Mann Michael E, Steinman Byron A, Brouillette Daniel J, Miller Sonya K
Department of Meteorology and Atmospheric Science, The Pennsylvania State University, 514 Walker Building, University Park, PA 16802-5013, USA.
Department of Earth and Environmental Sciences and Large Lakes Observatory, University of Minnesota Duluth, 2205 East 5th Street, Duluth, MN 55812, USA.
Science. 2021 Mar 5;371(6533):1014-1019. doi: 10.1126/science.abc5810.
Past research argues for an internal multidecadal (40- to 60-year) oscillation distinct from climate noise. Recent studies have claimed that this so-termed Atlantic Multidecadal Oscillation is instead a manifestation of competing time-varying effects of anthropogenic greenhouse gases and sulfate aerosols. That conclusion is bolstered by the absence of robust multidecadal climate oscillations in control simulations of current-generation models. Paleoclimate data, however, do demonstrate multidecadal oscillatory behavior during the preindustrial era. By comparing control and forced "Last Millennium" simulations, we show that these apparent multidecadal oscillations are an artifact of pulses of volcanic activity during the preindustrial era that project markedly onto the multidecadal (50- to 70-year) frequency band. We conclude that there is no compelling evidence for internal multidecadal oscillations in the climate system.
过去的研究认为存在一种与气候噪声不同的内部多年代际(40至60年)振荡。最近的研究声称,这种所谓的大西洋多年代际振荡实际上是人为温室气体和硫酸盐气溶胶随时间变化的竞争效应的一种表现。当前一代模型的控制模拟中缺乏稳健的多年代际气候振荡,这一结论得到了支持。然而,古气候数据确实表明在工业化前时代存在多年代际振荡行为。通过比较控制模拟和强迫的“过去一千年”模拟,我们表明这些明显的多年代际振荡是工业化前时代火山活动脉冲的一种假象,这些脉冲显著投射到多年代际(50至70年)频段上。我们得出结论,气候系统中没有令人信服的证据表明存在内部多年代际振荡。