格陵兰冰盖底部蕴藏着气候变化的关键信息，对理解未来地球气候系统演化有着重要的科学意义。本文回顾了中国团队参加格陵兰深冰芯考察计划的过程和历史，讨论了深冰芯、冰盖和气候变化之间的联系，并展望了未来在冰盖和气候不稳定性领域的研究方向。
The base of the Greenland ice sheet holds crucial information on climate change, which is of scientific importance for understanding the future evolution of Earth's climate system. This paper reviews the involvement of the Chinese team in the Greenland deep ice core drilling project, discusses the connections between deep ice cores, ice sheets, and climate change, and explores future research directions in the field of ice sheet and climate instability
[1] TAYLOR K C, HAMMER C U, ALLEY R B, et al. Electrical conductivity measurements from the GISP2 and GRIP Greenland ice cores [J]. Nature, 1993, 366: 549-552．
[2] XIAO C, DU Z, HANDLEY M J, et al. Iron in the NEEM ice core relative to Asian loess records over the last glacial-interglacial cycle
[J]. National Science Review, 2021, 8(7): nwaa144.
[3] NEEM community members. Eemian interglacial reconstructed from a Greenland folded ice core [J]. Nature, 2013, 493: 489-494.
[4] ZEISING O, HUMBERT A. Indication of high basal melting at the EastGRIP drill site on the Northeast Greenland Ice Stream [J]. The
Cryosphere, 2021, 15(7): 3119-3128.
[5] ZHANG T, COLGAN W, WANSING A, et al. Evaluating different geothermal heat flow maps as basal boundary conditions during
spin-up of the Greenland ice sheet [J]. The Cryosphere, 2024, 18(1): 387-402.
