Minière Audrey, von Schuckmann Karina, Sallée Jean-Baptiste, Vogt Linus
Université Toulouse III - Paul Sabatier, Toulouse, France.
Mercator Ocean International, Toulouse, France.
Sci Rep. 2023 Dec 27;13(1):22975. doi: 10.1038/s41598-023-49353-1.
Global heating of the Earth system is unequivocal. However, detecting an acceleration of Earth heating has remained elusive to date, despite suggestive evidence of a potential increase in heating rates. In this study, we demonstrate that since 1960, the warming of the world ocean has accelerated at a relatively consistent pace of 0.15 ± 0.05 (W/m)/decade, while the land, cryosphere, and atmosphere have exhibited an accelerated pace of 0.013 ± 0.003 (W/m)/decade. This has led to a substantial increase in ocean warming, with a magnitude of 0.91 ± 0.80 W/m between the decades 1960-1970 and 2010-2020, which overlies substantial decadal-scale variability in ocean warming of up to 0.6 W/m. Our findings withstand a wide range of sensitivity analyses and are consistent across different observation-based datasets. The long-term acceleration of Earth warming aligns qualitatively with the rise in CO concentrations and the decline in aerosol concentration during the same period, but further investigations are necessary to properly attribute these changes.
地球系统的全球变暖是确凿无疑的。然而,尽管有迹象表明升温速率可能增加,但迄今为止,检测到地球升温加速仍然难以实现。在本研究中,我们证明,自1960年以来,世界海洋变暖以相对一致的速度加速,为0.15±0.05(瓦/平方米)/十年,而陆地、冰冻圈和大气的升温速度为0.013±0.003(瓦/平方米)/十年。这导致海洋变暖大幅增加,在1960 - 1970年和2010 - 2020年这两个十年间,变暖幅度为0.91±0.80瓦/平方米,叠加了海洋变暖高达0.6瓦/平方米的显著年代际尺度变化。我们的研究结果经受住了广泛的敏感性分析,并且在不同的基于观测的数据集之间是一致的。地球变暖的长期加速在定性上与同期二氧化碳浓度的上升和气溶胶浓度的下降相一致,但需要进一步研究来正确归因这些变化。