Observation, Prediction, Simulation, and Future Projections of Sudden Stratospheric Warming and Its Impact

A special issue of Atmosphere (ISSN 2073-4433). This special issue belongs to the section "Climatology".

Deadline for manuscript submissions: closed (7 November 2022) | Viewed by 2023

Special Issue Editors

School of Atmospheric Science, Nanjing University of Information Science and Technology, Nanjing 210044, China
Interests: sudden stratospheric warming; quasi-biennial oscillation; stratosphere-troposphere coupling; air-sea interaction; global change
School of Atmospheric Sciences, Nanjing University, Nanjing 210023, China
Interests: general circulation of the atmosphere; stratosphere-troposphere dynamical coupling; tropical-extratropical teleconnections; ocean-atmosphere interactions and East Asian Monsoon
China Meteorological Administration, Earth System Modeling and Prediction Centre (CEMC), Beijing 100081, China
Interests: middle-atmosphere modeling; gravity wave parameterization; subgrid-scale orographic drag; stratosphere-troposphere interaction; sudden stratospheric warming; stratospheric final warming; stratospheric quasi-biennial oscillation; Brewer-Dobson circulation; stratospheric polar vortex

Special Issue Information

Dear Colleagues,

As one of the most radical phenomena in the climate system, sudden stratospheric warming (SSW) mainly occurs in the Northern Hemisphere in midwinter, when the Arctic stratosphere warms by tens of degrees within a week. SSWs and some early find warmings (SFWs) are a period of strong stratosphere-troposphere coupling, and the negative northern annular mode (NAM) signal associated with SSWs and SFWs can propagate downward from the stratosphere to the troposphere, which possibly increases the possibility of the continental cold surge and its predictability on the sub-seasonal to seasonal timescale. One recent example is the persistent continental cold surge in Eurasia and North America following the January 2021 SSW. Due to the possible downward impact of SSWs, their predictability has attracted wide attention in the community in past years. Further, underrepresentation of SSWs is still a common bias for some CMIP5/6 models, which partially contributes to uncertainty in the future projection of SSWs. Divergence still exists in the literature for the projected future change in the frequency, intensity, and possible near-surface impact of SSWs. As some SSWs were observed in the Southern Hemisphere in spring, a possible impact of SSWs in the Southern Hemisphere also rouses wide interest. However, it is still unknown what the (especially the minor) SSW in the Southern Hemisphere will change in the future. Due to those limitations of SSW studies, we are pleased to announce the Special Issue “Observation, Prediction, Simulation and Future Projection of Sudden Stratospheric Warming and Its Impact”.

Manuscripts solicited for this Special Issue are in research areas including, but not limited to, the following topics:

  • Observational characteristics of SSWs in both hemispheres in reanalysis and satellite datasets;
  • The possible impact of SSWs on regional rainfall (drought and flood), near-surface temperature (cold surge and heat wave), and PM2.5 concentration;
  • Case or composite studies of the SSW predictability using sub-seasonal to seasonal (S2S) reforecasts/forecasts;
  • The reproducibility of the stratospheric polar vortex and SSWs in some individual models or multiple models from a series of CMIPs, especially the most recent CMIP6;
  • Possible changes and future projection of SSW’s impacts.

Other topics related to stratospheric dynamics, physics (especially radiation), and chemistry are also welcome.

Dr. Jian Rao
Dr. Ming Bao
Dr. Yixiong Lu
Guest Editors

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Keywords

  • sudden stratospheric warming (SSW)
  • sub-seasonal to seasonal (S2S) forecasts
  • CMIP5/6
  • model simulation
  • future projection

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Published Papers (1 paper)

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Research

17 pages, 4228 KiB  
Article
Simulation of Northern Winter Stratospheric Polar Vortex Regimes in CESM2-WACCM
by Dong Guo, Zhuoqi Liang, Qiang Gui, Qian Lu, Qiong Zheng and Shuyang Yu
Atmosphere 2023, 14(2), 243; https://doi.org/10.3390/atmos14020243 - 26 Jan 2023
Viewed by 1513
Abstract
The possible impact of various Arctic polar vortex regimes for the stratosphere on the Northern Hemisphere extratropics has not been fully understood. Previous study has classified the stratospheric Arctic vortex to six regimes using the k-mean clustering algorithm based on the ERA5 reanalysis. [...] Read more.
The possible impact of various Arctic polar vortex regimes for the stratosphere on the Northern Hemisphere extratropics has not been fully understood. Previous study has classified the stratospheric Arctic vortex to six regimes using the k-mean clustering algorithm based on the ERA5 reanalysis. The stability and robustness of the classification is further verified with a much longer model dataset and historical integrations from CESM2-WACCM. Consistent with the reanalysis, we clustered the Arctic stratospheric polar vortex forms into six patterns, named as homogeneously-intensified and -weakened regimes (HI, HW), North America-intensified and -weakened regimes (NAI, HAW), and Eurasia-intensified and -weakened regimes (EUI, EUW). A zonally uniform positive (negative) Northern Annular Mode (NAM) pattern develops during the HI (HW) regime from the stratosphere to troposphere. The NAM-like pattern shifts toward the western hemisphere with the largest negative (positive) anomalous height center shifting to North America during the NAI (NAW) regime. In contrast, the maximum polar anomaly center moves towards polar Eurasia during the EUI (EUW) regime. The HI, NAI, and EUW regimes are accompanied with weakened wave activities, while the HW, NAW, and EUI regimes are preceded by enhanced planetary waves. Accordingly, persistent anomalies of warmth (coldness) exist over midlatitude Eurasia and North America during the HI (HW). Anomalous warmth (coldness) centers exist in northern Eurasia, while anomalous coldness (warmth) centers exist around the Mediterranean Sea during the NAI (NAW) regime. Anomalous warmth (coldness) centers develop in East Asia in the EUI (EUW) periods. The rainfall anomaly distributions also vary with the stratospheric polar vortex regime. The frequency for stratospheric regimes during SSWs and strong vortex events is also assessed and consistent with previous findings. Full article
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