Coherent backscatter enhancement in bistatic Ku- and X-band radar observations of dry snow
The coherent backscatter opposition effect (CBOE) enhances the backscatter intensity of electromagnetic waves by up to a factor of 2 in a very narrow cone around the direct return direction when multiple scattering occurs in a weakly absorbing, disordered medium. So far, this effect has not been inv...
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Copernicus Publications
2022
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Online Access: | https://doi.org/10.5194/tc-16-2859-2022 https://doaj.org/article/805bd9f821f04ae994283af7f8d99f85 |
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ftdoajarticles:oai:doaj.org/article:805bd9f821f04ae994283af7f8d99f85 2023-05-15T18:32:27+02:00 Coherent backscatter enhancement in bistatic Ku- and X-band radar observations of dry snow M. Stefko S. Leinss O. Frey I. Hajnsek 2022-07-01T00:00:00Z https://doi.org/10.5194/tc-16-2859-2022 https://doaj.org/article/805bd9f821f04ae994283af7f8d99f85 EN eng Copernicus Publications https://tc.copernicus.org/articles/16/2859/2022/tc-16-2859-2022.pdf https://doaj.org/toc/1994-0416 https://doaj.org/toc/1994-0424 doi:10.5194/tc-16-2859-2022 1994-0416 1994-0424 https://doaj.org/article/805bd9f821f04ae994283af7f8d99f85 The Cryosphere, Vol 16, Pp 2859-2879 (2022) Environmental sciences GE1-350 Geology QE1-996.5 article 2022 ftdoajarticles https://doi.org/10.5194/tc-16-2859-2022 2022-12-31T00:24:49Z The coherent backscatter opposition effect (CBOE) enhances the backscatter intensity of electromagnetic waves by up to a factor of 2 in a very narrow cone around the direct return direction when multiple scattering occurs in a weakly absorbing, disordered medium. So far, this effect has not been investigated in terrestrial snow in the microwave spectrum. It has also received little attention in scattering models. We present the first characterization of the CBOE in dry snow using ground-based and spaceborne bistatic radar systems. For a seasonal snowpack in the Ku-band (17.2 GHz), we found backscatter enhancement of 50 %–60 % ( +1.8 –2.0 dB) at a zero bistatic angle and a peak half-width at half-maximum (HWHM) of 0.25 ∘ . In the X-band (9.65 GHz), we found backscatter enhancement of at least 35 % ( +1.3 dB) and an estimated HWHM of 0.12 ∘ in the accumulation areas of glaciers in the Jungfrau–Aletsch region, Switzerland. Sampling of the peak shape at different bistatic angles allows estimating the scattering and absorption mean free paths, Λ T and Λ A . In the VV polarization, we obtained <math xmlns="http://www.w3.org/1998/Math/MathML" id="M7" display="inline" overflow="scroll" dspmath="mathml"><mrow><msub><mi mathvariant="normal">Λ</mi><mi mathvariant="normal">T</mi></msub><mo>=</mo><mn mathvariant="normal">0.4</mn><mo>±</mo><mn mathvariant="normal">0.1</mn></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="70pt" height="12pt" class="svg-formula" dspmath="mathimg" md5hash="12b3468f431a12d406d1166ba34a5406"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="tc-16-2859-2022-ie00001.svg" width="70pt" height="12pt" src="tc-16-2859-2022-ie00001.png"/></svg:svg> m and <math xmlns="http://www.w3.org/1998/Math/MathML" id="M8" display="inline" overflow="scroll" dspmath="mathml"><mrow><msub><mi mathvariant="normal">Λ</mi><mi ... Article in Journal/Newspaper The Cryosphere Directory of Open Access Journals: DOAJ Articles The Cryosphere 16 7 2859 2879 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Environmental sciences GE1-350 Geology QE1-996.5 |
spellingShingle |
Environmental sciences GE1-350 Geology QE1-996.5 M. Stefko S. Leinss O. Frey I. Hajnsek Coherent backscatter enhancement in bistatic Ku- and X-band radar observations of dry snow |
topic_facet |
Environmental sciences GE1-350 Geology QE1-996.5 |
description |
The coherent backscatter opposition effect (CBOE) enhances the backscatter intensity of electromagnetic waves by up to a factor of 2 in a very narrow cone around the direct return direction when multiple scattering occurs in a weakly absorbing, disordered medium. So far, this effect has not been investigated in terrestrial snow in the microwave spectrum. It has also received little attention in scattering models. We present the first characterization of the CBOE in dry snow using ground-based and spaceborne bistatic radar systems. For a seasonal snowpack in the Ku-band (17.2 GHz), we found backscatter enhancement of 50 %–60 % ( +1.8 –2.0 dB) at a zero bistatic angle and a peak half-width at half-maximum (HWHM) of 0.25 ∘ . In the X-band (9.65 GHz), we found backscatter enhancement of at least 35 % ( +1.3 dB) and an estimated HWHM of 0.12 ∘ in the accumulation areas of glaciers in the Jungfrau–Aletsch region, Switzerland. Sampling of the peak shape at different bistatic angles allows estimating the scattering and absorption mean free paths, Λ T and Λ A . In the VV polarization, we obtained <math xmlns="http://www.w3.org/1998/Math/MathML" id="M7" display="inline" overflow="scroll" dspmath="mathml"><mrow><msub><mi mathvariant="normal">Λ</mi><mi mathvariant="normal">T</mi></msub><mo>=</mo><mn mathvariant="normal">0.4</mn><mo>±</mo><mn mathvariant="normal">0.1</mn></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="70pt" height="12pt" class="svg-formula" dspmath="mathimg" md5hash="12b3468f431a12d406d1166ba34a5406"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="tc-16-2859-2022-ie00001.svg" width="70pt" height="12pt" src="tc-16-2859-2022-ie00001.png"/></svg:svg> m and <math xmlns="http://www.w3.org/1998/Math/MathML" id="M8" display="inline" overflow="scroll" dspmath="mathml"><mrow><msub><mi mathvariant="normal">Λ</mi><mi ... |
format |
Article in Journal/Newspaper |
author |
M. Stefko S. Leinss O. Frey I. Hajnsek |
author_facet |
M. Stefko S. Leinss O. Frey I. Hajnsek |
author_sort |
M. Stefko |
title |
Coherent backscatter enhancement in bistatic Ku- and X-band radar observations of dry snow |
title_short |
Coherent backscatter enhancement in bistatic Ku- and X-band radar observations of dry snow |
title_full |
Coherent backscatter enhancement in bistatic Ku- and X-band radar observations of dry snow |
title_fullStr |
Coherent backscatter enhancement in bistatic Ku- and X-band radar observations of dry snow |
title_full_unstemmed |
Coherent backscatter enhancement in bistatic Ku- and X-band radar observations of dry snow |
title_sort |
coherent backscatter enhancement in bistatic ku- and x-band radar observations of dry snow |
publisher |
Copernicus Publications |
publishDate |
2022 |
url |
https://doi.org/10.5194/tc-16-2859-2022 https://doaj.org/article/805bd9f821f04ae994283af7f8d99f85 |
genre |
The Cryosphere |
genre_facet |
The Cryosphere |
op_source |
The Cryosphere, Vol 16, Pp 2859-2879 (2022) |
op_relation |
https://tc.copernicus.org/articles/16/2859/2022/tc-16-2859-2022.pdf https://doaj.org/toc/1994-0416 https://doaj.org/toc/1994-0424 doi:10.5194/tc-16-2859-2022 1994-0416 1994-0424 https://doaj.org/article/805bd9f821f04ae994283af7f8d99f85 |
op_doi |
https://doi.org/10.5194/tc-16-2859-2022 |
container_title |
The Cryosphere |
container_volume |
16 |
container_issue |
7 |
container_start_page |
2859 |
op_container_end_page |
2879 |
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1766216575339200512 |