January 1, 2000 Journal article Open Access

Frédérique Rémy; C. Bianchi; Ignazio E. Tabacco; Laurent Testut

JSON Export

{
  "conceptrecid": "121926", 
  "created": "2023-09-27T14:46:00.786029+00:00", 
  "doi": "10.3189/172756400781820877", 
  "files": [
    {
      "bucket": "2c2f0430-fd20-43a9-ba5b-afa1606f95e8", 
      "checksum": "md5:0b67863af6e6347bf930958dd1c772a8", 
      "key": "fulltext.pdf", 
      "links": {
        "self": "https://www.openaccessrepository.it/api/files/2c2f0430-fd20-43a9-ba5b-afa1606f95e8/fulltext.pdf"
      }, 
      "size": 193513, 
      "type": "pdf"
    }
  ], 
  "id": 121927, 
  "links": {
    "badge": "https://www.openaccessrepository.it/badge/doi/10.3189/172756400781820877.svg", 
    "bucket": "https://www.openaccessrepository.it/api/files/2c2f0430-fd20-43a9-ba5b-afa1606f95e8", 
    "doi": "https://doi.org/10.3189/172756400781820877", 
    "html": "https://www.openaccessrepository.it/record/121927", 
    "latest": "https://www.openaccessrepository.it/api/records/121927", 
    "latest_html": "https://www.openaccessrepository.it/record/121927"
  }, 
  "metadata": {
    "access_right": "open", 
    "access_right_category": "success", 
    "communities": [
      {
        "id": "itmirror"
      }
    ], 
    "creators": [
      {
        "name": "Fr\u00e9d\u00e9rique R\u00e9my"
      }, 
      {
        "name": "C. Bianchi"
      }, 
      {
        "name": "Ignazio E. Tabacco"
      }, 
      {
        "name": "Laurent Testut"
      }
    ], 
    "description": "AbstractImproved knowledge of geometrical boundary conditions, such as bedrock geometry and surface topography, can contribute significantly to glaciological studies including ice-sheet-flow modelling. Precise thickness and altimetric data allow an estimation of ice-flow direction, the balance velocity and the basal shear stress. These parameters are calculated along a 1160 km profile in East Antarctica using a relationship between shear stress, basal temperature, the Glen flow exponent and a parameter related to strain rate. Strong variations of the flow-law parameters and basal conditions are found to play a major role in the ice-flow pattern. Sliding, anisotropy and longitudinal stress strongly perturb the validity of the law, but their signature can be identified.", 
    "doi": "10.3189/172756400781820877", 
    "keywords": [
      "NEANIAS Atmospheric Research Community", 
      "Earth-Surface Processes"
    ], 
    "language": "eng", 
    "license": {
      "id": "other-open"
    }, 
    "notes": "", 
    "publication_date": "2000-01-01", 
    "relations": {
      "version": [
        {
          "count": 1, 
          "index": 0, 
          "is_last": true, 
          "last_child": {
            "pid_type": "recid", 
            "pid_value": "121927"
          }, 
          "parent": {
            "pid_type": "recid", 
            "pid_value": "121926"
          }
        }
      ]
    }, 
    "resource_type": {
      "subtype": "article", 
      "title": "Journal article", 
      "type": "publication"
    }, 
    "title": "Influence of geometrical boundary conditions on the estimation of rheological parameters"
  }, 
  "owners": [
    14
  ], 
  "revision": 1, 
  "stats": {
    "downloads": 0.0, 
    "unique_downloads": 0.0, 
    "unique_views": 0.0, 
    "version_downloads": 0.0, 
    "version_unique_downloads": 0.0, 
    "version_unique_views": 0.0, 
    "version_views": 0.0, 
    "version_volume": 0.0, 
    "views": 0.0, 
    "volume": 0.0
  }, 
  "updated": "2023-09-27T14:46:00.897324+00:00"
}