Davis N A, Richter J H, Glanville A A, Edwards J, LaJoie E
Atmospheric Chemistry Observations and Modeling Laboratory, National Center for Atmospheric Research, Boulder, CO, USA.
Climate and Global Dynamics Laboratory, National Center for Atmospheric Research, Boulder, CO, USA.
Nat Commun. 2022 Mar 3;13(1):1136. doi: 10.1038/s41467-022-28836-1.
Subseasonal weather prediction can reduce economic disruption and loss of life, especially during "windows of opportunity" when noteworthy events in the Earth system are followed by characteristic weather patterns. Sudden stratospheric warmings (SSWs), breakdowns of the winter stratospheric polar vortex, are one such event. They often precede warm temperatures in Northern Canada and cold, stormy weather throughout Europe and the United States - including the most recent SSW on January 5th, 2021. Here we assess the drivers of surface weather in the weeks following the SSW through initial condition "scrambling" experiments using the real-time CESM2(WACCM6) Earth system prediction framework. We find that the SSW itself had a limited impact, and that stratospheric polar vortex stretching and wave reflection had no discernible contribution to the record cold in North America in February. Instead, the tropospheric circulation and bidirectional coupling between the troposphere and stratosphere were dominant contributors to variability.
次季节天气预报可以减少经济破坏和生命损失,特别是在地球系统中值得关注的事件之后紧接着出现特征性天气模式的“机会窗口”期间。平流层突然增温(SSW),即冬季平流层极地涡旋的崩溃,就是这样一种事件。它们常常先于加拿大北部的温暖气温以及欧洲和美国各地的寒冷、暴风雨天气出现——包括2021年1月5日的最近一次平流层突然增温。在此,我们通过使用实时CESM2(WACCM6)地球系统预测框架的初始条件“扰频”实验,评估了平流层突然增温后数周地面天气的驱动因素。我们发现,平流层突然增温本身的影响有限,平流层极地涡旋伸展和波反射对2月北美创纪录的寒冷天气没有明显贡献。相反,对流层环流以及对流层与平流层之间的双向耦合是变率的主要贡献因素。