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This page provides a simple browsing interface for finding entities described by a property and a named value. Other available search interfaces include the page property search, and the ask query builder.
List of results
- Lab-0017 + (<p>The Kudryavtsev et al. (1974), or … <p>The Kudryavtsev et al. (1974), or Ku model, presents an approximate solution of the Stefan problem. The model provides a steady-state solution under the assumption of sinusoidal air temperature forcing. It considers snow, vegetation, and soil layers as thermal damping to variation of air temperature. The layer of soil is considered to be a homogeneous column with different thermal properties in the frozen and thawed states. The main outputs are annual maximum frozen/thaw depth and mean annual temperature at the top of permafrost (or at the base of the active layer). It can be applied over a wide variety of climatic conditions.</p></br></br><p>The Ku model is part of the Permamodel Toolbox, see Overeem ''et al.'' 2018.</p> of the Permamodel Toolbox, see Overeem ''et al.'' 2018.</p>)
- Lab-0002 + (<p>The Kudryavtsev et al. (1974), or … <p>The Kudryavtsev et al. (1974), or Ku model, presents an approximate solution of the Stefan problem. The model provides a steady-state solution under the assumption of sinusoidal air temperature forcing. It considers snow, vegetation, and soil layers as thermal damping to variation of air temperature. The layer of soil is considered to be a homogeneous column with different thermal properties in the frozen and thawed states. The main outputs are annual maximum frozen/thaw depth and mean annual temperature at the top of permafrost (or at the base of the active layer). It can be applied over a wide variety of climatic conditions.</p></br></br><p>The Ku model is part of the Permamodel Toolbox, see Overeem ''et al.'' 2018.</p> of the Permamodel Toolbox, see Overeem ''et al.'' 2018.</p>)
