Sudden Stratospheric Warmings
نویسندگان
چکیده
Sudden stratospheric warmings (SSWs) are impressive fluid dynamical events in which large and rapid temperature increases the winter polar stratosphere (∼10–50 km) associated with a complete reversal of climatological wintertime westerly winds. SSWs caused by breaking planetary-scale waves that propagate upwards from troposphere. During an SSW, vortex breaks down, accompanied descent warming air latitudes, mirrored ascent cooling above warming. The column affect tropospheric weather, shifting jet streams, storm tracks, Northern Annular Mode, making cold outbreaks over North America Eurasia more likely. atmosphere stratosphere, producing widespread effects on atmospheric chemistry, temperatures, winds, neutral (nonionized) particles electron densities, electric fields. These span both hemispheres. Given their crucial role whole atmosphere, also seen as key process to analyze climate change studies subseasonal seasonal prediction. This work reviews current knowledge most important aspects SSWs, historical background processes, modeling, impact other layers.
منابع مشابه
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ژورنال
عنوان ژورنال: Reviews of Geophysics
سال: 2021
ISSN: ['1944-9208', '8755-1209', '0034-6853', '0096-1043']
DOI: https://doi.org/10.1029/2020rg000708