Antarctica ice sheet basal melting enhanced by high mantle heat

Antarctica is losing ice mass by basal melting associated with processes in deep Earth and reflected in geothermal heat flux. The latter is poorly known and existing models based on disputed assumptions are controversial. Here I present a new geophysical model for lithospheric thickness and mantle h...

Full description

Bibliographic Details
Published in:Earth-Science Reviews
Main Author: Artemieva, Irina M.
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier 2022
Subjects:
Online Access:https://oceanrep.geomar.de/id/eprint/55172/
https://oceanrep.geomar.de/id/eprint/55172/2/1-s2.0-S0012825222000381-main.pdf
https://oceanrep.geomar.de/id/eprint/55172/8/1-s2.0-S0012825222000381-mmc1.pdf
https://doi.org/10.1016/j.earscirev.2022.103954