Review article: Geothermal heat flow in Antarctica:  current and future directions

GSTDTAP > 资源环境科学

DOI	10.5194/tc-14-3843-2020
	Review article: Geothermal heat flow in Antarctica: current and future directions
	admin
	2020-12-09
出版年	2020
国家	欧洲
领域	气候变化 ; 资源环境
英文摘要	The Antarctic ice sheet is the largest source for sea level rise. However, one key control on ice sheet flow remains poorly constrained: the effect of heat from the rocks beneath the ice sheet (known as geothermal heat flow). Although this may not seem like a lot of heat, beneath thick, slow ice this heat can control how well the ice flows and can lead to melting of the ice sheet. We discuss the methods used to estimate this heat, compile existing data, and recommend future research.
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来源平台	European Geosciences Union
引用统计
文献类型	科技报告
条目标识符	http://119.78.100.173/C666/handle/2XK7JSWQ/308428
专题	资源环境科学气候变化
推荐引用方式 GB/T 7714	admin. Review article: Geothermal heat flow in Antarctica: current and future directions,2020.