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GreenCrust: Tracing a Greenland’s crustal structure under the ice with geophysical inversion and an assessment of geothermal heat flow

Subject Area Geophysics
Term from 2021 to 2024
Project identifier Deutsche Forschungsgemeinschaft (DFG) - Project number 459524577
 
Final Report Year 2024

Final Report Abstract

Greenland's ice mass loss has been one of the largest contributors to global sea level rise since the early 2000s. However, the mechanisms driving the mass loss are not fully understood, and particularly large uncertainties are associated with the conditions under the ice. In our project, we have (i) contributed to a new database of heat flow measurements for Greenland and especially their statistical evaluation applying machine learning. Despite the new database, competing models are commonly used in literature and their implications for ice sheet dynamics have been assessed in (ii). An especially suspicious observation point is the NGRIP (North Greenland Ice Core Project) measurement in Central Greenland and (iii) from statistical analysis, it could be shown that this point has to be treated as an outlier, at least for estimating regional heat flow. This has implications for the crustal contribution to heat flow as shown (iv) by a stepwise modelling of the lithospheric structure of Greenland. Lacking in this lithospheric scale model, is well-constrained information on thermal parameters of the crust and (v) therefore, we measured new samples from Greenland and compared these to estimates available from global databases. These data and models are used as input for (vi) a high-resolution crustal model for Greenland, where we specifically addressed the sub-ice geology and provided an estimate of the potential contribution of the crust to heat flow under the ice.

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