Heat flux anomalies in Antarctica revealed from satellite magnetic data

The geothermal heat flux is an important factor in the dynamics of ice sheets; it affects the occurrence of subglacial lakes, the onset of ice streams, and mass losses from the ice sheet base. Because direct heat flux measurements in ice-covered regions are difficult to obtain, we developed a method...

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Bibliographic Details
Published in:Science
Main Authors: Maule, Cathrine Fox, Purucker, Michael E., Olsen, Nils, Mosegaard, Klaus
Format: Article in Journal/Newspaper
Language:English
Published: 2005
Subjects:
Online Access:https://orbit.dtu.dk/en/publications/92d61a74-6a79-4d97-b724-711656ef5d7a
https://doi.org/10.1126/science.1106888
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Summary:The geothermal heat flux is an important factor in the dynamics of ice sheets; it affects the occurrence of subglacial lakes, the onset of ice streams, and mass losses from the ice sheet base. Because direct heat flux measurements in ice-covered regions are difficult to obtain, we developed a method that uses satellite magnetic data to estimate the heat flux underneath the Antarctic ice sheet. We found that the heat flux underneath the ice sheet varies from 40 to 185 megawatts per square meter and that areas of high heat flux coincide with known current volcanism and some areas known to have ice streams.