Model:GIPL: Difference between revisions
m (Text replacement - "Add_reference_upload_buttons" to "Add_reference_upload_button") |
|||
Line 106: | Line 106: | ||
== References == | == References == | ||
<br>{{ | <br>{{Add_reference_upload_button}}<br><br> | ||
{{#ifexist:Template:{{PAGENAME}}-citation-indices|{{{{PAGENAME}}-citation-indices}}|}}<br> | {{#ifexist:Template:{{PAGENAME}}-citation-indices|{{{{PAGENAME}}-citation-indices}}|}}<br> | ||
{{Add_model_references}} | {{Add_model_references}} |
Revision as of 11:18, 1 May 2017
GIPL
Metadata
|
|
Introduction
GIPL(Geophysical Institute Permafrost Laboratory) is an implicit finite difference one-dimensional heat flow numerical model.The model uses fine vertical resolution grid which preserves the latent-heat effects in the phase transition zone, even under conditions of rapid or abrupt changes in the temperature fields. It includes upper boundary condition (usually air temperature), constant geothermal heat flux at the lower boundary (typically from 500 to 1000 m) and initial temperature distribution with depth. The other inputs are precipitation, prescribed water content and thermal properties of the multilayered soil column. As an output the model produces temperature distributions at different depths, active layer thickness and calculates time of freeze up. The results include temperatures at different depths and active layer thickness, freeze-up days.
IRF
Issues
Does not include convective heat transfer.
Visualization
References
Nr. of publications: | 30 |
Total citations: | 1155 |
h-index: | 16 |
m-quotient: | 0.76 |
Source code
Suggested way to reference a version of the model source code following data reference guidelines:
Publication(s) | Model described | Citations |
---|
Overview and general
Publication(s) | Model described | Citations |
---|
Applications
Publication(s) | Model described | Citations |
---|
Related theory and data
Publication(s) | Model described | Citations |
---|