Institute for Marine and Antarctic Studies, University of Tasmania, Hobart, Tasmania, Australia.
Australian Research Council Centre of Excellence for Climate Extremes, University of Tasmania, Hobart, Tasmania, Australia.
Nat Commun. 2020 Aug 28;11(1):4352. doi: 10.1038/s41467-020-18241-x.
Global climate models project the intensification of marine heatwaves in coming decades due to global warming. However, the spatial resolution of these models is inadequate to resolve mesoscale processes that dominate variability in boundary current regions where societal and economic impacts of marine heatwaves are substantial. Here we compare the historical and projected changes in marine heatwaves in a 0.1° ocean model with 23 coarser-resolution climate models. Western boundary currents are the regions where the models disagree the most with observations and among themselves in simulating marine heatwaves of the past and the future. The lack of eddy-driven variability in the coarse-resolution models results in less intense marine heatwaves over the historical period and greater intensification in the coming decades. Although the projected changes agree well at the global scale, the greater spatial details around western boundary currents provided by the high-resolution model may be valuable for effective adaptation planning.
全球气候模型预计,由于全球变暖,未来几十年海洋热浪将加剧。然而,这些模型的空间分辨率不足以解决主导边界流区域变化的中尺度过程,而海洋热浪对社会和经济的影响在这些区域是巨大的。在这里,我们将 0.1°海洋模型与 23 个较粗分辨率气候模型中的历史和预测海洋热浪变化进行了比较。在过去和未来的海洋热浪模拟中,西部边界流是模型与观测结果最不一致的区域,也是模型之间最不一致的区域。粗分辨率模型中缺乏由涡流驱动的可变性,导致历史时期的海洋热浪强度较低,未来几十年的强度增强。尽管在全球范围内预测的变化情况良好,但高分辨率模型提供的西部边界流周围更详细的空间信息可能对有效的适应规划有价值。