March 28, 2022 Journal article Open Access

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

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{
  "@context": "https://schema.org/", 
  "@id": "https://doi.org/10.1017/jog.2022.19", 
  "@type": "ScholarlyArticle", 
  "creator": [
    {
      "@type": "Person", 
      "name": "Kenneth C. Jezek"
    }, 
    {
      "@type": "Person", 
      "name": "Caglar Yardim"
    }, 
    {
      "@type": "Person", 
      "name": "Joel T. Johnson"
    }, 
    {
      "@type": "Person", 
      "name": "Giovanni Macelloni"
    }, 
    {
      "@type": "Person", 
      "name": "Marco Brogioni"
    }
  ], 
  "datePublished": "2022-03-28", 
  "description": "Abstract\n\t  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 \u00d7 10\u22128 to 8 \u00d7 10\u22128 kPa\u22123 a\u22121 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\u22122 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\u22122 in the central portion of the profile.", 
  "headline": "Analysis of ice-sheet temperature profiles from low-frequency airborne remote sensing", 
  "identifier": "https://doi.org/10.1017/jog.2022.19", 
  "image": "https://zenodo.org/static/img/logos/zenodo-gradient-round.svg", 
  "inLanguage": {
    "@type": "Language", 
    "alternateName": "eng", 
    "name": "English"
  }, 
  "keywords": [
    "Earth-Surface Processes"
  ], 
  "license": "https://creativecommons.org/licenses/by/4.0/", 
  "name": "Analysis of ice-sheet temperature profiles from low-frequency airborne remote sensing", 
  "url": "https://www.openaccessrepository.it/record/90489"
}