Snow stratigraphy observations from Operation IceBridge surveys in Alaska using S and C band airborne ultra-wideband FMCW (frequency-modulated continuous wave) radar
<p>During the concluding phase of the NASA Operation IceBridge (OIB), we successfully completed two airborne measurement campaigns (in 2018 and 2021, respectively) using a compact S and C band radar installed on a Single Otter aircraft and collected data over Alaskan mountains, ice fields, and...
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| Format: | Article |
| Language: | English |
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Copernicus Publications
2023-01-01
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| Series: | The Cryosphere |
| Online Access: | https://tc.copernicus.org/articles/17/175/2023/tc-17-175-2023.pdf |
| _version_ | 1797952015259664384 |
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| author | J. Li F. Rodriguez-Morales X. Fettweis O. Ibikunle C. Leuschen J. Paden D. Gomez-Garcia E. Arnold |
| author_facet | J. Li F. Rodriguez-Morales X. Fettweis O. Ibikunle C. Leuschen J. Paden D. Gomez-Garcia E. Arnold |
| author_sort | J. Li |
| collection | DOAJ |
| description | <p>During the concluding phase of the NASA Operation
IceBridge (OIB), we successfully completed two airborne measurement
campaigns (in 2018 and 2021, respectively) using a compact S and C band radar
installed on a Single Otter aircraft and collected data over Alaskan
mountains, ice fields, and glaciers. This paper reports seasonal snow depths
derived from radar data. We found large variations in seasonal
radar-inferred depths with multi-modal distributions assuming a constant
relative permittivity for snow equal to 1.89. About 34 % of the snow
depths observed in 2018 were between 3.2 and 4.2 m, and close to 30 % of the
snow depths observed in 2021 were between 2.5 and 3.5 m. We observed snow
strata in ice facies, combined percolation and wet-snow facies, and dry-snow facies from
radar data and identified the transition areas from wet-snow facies to ice
facies for multiple glaciers based on the snow strata and radar
backscattering characteristics. Our analysis focuses on the measured strata
of multiple years at the caldera of Mount Wrangell (K'elt'aeni) to estimate the local
snow accumulation rate. We developed a method for using our radar readings
of multi-year strata to constrain the uncertain parameters of interpretation
models with the assumption that most of the snow layers detected by the
radar at the caldera are annual accumulation layers. At a 2004 ice core and
2005 temperature sensor tower site, the locally estimated average snow
accumulation rate is <span class="inline-formula">∼2.89</span> m w.e. a<span class="inline-formula"><sup>−1</sup></span> between the years
2003 and 2021. Our estimate of the snow accumulation rate between 2005 and
2006 is 2.82 m w.e. a<span class="inline-formula"><sup>−1</sup></span>, which matches closely to the 2.75 m w.e. a<span class="inline-formula"><sup>−1</sup></span> inferred from independent ground-truth measurements made the same
year. The snow accumulation rate between the years 2003 and 2021 also showed
a linear increasing trend of 0.011 m w.e. a<span class="inline-formula"><sup>−2</sup></span>. This trend is
corroborated by comparisons with the surface mass balance (SMB) derived for
the same period from the regional atmospheric climate model MAR (Modèle
Atmosphérique Régional). According to MAR data, which show an
increase of 0.86 <span class="inline-formula"><sup>∘</sup></span>C in this area for the period of 2003–2021, the
linear upward trend is associated with the increase in snowfall and rainfall
events, which may be attributed to elevated global temperatures. The
findings of this study confirmed the viability of our methodology, as well
as its underlying assumptions and interpretation models.</p> |
| first_indexed | 2024-04-10T22:39:41Z |
| format | Article |
| id | doaj.art-8b93fe8083424a6c9acede70e651b843 |
| institution | Directory Open Access Journal |
| issn | 1994-0416 1994-0424 |
| language | English |
| last_indexed | 2024-04-10T22:39:41Z |
| publishDate | 2023-01-01 |
| publisher | Copernicus Publications |
| record_format | Article |
| series | The Cryosphere |
| spelling | doaj.art-8b93fe8083424a6c9acede70e651b8432023-01-16T07:36:09ZengCopernicus PublicationsThe Cryosphere1994-04161994-04242023-01-011717519310.5194/tc-17-175-2023Snow stratigraphy observations from Operation IceBridge surveys in Alaska using S and C band airborne ultra-wideband FMCW (frequency-modulated continuous wave) radarJ. Li0F. Rodriguez-Morales1X. Fettweis2O. Ibikunle3C. Leuschen4J. Paden5D. Gomez-Garcia6E. Arnold7The Center for Remote Sensing and Integrated Systems (CReSIS), University of Kansas, Lawrence, KS 66045, USAThe Center for Remote Sensing and Integrated Systems (CReSIS), University of Kansas, Lawrence, KS 66045, USADepartment of Geography, SPHERES research unit, University of Liège, Liège, BelgiumThe Center for Remote Sensing and Integrated Systems (CReSIS), University of Kansas, Lawrence, KS 66045, USAThe Center for Remote Sensing and Integrated Systems (CReSIS), University of Kansas, Lawrence, KS 66045, USAThe Center for Remote Sensing and Integrated Systems (CReSIS), University of Kansas, Lawrence, KS 66045, USAThe Center for Remote Sensing and Integrated Systems (CReSIS), University of Kansas, Lawrence, KS 66045, USAThe Center for Remote Sensing and Integrated Systems (CReSIS), University of Kansas, Lawrence, KS 66045, USA<p>During the concluding phase of the NASA Operation IceBridge (OIB), we successfully completed two airborne measurement campaigns (in 2018 and 2021, respectively) using a compact S and C band radar installed on a Single Otter aircraft and collected data over Alaskan mountains, ice fields, and glaciers. This paper reports seasonal snow depths derived from radar data. We found large variations in seasonal radar-inferred depths with multi-modal distributions assuming a constant relative permittivity for snow equal to 1.89. About 34 % of the snow depths observed in 2018 were between 3.2 and 4.2 m, and close to 30 % of the snow depths observed in 2021 were between 2.5 and 3.5 m. We observed snow strata in ice facies, combined percolation and wet-snow facies, and dry-snow facies from radar data and identified the transition areas from wet-snow facies to ice facies for multiple glaciers based on the snow strata and radar backscattering characteristics. Our analysis focuses on the measured strata of multiple years at the caldera of Mount Wrangell (K'elt'aeni) to estimate the local snow accumulation rate. We developed a method for using our radar readings of multi-year strata to constrain the uncertain parameters of interpretation models with the assumption that most of the snow layers detected by the radar at the caldera are annual accumulation layers. At a 2004 ice core and 2005 temperature sensor tower site, the locally estimated average snow accumulation rate is <span class="inline-formula">∼2.89</span> m w.e. a<span class="inline-formula"><sup>−1</sup></span> between the years 2003 and 2021. Our estimate of the snow accumulation rate between 2005 and 2006 is 2.82 m w.e. a<span class="inline-formula"><sup>−1</sup></span>, which matches closely to the 2.75 m w.e. a<span class="inline-formula"><sup>−1</sup></span> inferred from independent ground-truth measurements made the same year. The snow accumulation rate between the years 2003 and 2021 also showed a linear increasing trend of 0.011 m w.e. a<span class="inline-formula"><sup>−2</sup></span>. This trend is corroborated by comparisons with the surface mass balance (SMB) derived for the same period from the regional atmospheric climate model MAR (Modèle Atmosphérique Régional). According to MAR data, which show an increase of 0.86 <span class="inline-formula"><sup>∘</sup></span>C in this area for the period of 2003–2021, the linear upward trend is associated with the increase in snowfall and rainfall events, which may be attributed to elevated global temperatures. The findings of this study confirmed the viability of our methodology, as well as its underlying assumptions and interpretation models.</p>https://tc.copernicus.org/articles/17/175/2023/tc-17-175-2023.pdf |
| spellingShingle | J. Li F. Rodriguez-Morales X. Fettweis O. Ibikunle C. Leuschen J. Paden D. Gomez-Garcia E. Arnold Snow stratigraphy observations from Operation IceBridge surveys in Alaska using S and C band airborne ultra-wideband FMCW (frequency-modulated continuous wave) radar The Cryosphere |
| title | Snow stratigraphy observations from Operation IceBridge surveys in Alaska using S and C band airborne ultra-wideband FMCW (frequency-modulated continuous wave) radar |
| title_full | Snow stratigraphy observations from Operation IceBridge surveys in Alaska using S and C band airborne ultra-wideband FMCW (frequency-modulated continuous wave) radar |
| title_fullStr | Snow stratigraphy observations from Operation IceBridge surveys in Alaska using S and C band airborne ultra-wideband FMCW (frequency-modulated continuous wave) radar |
| title_full_unstemmed | Snow stratigraphy observations from Operation IceBridge surveys in Alaska using S and C band airborne ultra-wideband FMCW (frequency-modulated continuous wave) radar |
| title_short | Snow stratigraphy observations from Operation IceBridge surveys in Alaska using S and C band airborne ultra-wideband FMCW (frequency-modulated continuous wave) radar |
| title_sort | snow stratigraphy observations from operation icebridge surveys in alaska using s and c band airborne ultra wideband fmcw frequency modulated continuous wave radar |
| url | https://tc.copernicus.org/articles/17/175/2023/tc-17-175-2023.pdf |
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