Using specularity content to evaluate eight geothermal heat flow maps of Totten Glacier
<p>Geothermal heat flow (GHF) is the dominant factor affecting the basal thermal regime of ice sheet dynamics. But it is poorly defined for the Antarctic ice sheet. We compare the basal thermal state of the Totten Glacier catchment as simulated by eight different GHF datasets. We use a basal e...
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| Format: | Article |
| Language: | English |
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Copernicus Publications
2024-01-01
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| Series: | The Cryosphere |
| Online Access: | https://tc.copernicus.org/articles/18/103/2024/tc-18-103-2024.pdf |
| _version_ | 1797366267995226112 |
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| author | Y. Huang L. Zhao M. Wolovick Y. Ma J. C. Moore |
| author_facet | Y. Huang L. Zhao M. Wolovick Y. Ma J. C. Moore |
| author_sort | Y. Huang |
| collection | DOAJ |
| description | <p>Geothermal heat flow (GHF) is the dominant factor affecting the basal thermal regime of ice sheet dynamics. But it is poorly defined for the Antarctic ice sheet. We compare the basal thermal state of the Totten Glacier catchment as simulated by eight different GHF datasets. We use a basal energy and water flow model coupled with a 3D full-Stokes ice dynamics model to estimate the basal temperature, basal friction heat and basal melting rate. In addition to the location of subglacial lakes, we use specularity content of the airborne radar returns as a two-sided constraint to discriminate between local wet or dry basal conditions and compare the returns with the basal state simulations with different GHFs. Two medium magnitude GHF distribution maps derived from seismic modelling rank well at simulating both cold- and warm-bed regions, the GHFs from Shen et al. (2020) and Shapiro and Ritzwoller (2004). The best-fit simulated result shows that most of the inland bed area is frozen. Only the central inland subglacial canyon, co-located with high specularity content, reaches the pressure melting point consistently in all the eight GHFs. Modelled basal melting rates in the slow-flowing region are generally 0–5 mm yr<span class="inline-formula"><sup>−1</sup></span> but with local maxima of 10 mm yr<span class="inline-formula"><sup>−1</sup></span> at the central inland subglacial canyon. The fast-flowing grounded glaciers close to the Totten ice shelf are lubricating their bases with meltwater at rates of 10–400 mm yr<span class="inline-formula"><sup>−1</sup></span>.</p> |
| first_indexed | 2024-03-08T17:01:52Z |
| format | Article |
| id | doaj.art-6edf3e30da494a3ca505fddb9fb4b597 |
| institution | Directory Open Access Journal |
| issn | 1994-0416 1994-0424 |
| language | English |
| last_indexed | 2024-03-08T17:01:52Z |
| publishDate | 2024-01-01 |
| publisher | Copernicus Publications |
| record_format | Article |
| series | The Cryosphere |
| spelling | doaj.art-6edf3e30da494a3ca505fddb9fb4b5972024-01-04T08:24:26ZengCopernicus PublicationsThe Cryosphere1994-04161994-04242024-01-011810311910.5194/tc-18-103-2024Using specularity content to evaluate eight geothermal heat flow maps of Totten GlacierY. Huang0L. Zhao1M. Wolovick2Y. Ma3J. C. Moore4State Key Laboratory of Earth Surface Processes and Resource Ecology, Faculty of Geographical Science, Beijing Normal University, Beijing 100875, ChinaState Key Laboratory of Earth Surface Processes and Resource Ecology, Faculty of Geographical Science, Beijing Normal University, Beijing 100875, ChinaGlaciology Section, Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar- und Meeresforschung, Bremerhaven, GermanyState Key Laboratory of Earth Surface Processes and Resource Ecology, Faculty of Geographical Science, Beijing Normal University, Beijing 100875, ChinaArctic Centre, University of Lapland, Rovaniemi, Finland<p>Geothermal heat flow (GHF) is the dominant factor affecting the basal thermal regime of ice sheet dynamics. But it is poorly defined for the Antarctic ice sheet. We compare the basal thermal state of the Totten Glacier catchment as simulated by eight different GHF datasets. We use a basal energy and water flow model coupled with a 3D full-Stokes ice dynamics model to estimate the basal temperature, basal friction heat and basal melting rate. In addition to the location of subglacial lakes, we use specularity content of the airborne radar returns as a two-sided constraint to discriminate between local wet or dry basal conditions and compare the returns with the basal state simulations with different GHFs. Two medium magnitude GHF distribution maps derived from seismic modelling rank well at simulating both cold- and warm-bed regions, the GHFs from Shen et al. (2020) and Shapiro and Ritzwoller (2004). The best-fit simulated result shows that most of the inland bed area is frozen. Only the central inland subglacial canyon, co-located with high specularity content, reaches the pressure melting point consistently in all the eight GHFs. Modelled basal melting rates in the slow-flowing region are generally 0–5 mm yr<span class="inline-formula"><sup>−1</sup></span> but with local maxima of 10 mm yr<span class="inline-formula"><sup>−1</sup></span> at the central inland subglacial canyon. The fast-flowing grounded glaciers close to the Totten ice shelf are lubricating their bases with meltwater at rates of 10–400 mm yr<span class="inline-formula"><sup>−1</sup></span>.</p>https://tc.copernicus.org/articles/18/103/2024/tc-18-103-2024.pdf |
| spellingShingle | Y. Huang L. Zhao M. Wolovick Y. Ma J. C. Moore Using specularity content to evaluate eight geothermal heat flow maps of Totten Glacier The Cryosphere |
| title | Using specularity content to evaluate eight geothermal heat flow maps of Totten Glacier |
| title_full | Using specularity content to evaluate eight geothermal heat flow maps of Totten Glacier |
| title_fullStr | Using specularity content to evaluate eight geothermal heat flow maps of Totten Glacier |
| title_full_unstemmed | Using specularity content to evaluate eight geothermal heat flow maps of Totten Glacier |
| title_short | Using specularity content to evaluate eight geothermal heat flow maps of Totten Glacier |
| title_sort | using specularity content to evaluate eight geothermal heat flow maps of totten glacier |
| url | https://tc.copernicus.org/articles/18/103/2024/tc-18-103-2024.pdf |
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