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评估 CMIP6 模式模拟的全球陆地区域近地表风速及其未来预测。

Evaluation of global terrestrial near-surface wind speed simulated by CMIP6 models and their future projections.

机构信息

Regional Climate Group, Department of Earth Sciences, University of Gothenburg, Gothenburg, Sweden.

Key Laboratory of Atmospheric Environment and Processes in the Boundary Layer over the Low-Latitude Plateau Region, Department of Atmospheric Science, Yunnan University, Kunming, People's Republic of China.

出版信息

Ann N Y Acad Sci. 2022 Dec;1518(1):249-263. doi: 10.1111/nyas.14910. Epub 2022 Oct 14.

Abstract

We evaluate the performance of Coupled Model Intercomparison Project Phase 6 (CMIP6) models in simulating the observed global terrestrial near-surface wind speed (NSWS) and project its future changes under three different Shared Socioeconomic Pathways (SSPs). Results show that the CESM2 has the best ability in reproducing the observed NSWS trends, although all models examined are generally not doing well. Based on projections of CESM2, the global NSWS will decrease from 2021 to 2100 under all three SSPs. The projected NSWS declines significantly over the north of 20°N, especially across North America, Europe, and the mid-to-high latitudes of Asia; meanwhile, it increases over the south of 20°N. Under SSP585, there would be more light-windy days and fewer strong-windy days than those under SSP245, which leads to a significant global NSWS decline. Robust hemispheric-asymmetric changes in the NSWS could be due to the temperature gradient in the two hemispheres under global warming, with -1.2%, -3.5%, and -4.1% in the Northern Hemisphere, and 0.8%, 1.0%, and 1.5% in the Southern Hemisphere, for the near-term (2021-2040), mid-term (2041-2060), and long-term (2081-2100), respectively.

摘要

我们评估了耦合模式比较计划第六阶段(CMIP6)模型在模拟观测到的全球陆地区域近地表风速(NSWS)方面的性能,并根据三种不同的共享社会经济路径(SSP)预测其未来变化。结果表明,CESM2 模型在再现观测到的 NSWS 趋势方面具有最佳能力,尽管所有被考察的模型总体上表现不佳。根据 CESM2 的预测,在所有三种 SSP 下,全球 NSWS 将从 2021 年到 2100 年减少。在 20°N 以北地区,尤其是北美、欧洲和亚洲中高纬度地区,预计 NSWS 将显著下降;而在 20°N 以南地区,NSWS 将增加。在 SSP585 下,与 SSP245 相比,弱风日数会增加,大风日数会减少,这导致全球 NSWS 显著下降。NSWS 呈现出显著的半球非对称变化,这可能是由于全球变暖导致的两个半球之间的温度梯度造成的,北半球的变化分别为-1.2%、-3.5%和-4.1%,南半球的变化分别为 0.8%、1.0%和 1.5%,分别对应近期(2021-2040 年)、中期(2041-2060 年)和长期(2081-2100 年)。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b361/10092706/36ae51257fbf/NYAS-1518-249-g003.jpg

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