Modeling of the L-Band emission and scattering of soil layers with consideration of Moisture and Temperature gradients.
International audience In the context of the European Space Agency's (ESA) Soil Moisture and Ocean Salinity (SMOS) mission, we present a study of the emission and of the bistatic scattering coefficient of rough surfaces at 1.4 GHz and the effects of moisture and temperature gradients. A new app...
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Language: | English |
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HAL CCSD
2012
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Online Access: | https://hal.science/hal-00985951 |
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ftunivnantes:oai:HAL:hal-00985951v1 |
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record_format |
openpolar |
institution |
Open Polar |
collection |
Université de Nantes: HAL-UNIV-NANTES |
op_collection_id |
ftunivnantes |
language |
English |
topic |
permittivity modeling temperature gradient moisture gradient remote sensing SMOS [SPI.ELEC]Engineering Sciences [physics]/Electromagnetism [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment [SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph] [PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph] [SDE.MCG]Environmental Sciences/Global Changes |
spellingShingle |
permittivity modeling temperature gradient moisture gradient remote sensing SMOS [SPI.ELEC]Engineering Sciences [physics]/Electromagnetism [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment [SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph] [PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph] [SDE.MCG]Environmental Sciences/Global Changes Demontoux, François Lawrence, Heather Wigneron, Jean Pierre Mironov, V. Kosolapova, L.G. Kerr, Yann H. Modeling of the L-Band emission and scattering of soil layers with consideration of Moisture and Temperature gradients. |
topic_facet |
permittivity modeling temperature gradient moisture gradient remote sensing SMOS [SPI.ELEC]Engineering Sciences [physics]/Electromagnetism [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment [SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph] [PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph] [SDE.MCG]Environmental Sciences/Global Changes |
description |
International audience In the context of the European Space Agency's (ESA) Soil Moisture and Ocean Salinity (SMOS) mission, we present a study of the emission and of the bistatic scattering coefficient of rough surfaces at 1.4 GHz and the effects of moisture and temperature gradients. A new approach for the calculation of rough surface scattering and emission at L-band has recently been. This approach relies on the use of ANSYS's numerical computation software HFSS (High Frequency Structure Simulator), which in turn solves Maxwell's equations using the Finite Element Method (FEM). The interest of this approach is that it can be extended to calculate the emission and scattering of complicated multilayer media, including features such as volume effects, gradients effects and inclusions, as well as rough surfaces. At L band, volume effects in the upper layer of soil should be taken into account. In particular, moisture or thermal phenomena lead to the presence of gradients. In this paper we present the work we have done to use FEM method to compute thermal effects and water infiltration effects in ground. Coupling electromagnetic and thermal computation we are able to study scattering of media such as permafrost or effects of rapid changes in temperature condition. We can also study the effect of moisture gradients or the impact of rainfall events on bistatic scattering coefficient or emissivity of soil. It can also be very useful for global observations with a frequent repeat coverage (future NASA Soil Moisture Active/Passive mission SMAP). In the present study we present the effects of water infiltration in ground (as moisture gradients) on the emissivity and bi-static scattering coefficient of soil. |
author2 |
Laboratoire de l'intégration, du matériau au système (IMS) Université Sciences et Technologies - Bordeaux 1 (UB)-Institut Polytechnique de Bordeaux-Centre National de la Recherche Scientifique (CNRS) Centre d'études spatiales de la biosphère (CESBIO) Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3) Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP) Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE) Écologie fonctionnelle et physique de l'environnement (EPHYSE) Institut National de la Recherche Agronomique (INRA) Kirensky Institute of Physics Russian Academy of Sciences Moscow (RAS) SMOS |
format |
Conference Object |
author |
Demontoux, François Lawrence, Heather Wigneron, Jean Pierre Mironov, V. Kosolapova, L.G. Kerr, Yann H. |
author_facet |
Demontoux, François Lawrence, Heather Wigneron, Jean Pierre Mironov, V. Kosolapova, L.G. Kerr, Yann H. |
author_sort |
Demontoux, François |
title |
Modeling of the L-Band emission and scattering of soil layers with consideration of Moisture and Temperature gradients. |
title_short |
Modeling of the L-Band emission and scattering of soil layers with consideration of Moisture and Temperature gradients. |
title_full |
Modeling of the L-Band emission and scattering of soil layers with consideration of Moisture and Temperature gradients. |
title_fullStr |
Modeling of the L-Band emission and scattering of soil layers with consideration of Moisture and Temperature gradients. |
title_full_unstemmed |
Modeling of the L-Band emission and scattering of soil layers with consideration of Moisture and Temperature gradients. |
title_sort |
modeling of the l-band emission and scattering of soil layers with consideration of moisture and temperature gradients. |
publisher |
HAL CCSD |
publishDate |
2012 |
url |
https://hal.science/hal-00985951 |
op_coverage |
Rome, Italy |
genre |
permafrost |
genre_facet |
permafrost |
op_source |
dans actes 12th Specialist Meeting on Microwave Radiometry and Remote Sensing of the Environmen 12th Specialist Meeting on Microwave Radiometry and Remote Sensing of the Environment https://hal.science/hal-00985951 12th Specialist Meeting on Microwave Radiometry and Remote Sensing of the Environment, Mar 2012, Rome, Italy. pp.1-10 |
op_relation |
hal-00985951 https://hal.science/hal-00985951 |
_version_ |
1766166846375985152 |
spelling |
ftunivnantes:oai:HAL:hal-00985951v1 2023-05-15T17:58:16+02:00 Modeling of the L-Band emission and scattering of soil layers with consideration of Moisture and Temperature gradients. Demontoux, François Lawrence, Heather Wigneron, Jean Pierre Mironov, V. Kosolapova, L.G. Kerr, Yann H. Laboratoire de l'intégration, du matériau au système (IMS) Université Sciences et Technologies - Bordeaux 1 (UB)-Institut Polytechnique de Bordeaux-Centre National de la Recherche Scientifique (CNRS) Centre d'études spatiales de la biosphère (CESBIO) Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3) Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP) Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE) Écologie fonctionnelle et physique de l'environnement (EPHYSE) Institut National de la Recherche Agronomique (INRA) Kirensky Institute of Physics Russian Academy of Sciences Moscow (RAS) SMOS Rome, Italy 2012-03-05 https://hal.science/hal-00985951 en eng HAL CCSD hal-00985951 https://hal.science/hal-00985951 dans actes 12th Specialist Meeting on Microwave Radiometry and Remote Sensing of the Environmen 12th Specialist Meeting on Microwave Radiometry and Remote Sensing of the Environment https://hal.science/hal-00985951 12th Specialist Meeting on Microwave Radiometry and Remote Sensing of the Environment, Mar 2012, Rome, Italy. pp.1-10 permittivity modeling temperature gradient moisture gradient remote sensing SMOS [SPI.ELEC]Engineering Sciences [physics]/Electromagnetism [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment [SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph] [PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph] [SDE.MCG]Environmental Sciences/Global Changes info:eu-repo/semantics/conferenceObject Conference papers 2012 ftunivnantes 2023-02-21T23:43:37Z International audience In the context of the European Space Agency's (ESA) Soil Moisture and Ocean Salinity (SMOS) mission, we present a study of the emission and of the bistatic scattering coefficient of rough surfaces at 1.4 GHz and the effects of moisture and temperature gradients. A new approach for the calculation of rough surface scattering and emission at L-band has recently been. This approach relies on the use of ANSYS's numerical computation software HFSS (High Frequency Structure Simulator), which in turn solves Maxwell's equations using the Finite Element Method (FEM). The interest of this approach is that it can be extended to calculate the emission and scattering of complicated multilayer media, including features such as volume effects, gradients effects and inclusions, as well as rough surfaces. At L band, volume effects in the upper layer of soil should be taken into account. In particular, moisture or thermal phenomena lead to the presence of gradients. In this paper we present the work we have done to use FEM method to compute thermal effects and water infiltration effects in ground. Coupling electromagnetic and thermal computation we are able to study scattering of media such as permafrost or effects of rapid changes in temperature condition. We can also study the effect of moisture gradients or the impact of rainfall events on bistatic scattering coefficient or emissivity of soil. It can also be very useful for global observations with a frequent repeat coverage (future NASA Soil Moisture Active/Passive mission SMAP). In the present study we present the effects of water infiltration in ground (as moisture gradients) on the emissivity and bi-static scattering coefficient of soil. Conference Object permafrost Université de Nantes: HAL-UNIV-NANTES |