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Radar attenuation d...
Radar attenuation demonstrates advective cooling in the Siple Coast ice streams
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- Hills, Benjamin H. (författare)
- Department of Earth and Space Sciences, University of Washington, Seattle, WA, USA.; Applied Physics Laboratory, Polar Science Center, University of Washington, Seattle, WA, USA.
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- Christianson, Knut (författare)
- Department of Earth and Space Sciences, University of Washington, Seattle, WA, USA.
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- Jacobel, Robert W. (författare)
- Department of Physics, St Olaf College, Northfield, MN, USA.
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- Conway, Howard (författare)
- Department of Earth and Space Sciences, University of Washington, Seattle, WA, USA.
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- Pettersson, Rickard (författare)
- Uppsala universitet,Luft-, vatten- och landskapslära
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Department of Earth and Space Sciences, University of Washington, Seattle, WA, USA; Applied Physics Laboratory, Polar Science Center, University of Washington, Seattle, WA, USA. Department of Earth and Space Sciences, University of Washington, Seattle, WA, USA. (creator_code:org_t)
- 2022-10-11
- 2022
- Engelska.
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Ingår i: Journal of Glaciology. - : Cambridge University Press. - 0022-1430 .- 1727-5652. ; 69:275, s. 566-576
- Relaterad länk:
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https://doi.org/10.1...
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https://uu.diva-port... (primary) (Raw object)
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https://urn.kb.se/re...
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https://doi.org/10.1...
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Abstract
Ämnesord
Stäng
- Ice streams are warmed by shear strain, both vertical shear near the bed and lateral shear at the margins. Warm ice deforms more easily, establishing a positive feedback loop in an ice stream where fast flow leads to warm ice and then to even faster flow. Here, we use radar attenuation measurements to show that the Siple Coast ice streams are colder than previously thought, which we hypothesize is due to along-flow advection of cold ice from upstream. We interpret the attenuation results within the context of previous ice-temperature measurements from nearby sites where hot-water boreholes were drilled. These in-situ temperatures are notably colder than model predictions, both in the ice streams and in an ice-stream shear margin. We then model ice temperature using a 1.5-dimensional numerical model which includes a parameterization for along-flow advection. Compared to analytical solutions, we find depth-averaged temperatures that are colder by 0.7°C in the Bindschadler Ice Stream, 2.7°C in the Kamb Ice Stream and 6.2–8.2°C in the Dragon Shear Margin of Whillans Ice Stream, closer to the borehole measurements at all locations. Modelled cooling corresponds to shear-margin thermal strengthening by 3–3.5 times compared to the warm-ice case, which must be compensated by some other weakening mechanism such as material damage or ice-crystal fabric anisotropy.
Ämnesord
- NATURVETENSKAP -- Geovetenskap och miljövetenskap -- Oceanografi, hydrologi och vattenresurser (hsv//swe)
- NATURAL SCIENCES -- Earth and Related Environmental Sciences -- Oceanography, Hydrology and Water Resources (hsv//eng)
Nyckelord
- ice dynamics
- ice streams
- ice temperature
- radio-echo sounding
- Earth Science with specialization in Physical Geography
- Geovetenskap med inriktning mot naturgeografi
Publikations- och innehållstyp
- ref (ämneskategori)
- art (ämneskategori)
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