| Summary: | Trabajo presentado en la European Geosciences Union General Assembly, celebrada en Viena (Austria), del 8 al 13 de abril de 2018 Stratospheric final warmings (SFWs) mark the final transition from the typical wintertime westerlies to summertime easterlies at high latitudes in the stratosphere. They occur in both hemispheres, but, due to the enhanced planetary wave activity, these events present a high inter-annual variability in the Northern Hemisphere. In particular, SFWs onset dates oscillate in a range of about two months and SFWs show different vertical temporal developments, i.e. events may occur first in the mid-stratosphere (10-hPa first SFWs) or in the upper stratosphere (1-hPa first SFWs). This variability has been shown to impact the polar ozone depletion, but also the tropospheric circulation, particularly over the North Atlantic sector. Thus, it is important to identify factors that influence SFW variability. However, most of the previous studies were essentially based on reanalysis data and so, the length of observations is relatively short to derive robust conclusions. In this study, we aim to improve the understanding of drivers, trends and surface impact of dynamical variability of boreal SFWs. To do this, we use multi-decadal integrations (145 years) of a fully coupled chemistry-climate model (CESM1(WACCM)) that ensure a large statistical sampling. Four sensitivity experiments are also analyzed to assess the impact of external factors such as quasi-biennial oscillation (QBO), sea surface temperature (SST) variability and anthropogenic emissions. Our results confirm previous reanalysis results regarding the differences in the time evolution of stratospheric conditions and surface impact between 10-hPa and 1-hPa first SFWs. Additionally, a tripolar SST pattern is, for the first time, identified over the North Atlantic in spring months related to the SFW variability. The analysis of the influence of remote modulators on SFWs revealed that the occurrence of stratospheric sudden warmings in the ...
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