Electromagnetic Modelling for the Active and Passive Remote Sensing of Polar Ice Sheet and Signal of Opportunity (SoOp) Land Observation
Climate has been changing dramatically over the past several decades. Terrestrial snow and polar ice sheets have been studied intensively as indicators of climate change. The following research supports two major objectives. The first objective is to use a new microwave remote sensing technique, P-b...
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ftumdeepblue:oai:deepblue.lib.umich.edu:2027.42/193383 2024-09-09T19:45:18+00:00 Electromagnetic Modelling for the Active and Passive Remote Sensing of Polar Ice Sheet and Signal of Opportunity (SoOp) Land Observation Xu, Haokui Tsang, Leung Ruf, Christopher S Eid, Aline Mortazawi, Amir Ann Arbor 2024 application/pdf https://hdl.handle.net/2027.42/193383 https://doi.org/10.7302/23028 en_US eng https://hdl.handle.net/2027.42/193383 https://dx.doi.org/10.7302/23028 orcid:0000-0002-5924-8903 Xu, Haokui; 0000-0002-5924-8903 Micorwave remote sensing Electrical Engineering Engineering Thesis 2024 ftumdeepblue https://doi.org/10.7302/23028 2024-06-19T00:03:08Z Climate has been changing dramatically over the past several decades. Terrestrial snow and polar ice sheets have been studied intensively as indicators of climate change. The following research supports two major objectives. The first objective is to use a new microwave remote sensing technique, P-band GNSS-SAR interferometry, to characterize the Snow Water Equivalent of Terrestrial. The second objective is to assist in estimating polar ice sheet mass balance using active and passive microwave remote sensing data. To support the GNSS-SAR remote sensing of terrestrial snow, my research focused on simulating the P-band near specular bistatic scattering coefficients of mountainous areas. Given that reliable measurement of the near specular scattering coefficients of land surface in the P-band Signal of Opportunity concept will only be available in the future, simulation work is currently the only way to understand the near specular bistatic scattering in the P-band. The bistatic scattering coefficient of variance fields, denoted by γ_v, is calculated at various scattering azimuth angles. Simulations using AKS show that the γ_v can exceed 10 dB across a range of azimuth angles, ϕ_s. The values are much larger than those of radar backscattering, suggesting potential support for employing a Synthetic Aperture Radar (SAR) concept based on Signals of Opportunity, particularly with data acquisition near the forward direction. The much stronger surface scattering ability loosens the requirements of receiving antenna gain. Large swath sensing of terrestrial snow is thus possible. Two subtopics are covered in my research to support the mass balance study. The first subtopic involved the density variation properties in the dry zone, while the second subtopic focused on the modeling work for the perennial firn aquifer. Fluctuation of firn density near the surface is a major uncertainty in characterizing mass balance. Previous research has shown that firn density profiles can be represented using three processes: “long” and ... Thesis Ice Sheet University of Michigan: Deep Blue Aks ENVELOPE(9.657,9.657,63.721,63.721) |
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University of Michigan: Deep Blue |
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ftumdeepblue |
language |
English |
topic |
Micorwave remote sensing Electrical Engineering Engineering |
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Micorwave remote sensing Electrical Engineering Engineering Xu, Haokui Electromagnetic Modelling for the Active and Passive Remote Sensing of Polar Ice Sheet and Signal of Opportunity (SoOp) Land Observation |
topic_facet |
Micorwave remote sensing Electrical Engineering Engineering |
description |
Climate has been changing dramatically over the past several decades. Terrestrial snow and polar ice sheets have been studied intensively as indicators of climate change. The following research supports two major objectives. The first objective is to use a new microwave remote sensing technique, P-band GNSS-SAR interferometry, to characterize the Snow Water Equivalent of Terrestrial. The second objective is to assist in estimating polar ice sheet mass balance using active and passive microwave remote sensing data. To support the GNSS-SAR remote sensing of terrestrial snow, my research focused on simulating the P-band near specular bistatic scattering coefficients of mountainous areas. Given that reliable measurement of the near specular scattering coefficients of land surface in the P-band Signal of Opportunity concept will only be available in the future, simulation work is currently the only way to understand the near specular bistatic scattering in the P-band. The bistatic scattering coefficient of variance fields, denoted by γ_v, is calculated at various scattering azimuth angles. Simulations using AKS show that the γ_v can exceed 10 dB across a range of azimuth angles, ϕ_s. The values are much larger than those of radar backscattering, suggesting potential support for employing a Synthetic Aperture Radar (SAR) concept based on Signals of Opportunity, particularly with data acquisition near the forward direction. The much stronger surface scattering ability loosens the requirements of receiving antenna gain. Large swath sensing of terrestrial snow is thus possible. Two subtopics are covered in my research to support the mass balance study. The first subtopic involved the density variation properties in the dry zone, while the second subtopic focused on the modeling work for the perennial firn aquifer. Fluctuation of firn density near the surface is a major uncertainty in characterizing mass balance. Previous research has shown that firn density profiles can be represented using three processes: “long” and ... |
author2 |
Tsang, Leung Ruf, Christopher S Eid, Aline Mortazawi, Amir Ann Arbor |
format |
Thesis |
author |
Xu, Haokui |
author_facet |
Xu, Haokui |
author_sort |
Xu, Haokui |
title |
Electromagnetic Modelling for the Active and Passive Remote Sensing of Polar Ice Sheet and Signal of Opportunity (SoOp) Land Observation |
title_short |
Electromagnetic Modelling for the Active and Passive Remote Sensing of Polar Ice Sheet and Signal of Opportunity (SoOp) Land Observation |
title_full |
Electromagnetic Modelling for the Active and Passive Remote Sensing of Polar Ice Sheet and Signal of Opportunity (SoOp) Land Observation |
title_fullStr |
Electromagnetic Modelling for the Active and Passive Remote Sensing of Polar Ice Sheet and Signal of Opportunity (SoOp) Land Observation |
title_full_unstemmed |
Electromagnetic Modelling for the Active and Passive Remote Sensing of Polar Ice Sheet and Signal of Opportunity (SoOp) Land Observation |
title_sort |
electromagnetic modelling for the active and passive remote sensing of polar ice sheet and signal of opportunity (soop) land observation |
publishDate |
2024 |
url |
https://hdl.handle.net/2027.42/193383 https://doi.org/10.7302/23028 |
long_lat |
ENVELOPE(9.657,9.657,63.721,63.721) |
geographic |
Aks |
geographic_facet |
Aks |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_relation |
https://hdl.handle.net/2027.42/193383 https://dx.doi.org/10.7302/23028 orcid:0000-0002-5924-8903 Xu, Haokui; 0000-0002-5924-8903 |
op_doi |
https://doi.org/10.7302/23028 |
_version_ |
1809914914652815360 |