Department of Atmospheric Science, Colorado State University, Fort Collins, CO, USA.
School of Environmental Sciences, University of East Anglia, Norwich, UK.
Nature. 2021 Nov;599(7885):425-430. doi: 10.1038/s41586-021-03943-z. Epub 2021 Nov 17.
Climate change has been and will be accompanied by widespread changes in surface temperature. It is clear that these changes include global-wide increases in mean surface temperature and changes in temperature variance that are more regionally-dependent. It is less clear whether they also include changes in the persistence of surface temperature. This is important as the effects of weather events on ecosystems and society depend critically on the length of the event. Here we provide an extensive survey of the response of surface temperature persistence to climate change over the twenty-first century from the output of 150 simulations run on four different Earth system models, and from simulations run on simplified models with varying representations of radiative processes and large-scale dynamics. Together, the results indicate that climate change simulations are marked by widespread changes in surface temperature persistence that are generally most robust over ocean areas and arise due to a seemingly broad range of physical processes. The findings point to both the robustness of widespread changes in persistence under climate change, and the critical need to better understand, simulate and constrain such changes.
气候变化已经并将伴随着地表温度的广泛变化。很明显,这些变化包括全球范围内平均地表温度的升高和温度方差的变化,后者更依赖于区域。目前还不太清楚它们是否还包括地表温度持续性的变化。这一点很重要,因为天气事件对生态系统和社会的影响在很大程度上取决于事件的持续时间。在这里,我们从四个不同的地球系统模型的 150 次模拟输出中,以及从具有不同辐射过程和大尺度动力表示的简化模型的模拟中,对二十一世纪地表温度持续性对气候变化的响应进行了广泛的调查。总的来说,结果表明,气候变化模拟的特点是地表温度持续性的广泛变化,这些变化在海洋地区最为显著,而且是由于一系列广泛的物理过程造成的。这些发现不仅表明了气候变化下持续性广泛变化的稳健性,而且还突出表明了迫切需要更好地理解、模拟和约束这些变化。