Statistical appraisal of geothermal heat flow observations in the Arctic by J. Freienstein, W. Szwillus, A. Wansing, J. Ebbing

“…We find that most of the continental heat flow observations have a high reliability and agreement to solid Earth models, except a few data points, such as, for example, the NGRIP (North Greenland Ice Core Project) point in central Greenland.</p> <p>For further testing, we perform a conditional simulation with focus on Greenland in which the local characteristics of heat flow structures can be considered. …”
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