Chen Di, Fu Min, Liu Xin, Sun Qizhen
Department of Earth, Atmospheric, and Planetary Sciences, Purdue University, West Lafayette, IN, USA.
National Marine Environmental Forecasting Center, Beijing, China.
Sci Rep. 2024 Jul 18;14(1):16585. doi: 10.1038/s41598-024-67391-1.
Simulating and predicting Arctic sea ice accurately remains an academic focus due to the complex and unclear mechanisms of Arctic sea ice variability and model biases. Meanwhile, the relevant forecasting and monitoring authorities are searching for models to meet practical needs. Given the previous ideal performance of cGENIE model in other fields and notable features, we evaluated the model's skill in simulating Arctic sea ice using multiple methods and it demonstrates great potential and combined advantages. On this basis, we examined the direct drivers of sea-ice variability and predicted the future spatio-temporal changes of Arctic sea ice using the model under different Representative Concentration Pathways (RCP) scenarios. Further studies also found that Arctic sea ice concentration shows large regional differences under RCP 8.5, while the magnitude of the reduction in Arctic sea ice thickness is generally greater compared to concentration, showing a more uniform consistency of change.
由于北极海冰变化机制复杂且不明确以及模型偏差,准确模拟和预测北极海冰仍然是一个学术焦点。与此同时,相关的预测和监测机构正在寻找满足实际需求的模型。鉴于cGENIE模型此前在其他领域的理想表现和显著特征,我们使用多种方法评估了该模型在模拟北极海冰方面的技能,结果表明它具有巨大潜力和综合优势。在此基础上,我们研究了海冰变化的直接驱动因素,并利用该模型在不同代表性浓度路径(RCP)情景下预测了北极海冰未来的时空变化。进一步的研究还发现,在RCP 8.5情景下,北极海冰浓度存在较大的区域差异,而北极海冰厚度的减少幅度总体上比浓度变化更大,呈现出更一致的变化趋势。