Yu Ling, Cao Hong, Yue Liang
State Grid Songjiang Power Supply Company, Shanghai, China.
PLoS One. 2025 Mar 21;20(3):e0319210. doi: 10.1371/journal.pone.0319210. eCollection 2025.
Wind energy, as one of the renewable energy sources, plays a crucial role in the global energy system's transition to clean energy. China possesses vast and widely distributed wind energy resources, and in recent years, it has rapidly developed and begun large-scale commercial utilization. Therefore, studying changes in surface wind speeds (SWSs) is highly important for wind energy development in China. This study utilizes two initial condition large ensemble simulations to project future changes in SWSs over China. The two sets of initial large ensemble models used are CanESM2-LE and CESM1-LE. By comparing the results from these two large ensemble models, the influence of internal variability of the climate system on SWSs in China are studied. Both models can effectively reproduce the climatological spatial distribution of SWSs in reanalysis. Results from both models indicate that external forcing leads to an increase in winter SWSs in eastern China, while SWSs decreases in the southeastern coastal areas and southwestern Tibet. In summer, SWSs exhibits a pattern of decrease in the north and increase in the south. The magnitude of wind speed changes is greater in winter than in summer. Additionally, as the projected period extends, the magnitude of these changes intensifies. The research results can provide a scientific basis for the future planning of wind power deployment.
风能作为可再生能源之一,在全球能源系统向清洁能源转型过程中发挥着关键作用。中国拥有广袤且分布广泛的风能资源,近年来,中国风能迅速发展并开始大规模商业利用。因此,研究地表风速(SWSs)的变化对中国风能开发至关重要。本研究利用两个初始条件大集合模拟来预测中国未来地表风速的变化。所使用的两组初始大集合模型分别是CanESM2 - LE和CESM1 - LE。通过比较这两个大集合模型的结果,研究了气候系统内部变率对中国地表风速的影响。两个模型都能有效再现再分析中地表风速的气候学空间分布。两个模型的结果均表明,外部强迫导致中国东部冬季地表风速增加,而东南部沿海地区和西藏西南部的地表风速降低。在夏季,地表风速呈现出北部降低、南部增加的模式。风速变化的幅度冬季大于夏季。此外,随着预测期的延长,这些变化的幅度会加剧。研究结果可为未来风电部署规划提供科学依据。