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1. The impact of split and displacement sudden stratospheric warmings on the troposphere

   https://doi.org/https://doi. org/10.1029/2020JD033989  

   White, I. P. ( April 2021 , Journal of geophysical research)

   null (Ed.)

   Although sudden stratospheric warmings (SSWs) can improve subseasonal-to-seasonal forecasts, it is unclear whether the two types of SSW - displacements and splits - have different near- surface effects. To examine the longer-term (i.e., multi-week lead) tropospheric response to displacements and splits, we utilize an intermediate-complexity model and impose wave-1 and wave-2 stratospheric heating perturbations spun-off from a control run. At longer lags, the tropospheric response is found to be insensitive to both the wavenumber and location of the imposed heating, in agreement with freely evolving displacements and splits identified in the control run. At shorter lags, however, large differences are found between displacements and splits in both the control run and the different wavenumber- forced events. In particular, in the control run, the free-running splits have an immediate barotropic response throughout the stratosphere and troposphere whereas displacements take 1–2 weeks before a near-surface response becomes evident. Interestingly, this barotropic response found during CTRL splits is not captured by the barotropically forced wave-2 events, indicating that the zonal-mean tropospheric circulation is somehow coupled with the generation of the wave-2 splits. It is also found that in the control run, displacements yield stronger Polar-Cap temperature anomalies than splits, yet both still yield similar magnitude tropospheric responses. Hence, the strength of the stratospheric warming is not the only governing factor in the surface response. Overall, SSW classification based on vortex morphology may be useful for subseasonal but not seasonal tropospheric prediction. 

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2. Stationary Waves Weaken and Delay the Near-Surface Response to Stratospheric Ozone Depletion

   https://doi.org/10.1175/JCLI-D-21-0874.1  

   Garfinkel, Chaim I. ; White, Ian ; Gerber, Edwin P. ; Son, Seok-Woo ; Jucker, Martin ( January 2023 , Journal of Climate)

   Abstract An intermediate-complexity moist general circulation model is used to investigate the factors controlling the magnitude of the surface impact from Southern Hemisphere springtime ozone depletion. In contrast to previous idealized studies, a model with full radiation is used; furthermore, the model can be run with a varied representation of the surface, from a zonally uniform aquaplanet to a configuration with realistic stationary waves. The model captures the observed summertime positive Southern Annular Mode response to stratospheric ozone depletion. While synoptic waves dominate the long-term poleward jet shift, the initial response includes changes in planetary waves that simultaneously moderate the polar cap cooling (i.e., a negative feedback) and also constitute nearly one-half of the initial momentum flux response that shifts the jet poleward. The net effect is that stationary waves weaken the circulation response to ozone depletion in both the stratosphere and troposphere and also delay the response until summer rather than spring when ozone depletion peaks. It is also found that Antarctic surface cooling in response to ozone depletion helps to strengthen the poleward shift; however, shortwave surface effects of ozone are not critical. These surface temperature and stationary wave feedbacks are strong enough to overwhelm the previously recognized jet latitude/persistence feedback, potentially explaining why some recent comprehensive models do not exhibit a clear relationship between jet latitude/persistence and the magnitude of the response to ozone. The jet response is shown to be linear with respect to the magnitude of the imposed stratospheric perturbation, demonstrating the usefulness of interannual variability in ozone depletion for subseasonal forecasting. 

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3. Sudden Stratospheric Warmings

   https://doi.org/10.1029/2020RG000708  

   Baldwin, Mark P. ; Ayarzagüena, Blanca ; Birner, Thomas ; Butchart, Neal ; Butler, Amy H. ; Charlton‐Perez, Andrew J. ; Domeisen, Daniela I. V. ; Garfinkel, Chaim I. ; Garny, Hella ; Gerber, Edwin P. ; et al ( January 2021 , Reviews of Geophysics)

   Sudden stratospheric warmings (SSWs) are impressive fluid dynamical events in which large and rapid temperature increases in the winter polar stratosphere (∼10–50 km) are associated with a complete reversal of the climatological wintertime westerly winds. SSWs are caused by the breaking of planetary‐scale waves that propagate upwards from the troposphere. During an SSW, the polar vortex breaks down, accompanied by rapid descent and warming of air in polar latitudes, mirrored by ascent and cooling above the warming. The rapid warming and descent of the polar air column affect tropospheric weather, shifting jet streams, storm tracks, and the Northern Annular Mode, making cold air outbreaks over North America and Eurasia more likely. SSWs affect the atmosphere above the stratosphere, producing widespread effects on atmospheric chemistry, temperatures, winds, neutral (nonionized) particles and electron densities, and electric fields. These effects span both hemispheres. Given their crucial role in the whole atmosphere, SSWs are also seen as a key process to analyze in climate change studies and subseasonal to seasonal prediction. This work reviews the current knowledge on the most important aspects of SSWs, from the historical background to dynamical processes, modeling, chemistry, and impact on other atmospheric layers.

    

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4. Monthly mean Eliassen-Palm fluxes and EP flux divergences for boreal winter months (Dec-Jan-Feb) from 1979 to 2020 using ERA5 data

   https://doi.org/10.5281/zenodo.10140775  

   Du, Wenyuan ; Hitchman, Matthew ( January 2023 , Zenodo)

   The European Centre for Medium-range Weather Forecasting (ECMWF) Reanalysis v5 (ERA5) data set (1979 – 2020) is used in many climate studies.  The present monthly mean data set of Eliassen-Palm fluxes (EP fluxes) and EP flux divergences, was created from twice-daily gridded values of ERA5 winds and temperature on pressure surfaces and is intended to fill a gap in availability.   It is compatible for use with ERA5 monthly mean data.   The EP flux is a diagnostic tool for assessing wave propagation and wave-mean flow interaction. It is a vector representation for the propagation of synoptic and planetary Rossby wave activity in the meridional plane.  An upward component indicates a poleward heat flux while an equatorward component indicates a poleward momentum flux.   EP flux divergence implies a source of Rossby wave activity, and EP flux convergence implies absorption of Rossby wave activity.  EP flux divergence represents the body force, or net effect of waves on the zonal mean zonal wind, with EP flux convergence causing deceleration of zonal mean westerlies and EP flux divergence causing acceleration. The primary effect of a region of EP flux convergence, however, is to induce poleward motion, with an associated mean meridional circulation and quadrupole of temperature anomalies in the meridional plane. EP fluxes are useful in investigating many planetary and synoptic scale weather phenomena such as the Quasi-Biennial Oscillation (QBO) and Sudden Stratospheric Warmings (SSWs).   The meridional and vertical components of the EP flux are calculated in pressure coordinates using the following initial conditions:  Ground density (rho_0 ):P_0/R_0/T_0 Ground pressure (P_0): 1013hPa Ground temperature (T_0): Temperature at 1000hPa Earth radius (a) = 6378km   Dimensions in the data: Latitude: 90°N-90°S (grid spacing is 0.25°, as in the ERA5 reanalysis)  Pressure: 1 hPa-1000 hPa (levels are the same as in the ERA5 reanalysis)  Time: January 1979 – December 2020; December, January, February (DJF) only; 00z and 12z 

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5. On the Downward Progression of Stratospheric Temperature Anomalies Using Long‐Term SABER Observations

   https://doi.org/10.1029/2022JD036487  

   Thurairajah, Brentha ; Cullens, Chihoko Yamashita ( June 2022 , Journal of Geophysical Research: Atmospheres)

   It is well known that stratospheric sudden warmings (SSWs) are a result of the interaction between planetary waves (PWs) and the stratospheric polar vortex. SSWs occur when breaking PWs slow down or even reverse this zonal wind jet and induce a sinking motion that adiabatically warms the stratosphere and lowers the stratopause. In this paper we characterize this downward progression of stratospheric temperature anomalies using 18 years (2003–2020) of Sounding of the Atmosphere using Broadband Radiometry (SABER) observations. SABER temperatures, derived zonal winds, PW activity and gravity wave (GW) activity during January and February of each year indicate a high‐degree of year‐to‐year variability. From 11 stratospheric warming events (9 major and 2 minor events), the descent rate of the stratopause altitude varies from 0.5 to 2 km/day and the lowest altitude the stratopause descends to varies from <20 to ∼50 km (i.e., no descent). A composite analysis of temperature and squared GW amplitude anomalies indicate that the downward descent of temperature anomalies from 50 to ∼25 km lags the downward progression of increased GW activity. This increased GW activity coincides with the weakening and reversal of the westward zonal winds in agreement with previous studies. Our study suggests that although PWs drive the onset of SSWs at 30 km, GWs also play a role in contributing to the descent of temperature anomalies from the stratopause to the middle and lower stratosphere.

    

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