Subglacial lakes are repositories of ancient climate conditions, provide habitats for life and
modulate ice flow, basal hydrology, biogeochemical fluxes and geomorphic activity. In this …

The Eurasian ice sheet complex (EISC) was the third largest ice mass during the Last
Glacial Maximum with a span of over 4500 km and responsible for around 20 m of eustatic …

Approximately half of Greenland's current annual mass loss is attributed to runoff from
surface melt. At higher elevations, however, melt does not necessarily equal runoff, because …

Ice sheets are currently ignored in global methane budgets,. Although ice sheets have been
proposed to contain large reserves of methane that may contribute to a rise in atmospheric …

The geological record of landforms and sediments produced beneath deglaciating ice
sheets offers insights into inaccessible glacial processes. Large subglacial valleys formed …

Greenland runoff, from ice mass loss and increasing rainfall, is increasing. That runoff, as
discharge, impacts the physical, chemical, and biological properties of the adjacent fjords …

摘要第三极和北极地区对于区域和全球环境, 社会经济以及国家战略的重要性日益凸现.
通过对第三极和北极气候与冰冻圈研究的现状, 趋势进行梳理总结, 为未来的系统研究提供借鉴 …

Meltwater runoff from the Greenland ice sheet surface influences surface mass balance
(SMB), ice dynamics, and global sea level rise, but is estimated with climate models and …

Coupling between runoff, hydrology, basal motion, and mass loss (“hydrology-dynamics”) is
a critical component of the Greenland Ice Sheet system. Despite considerable research …

Few subglacial lakes have been identified beneath the Greenland Ice Sheet (GrIS) despite
extensive documentation in Antarctica, where periodic release of water can impact ice flow …