Microwave penetration in polar snow and ice: Implications for GPR and SAR
The state of the continental ice masses has a direct impact on the global sea level. Changes in the polar regions will not only impact the people living in the Arctic, but also people living along coastlines around the world. Monitoring the current and future state of the global ice masses is theref...
Published in: | Annals of Glaciology |
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Format: | Doctoral or Postdoctoral Thesis |
Language: | English |
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2011
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Online Access: | http://hdl.handle.net/10852/12329 http://urn.nb.no/URN:NBN:no-29265 |
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ftoslouniv:oai:www.duo.uio.no:10852/12329 |
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Open Polar |
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Universitet i Oslo: Digitale utgivelser ved UiO (DUO) |
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English |
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VDP::450 Müller, Karsten Microwave penetration in polar snow and ice: Implications for GPR and SAR |
topic_facet |
VDP::450 |
description |
The state of the continental ice masses has a direct impact on the global sea level. Changes in the polar regions will not only impact the people living in the Arctic, but also people living along coastlines around the world. Monitoring the current and future state of the global ice masses is therefore of greatest interest. Microwave remote sensing of the cryosphere from ground, air or space is an active and fast developing field of research. In this thesis we investigate the interaction of microwaves with snow and ice by means of ground penetrating radar (GPR) and relate the findings to observations from space-borne radars (SAR or InSAR). We applied GPR to extend the 200 year mean surface mass balance (SMB) measurement from firn cores in a previously unmapped part of East Antarctica. Our findings show up to 50% lower values than estimated from modelling or remote sensing. However, our evaluated time period is much longer and our spatial resolution much finer. We relate our SMB values to radar backscatter from space-borne radar and use this correlation to further extend the SMB estimate over a 76000 km2 large area on the East Antarctic plateau. We investigate the position of the GPR phase center (zö) in snow, firn and ice in the interior and exterior of the East Antarctic Plateau and a glacier on Svalbard. Values of zö exceed 40 m in the dry firn of the East Antarctic Plateau at frequencies of 1.75 GHz. Thus, we have to expect a potential bias when measuring topography by means of InSAR in these areas. In coastal Antarctica and on an Arctic glacier zö often exceeds 5 m even at C-band. Consequently, deriving mass-balance estimates through monitoring elevation changes with radar are difficult to interpret. However, we find that zö aligns with the previous summer surface in the ablation zone of the glacier for S- and C-band frequencies. Thus, in this part of the glacier elevation changes can be monitored with InSAR. We attribute the difference in zö from the ablation zone to the firn zone of the glacier to a change in scattering mechanisms, which results in stronger radar backscatter from the firn zone. We use this difference to map the extent of the firn area by a simple threshold classification. |
author2 |
Svein-Erik Hamran, Jon-Ove Hagen |
format |
Doctoral or Postdoctoral Thesis |
author |
Müller, Karsten |
author_facet |
Müller, Karsten |
author_sort |
Müller, Karsten |
title |
Microwave penetration in polar snow and ice: Implications for GPR and SAR |
title_short |
Microwave penetration in polar snow and ice: Implications for GPR and SAR |
title_full |
Microwave penetration in polar snow and ice: Implications for GPR and SAR |
title_fullStr |
Microwave penetration in polar snow and ice: Implications for GPR and SAR |
title_full_unstemmed |
Microwave penetration in polar snow and ice: Implications for GPR and SAR |
title_sort |
microwave penetration in polar snow and ice: implications for gpr and sar |
publishDate |
2011 |
url |
http://hdl.handle.net/10852/12329 http://urn.nb.no/URN:NBN:no-29265 |
geographic |
Antarctic Arctic East Antarctica Svalbard |
geographic_facet |
Antarctic Arctic East Antarctica Svalbard |
genre |
Annals of Glaciology Antarc* Antarctic Antarctica Arctic East Antarctica glacier Svalbard |
genre_facet |
Annals of Glaciology Antarc* Antarctic Antarctica Arctic East Antarctica glacier Svalbard |
op_relation |
Paper I / Chapter 5 An 860-km surface mass balance profile on the East Antarctic Plateau derived by GPR. Karsten Müller, Anna Sinisalo, Helgard Ansch¨utz, Svein-Erik Hamran, Jon-Ove Hagen, Joseph R. McConnell, and Daniel R. Pasteris Annals of Glaciology, 51(55), 1-8. http://dx.doi.org/10.3189/172756410791392718 Paper II / Chapter 6 Phase-center of L-band radar in polar snow and ice. Karsten Müller, Svein-Erik Hamran, Anna Sinisalo, and Jon-Ove Hagen IEEE Transactions on Geoscience and Remote Sensing, Early Access 31 May 2011. (c) 2011 IEEE. Personal use of this material is permitted. http://dx.doi.org/10.1109/TGRS.2011.2140376 Paper III / Chapter 7 Change in microwave scattering mechanisms along Kongsvegen glacier, Svalbard and implications for SAR monitoring. Karsten Müller, Svein-Erik Hamran, Anna Sinisalo, and Jon-Ove Hagen In prep. The paper is removed from the thesis in DUO. http://dx.doi.org/10.3189/172756410791392718 http://dx.doi.org/10.1109/TGRS.2011.2140376 http://urn.nb.no/URN:NBN:no-29265 Müller, Karsten. Microwave penetration in polar snow and ice: Implications for GPR and SAR. Doktoravhandling, University of Oslo, 2011 http://hdl.handle.net/10852/12329 info:ofi/fmt:kev:mtx:ctx&ctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:dissertation&rft.au=Müller, Karsten&rft.title=Microwave penetration in polar snow and ice: Implications for GPR and SAR&rft.inst=University of Oslo&rft.date=2011&rft.degree=Doktoravhandling URN:NBN:no-29265 129655 120457598 Fulltext https://www.duo.uio.no/bitstream/handle/10852/12329/2/dravhandling-muller.pdf |
op_doi |
https://doi.org/10.3189/172756410791392718 https://doi.org/10.1109/TGRS.2011.2140376 |
container_title |
Annals of Glaciology |
container_volume |
51 |
container_issue |
55 |
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1 |
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8 |
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1766003408203939840 |
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ftoslouniv:oai:www.duo.uio.no:10852/12329 2023-05-15T13:29:49+02:00 Microwave penetration in polar snow and ice: Implications for GPR and SAR Müller, Karsten Svein-Erik Hamran, Jon-Ove Hagen 2011 http://hdl.handle.net/10852/12329 http://urn.nb.no/URN:NBN:no-29265 eng eng Paper I / Chapter 5 An 860-km surface mass balance profile on the East Antarctic Plateau derived by GPR. Karsten Müller, Anna Sinisalo, Helgard Ansch¨utz, Svein-Erik Hamran, Jon-Ove Hagen, Joseph R. McConnell, and Daniel R. Pasteris Annals of Glaciology, 51(55), 1-8. http://dx.doi.org/10.3189/172756410791392718 Paper II / Chapter 6 Phase-center of L-band radar in polar snow and ice. Karsten Müller, Svein-Erik Hamran, Anna Sinisalo, and Jon-Ove Hagen IEEE Transactions on Geoscience and Remote Sensing, Early Access 31 May 2011. (c) 2011 IEEE. Personal use of this material is permitted. http://dx.doi.org/10.1109/TGRS.2011.2140376 Paper III / Chapter 7 Change in microwave scattering mechanisms along Kongsvegen glacier, Svalbard and implications for SAR monitoring. Karsten Müller, Svein-Erik Hamran, Anna Sinisalo, and Jon-Ove Hagen In prep. The paper is removed from the thesis in DUO. http://dx.doi.org/10.3189/172756410791392718 http://dx.doi.org/10.1109/TGRS.2011.2140376 http://urn.nb.no/URN:NBN:no-29265 Müller, Karsten. Microwave penetration in polar snow and ice: Implications for GPR and SAR. Doktoravhandling, University of Oslo, 2011 http://hdl.handle.net/10852/12329 info:ofi/fmt:kev:mtx:ctx&ctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:dissertation&rft.au=Müller, Karsten&rft.title=Microwave penetration in polar snow and ice: Implications for GPR and SAR&rft.inst=University of Oslo&rft.date=2011&rft.degree=Doktoravhandling URN:NBN:no-29265 129655 120457598 Fulltext https://www.duo.uio.no/bitstream/handle/10852/12329/2/dravhandling-muller.pdf VDP::450 Doctoral thesis Doktoravhandling 2011 ftoslouniv https://doi.org/10.3189/172756410791392718 https://doi.org/10.1109/TGRS.2011.2140376 2020-06-21T08:42:08Z The state of the continental ice masses has a direct impact on the global sea level. Changes in the polar regions will not only impact the people living in the Arctic, but also people living along coastlines around the world. Monitoring the current and future state of the global ice masses is therefore of greatest interest. Microwave remote sensing of the cryosphere from ground, air or space is an active and fast developing field of research. In this thesis we investigate the interaction of microwaves with snow and ice by means of ground penetrating radar (GPR) and relate the findings to observations from space-borne radars (SAR or InSAR). We applied GPR to extend the 200 year mean surface mass balance (SMB) measurement from firn cores in a previously unmapped part of East Antarctica. Our findings show up to 50% lower values than estimated from modelling or remote sensing. However, our evaluated time period is much longer and our spatial resolution much finer. We relate our SMB values to radar backscatter from space-borne radar and use this correlation to further extend the SMB estimate over a 76000 km2 large area on the East Antarctic plateau. We investigate the position of the GPR phase center (zö) in snow, firn and ice in the interior and exterior of the East Antarctic Plateau and a glacier on Svalbard. Values of zö exceed 40 m in the dry firn of the East Antarctic Plateau at frequencies of 1.75 GHz. Thus, we have to expect a potential bias when measuring topography by means of InSAR in these areas. In coastal Antarctica and on an Arctic glacier zö often exceeds 5 m even at C-band. Consequently, deriving mass-balance estimates through monitoring elevation changes with radar are difficult to interpret. However, we find that zö aligns with the previous summer surface in the ablation zone of the glacier for S- and C-band frequencies. Thus, in this part of the glacier elevation changes can be monitored with InSAR. We attribute the difference in zö from the ablation zone to the firn zone of the glacier to a change in scattering mechanisms, which results in stronger radar backscatter from the firn zone. We use this difference to map the extent of the firn area by a simple threshold classification. Doctoral or Postdoctoral Thesis Annals of Glaciology Antarc* Antarctic Antarctica Arctic East Antarctica glacier Svalbard Universitet i Oslo: Digitale utgivelser ved UiO (DUO) Antarctic Arctic East Antarctica Svalbard Annals of Glaciology 51 55 1 8 |