Heat Flux Anomalies in Antarctica Revealed by Satellite Magnetic Data
Author(s) -
Cathrine Fox Maule,
Michael E. Purucker,
Nils Olsen,
Klaus Mosegaard
Publication year - 2005
Publication title -
science
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 12.556
H-Index - 1186
eISSN - 1095-9203
pISSN - 0036-8075
DOI - 10.1126/science.1106888
Subject(s) - heat flux , sea ice growth processes , geology , flux (metallurgy) , volcanism , sea ice thickness , geophysics , geothermal heating , ice sheet , satellite , cryosphere , sea ice , atmospheric sciences , geothermal gradient , climatology , heat transfer , geothermal energy , oceanography , materials science , physics , mechanics , paleontology , astronomy , metallurgy , tectonics
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.
Accelerating Research
Robert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom
Address
John Eccles HouseRobert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom