气候变化研究进展 ›› 2026, Vol. 22 ›› Issue (1): 1-13.doi: 10.12006/j.issn.1673-1719.2025.149
王千禧1,2, 李腾1,2(
), 唐学远3, 张通4, 张子谦5, 丁明虎6, 程晓1,2
收稿日期:2025-06-24
修回日期:2025-08-29
出版日期:2026-01-30
发布日期:2025-12-25
通讯作者:
李腾,男,助理教授,作者简介:王千禧,男,博士研究生
基金资助:
WANG Qian-Xi1,2, LI Teng1,2(
), TANG Xue-Yuan3, ZHANG Tong4, ZHANG Zi-Qian5, DING Ming-Hu6, CHENG Xiao1,2
Received:2025-06-24
Revised:2025-08-29
Online:2026-01-30
Published:2025-12-25
摘要:
冰盖临界点问题已成为冰盖-气候系统非线性响应研究的核心领域,蕴含深刻的反馈机制、临界阈值与不可逆性等关键科学议题。在系统梳理冰盖临界点基本内涵的基础上,重点解析正反馈机制如何驱动系统跨越稳定边界,以及负反馈过程在减缓变率、维持相对稳态中的潜在作用。进一步从格陵兰冰盖、西南极冰盖与东南极冰盖三大系统出发,剖析各自的临界演化路径、动态特征及其对扰动的响应差异,突出地形控制、冰-海耦合与局地扰动传播等关键因素的调节作用。结合系统耦合与级联机制的研究进展,指出多临界过程之间可能存在协同触发和级联风险,并梳理当前数值模拟中的主要不确定性来源及其改进思路。在此基础上,提出观测-模拟融合框架的优化路径,强调临界点识别与预警机制在未来冰盖演化和不确定性评估中的关键意义,以此支撑冰盖系统临界行为的理论深化与模拟能力提升,并夯实其在未来气候情景下潜在风险的理论基础。
王千禧, 李腾, 唐学远, 张通, 张子谦, 丁明虎, 程晓. 极地冰盖临界点:机制解析、系统响应与模拟挑战[J]. 气候变化研究进展, 2026, 22(1): 1-13.
WANG Qian-Xi, LI Teng, TANG Xue-Yuan, ZHANG Tong, ZHANG Zi-Qian, DING Ming-Hu, CHENG Xiao. Polar ice sheet tipping points: mechanisms, system responses, and modeling challenges[J]. Climate Change Research, 2026, 22(1): 1-13.
图2 冰盖系统接地线潜在稳态示意图(据Reese等[40]改绘)(a) MISI机制下的稳态分支图,(b)完全可逆系统 注:这里的控制参数如全球平均温度、气候条件等;冰盖系统状态如接地线位置、浮力线以上冰体积等。
Fig. 2 Schematic of potential steady states of the ice-sheet grounding line [40]. (a) Steady-state branches under the MISI mechanism, (b) fully reversible system
图3 冰盖系统对扰动的非线性响应类型与突变机制示意图(据Rosier等[66]改绘)(a)可逆线性响应,(b)低强迫引发强响应但仍可恢复,(c)产生滞后性失稳与迟滞现象,(d)出现永久性不可逆 注:其中,x1、x2、x3、xt为临界点,其中xt表示由于瞬态滞后,系统状态晚于控制量变化的临界点。
Fig. 3 Schematic illustration of types of nonlinear responses and tipping mechanisms of the ice-sheet system to perturbations [66]. (a) Reversible linear response, (b) strong but still reversible response triggered by weak forcing, (c) onset of delayed instability and hysteresis, (d) permanent, irreversible response
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