Inversion of Geothermal Heat Flux under the Ice Sheet of Princess Elizabeth Land, East Antarctica

Antarctic geothermal heat flux is a basic input variable for ice sheet dynamics simulation. It greatly affects the temperature and mechanical properties at the bottom of the ice sheet, influencing sliding, melting, and internal deformation. Due to the fact that the Antarctica is covered by a thick i...

Full description

Bibliographic Details
Published in:Remote Sensing
Main Authors: Lin Li, Xueyuan Tang, Jingxue Guo, Xiangbin Cui, Enzhao Xiao, Khalid Latif, Bo Sun, Qiao Zhang, Xiaosong Shi
Format: Article in Journal/Newspaper
Language:English
Published: MDPI AG 2021
Subjects:
Q
Online Access:https://doi.org/10.3390/rs13142760
https://doaj.org/article/8f408049fc9f42378161efff040f9b29