e2fd706 EN eng MMU Press https://journals.mmupress.com/index.php/jetap/article/view/241/275 https://doaj.org/toc/2682-8383 doi:10.33093/jetap.2021.3.2.2 2682-8383 https://doaj.org/article/b632aaedb2ea4788b52742fa7e2fd706 Journal of Engineering Technology and Applied Physics, Vol 3, Iss 2, Pp 7-13 (2021) surface volume scattering remote sensing theoretical modelling backscattering coefficient radiative tranfer equation Mechanics of engineering. Applied mechanics TA349-359 Technology T article 2021 ftdoajarticles https://doi.org/10.33093/jetap.2021.3.2.2 2023-03-26T01:34:23Z Remote sensing has been studied for a long timeto monitor the earth terrain. Remote sensing technology has been used globally in many different fields and one of the most popular area of study that usesremotesensing technology is snow monitoring.In previous researches, remote sensing has been modelled on snow area to study the scattering mechanisms of variousscattering processes. In this paper, surface volume second order term that was dropped inprevious studyis derived,included and studied to observe the improvement in thesurface volume backscattering coefficient. This new model isapplied on snow layer above ground and the snow layer is modelled as a volume of ice particles as the Mie scatterers that are closely packed and bounded by irregularboundaries.Various parameters are used to investigate the improvement of adding the new term. Results show improvementin cross-polarized return, for all the range of parameters studied.Comparison is made with the field measurement result from U.S. Army Cold Regions Research and Engineering Laboratory (CRREL) in 1990. Close agreement is shown between developed model and data field backscattering coefficient result. Article in Journal/Newspaper Cold Regions Research and Engineering Laboratory Directory of Open Access Journals: DOAJ Articles Journal of Engineering Technology and Applied Physics 3 2 7 13 |
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Open Polar |
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Directory of Open Access Journals: DOAJ Articles |
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ftdoajarticles |
language |
English |
topic |
surface volume scattering remote sensing theoretical modelling backscattering coefficient radiative tranfer equation Mechanics of engineering. Applied mechanics TA349-359 Technology T |
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surface volume scattering remote sensing theoretical modelling backscattering coefficient radiative tranfer equation Mechanics of engineering. Applied mechanics TA349-359 Technology T Dina Naqiba Nur Ezzaty Abd Wahid Syabeela Syahali Muhamad Jalaluddin Jamri An Improved Backscattering Theoretical Model for Snow Area |
topic_facet |
surface volume scattering remote sensing theoretical modelling backscattering coefficient radiative tranfer equation Mechanics of engineering. Applied mechanics TA349-359 Technology T |
description |
Remote sensing has been studied for a long timeto monitor the earth terrain. Remote sensing technology has been used globally in many different fields and one of the most popular area of study that usesremotesensing technology is snow monitoring.In previous researches, remote sensing has been modelled on snow area to study the scattering mechanisms of variousscattering processes. In this paper, surface volume second order term that was dropped inprevious studyis derived,included and studied to observe the improvement in thesurface volume backscattering coefficient. This new model isapplied on snow layer above ground and the snow layer is modelled as a volume of ice particles as the Mie scatterers that are closely packed and bounded by irregularboundaries.Various parameters are used to investigate the improvement of adding the new term. Results show improvementin cross-polarized return, for all the range of parameters studied.Comparison is made with the field measurement result from U.S. Army Cold Regions Research and Engineering Laboratory (CRREL) in 1990. Close agreement is shown between developed model and data field backscattering coefficient result. |
format |
Article in Journal/Newspaper |
author |
Dina Naqiba Nur Ezzaty Abd Wahid Syabeela Syahali Muhamad Jalaluddin Jamri |
author_facet |
Dina Naqiba Nur Ezzaty Abd Wahid Syabeela Syahali Muhamad Jalaluddin Jamri |
author_sort |
Dina Naqiba Nur Ezzaty Abd Wahid |
title |
An Improved Backscattering Theoretical Model for Snow Area |
title_short |
An Improved Backscattering Theoretical Model for Snow Area |
title_full |
An Improved Backscattering Theoretical Model for Snow Area |
title_fullStr |
An Improved Backscattering Theoretical Model for Snow Area |
title_full_unstemmed |
An Improved Backscattering Theoretical Model for Snow Area |
title_sort |
improved backscattering theoretical model for snow area |
publisher |
MMU Press |
publishDate |
2021 |
url |
https://doi.org/10.33093/jetap.2021.3.2.2 https://doaj.org/article/b632aaedb2ea4788b52742fa7e2fd706 |
genre |
Cold Regions Research and Engineering Laboratory |
genre_facet |
Cold Regions Research and Engineering Laboratory |
op_source |
Journal of Engineering Technology and Applied Physics, Vol 3, Iss 2, Pp 7-13 (2021) |
op_relation |
https://journals.mmupress.com/index.php/jetap/article/view/241/275 https://doaj.org/toc/2682-8383 doi:10.33093/jetap.2021.3.2.2 2682-8383 https://doaj.org/article/b632aaedb2ea4788b52742fa7e2fd706 |
op_doi |
https://doi.org/10.33093/jetap.2021.3.2.2 |
container_title |
Journal of Engineering Technology and Applied Physics |
container_volume |
3 |
container_issue |
2 |
container_start_page |
7 |
op_container_end_page |
13 |
_version_ |
1766391304158183424 |