March 28, 2022 Journal article Open Access

Kenneth C. Jezek; Caglar Yardim; Joel T. Johnson; Giovanni Macelloni; Marco Brogioni

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    <subfield code="a">Kenneth C. Jezek</subfield>
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    <subfield code="a">Analysis of ice-sheet temperature profiles from low-frequency airborne remote sensing</subfield>
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    <subfield code="a">Caglar Yardim</subfield>
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    <subfield code="a">Marco Brogioni</subfield>
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    <subfield code="a">Earth-Surface Processes</subfield>
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    <subfield code="a">Abstract
	  Ice internal temperature and basal geothermal heat flux (GHF) are analyzed along a study line in northwestern Greenland. The temperatures were obtained from a previously reported inversion of airborne microwave brightness-temperature spectra. The temperatures vary slowly through the upper ice sheet and more rapidly near the base increasing from ~259 K near Camp Century to values near the melting point near NorthGRIP. The flow-law rate factor is computed from temperature data and analytic expressions. The rate factor increases from ~1 × 10−8 to 8 × 10−8 kPa−3 a−1 along the line. A laminar flow model combined with the depth-dependent rate factor is used to estimate horizontal velocity. The modeled surface velocities are about a factor of 10 less than interferometric synthetic aperture radar (InSAR) surface velocities. The laminar velocities are fitted to the InSAR velocities through a factor of 8 enhancement of the rate factor for the lower 25% of the column. GHF values retrieved from the brightness temperature spectra increase from ~55 to 84 mW m−2 from Camp Century to NorthGRIP. A strain heating correction improves agreement with other geophysical datasets near Camp Century and NEEM but differ by ~15 mW m−2 in the central portion of the profile.</subfield>
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    <subfield code="a">10.1017/jog.2022.19</subfield>
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