Asikainen, T., Salminen, A., Maliniemi, V., & Mursula, K. ( 2020). Influence of enhanced planetary wave activity on the polar vortex enhancement related to energetic electron precipitation. Journal Geophysical Research: Atmospheres, 125, e2019JD032137. https://doi.org/10.1029/2019JD032137
Influence of enhanced planetary wave activity on the polar vortex enhancement related to energetic electron precipitation
|Author:||Asikainen, Timo1; Salminen, Antti1; Maliniemi, Ville2;|
1Space Physics and Astronomy Research Unit, University of Oulu, Oulu, Finland
2Centre for Space Science, Department of Physics and Technology, University of Bergen, Bergen, Norway
|Online Access:||PDF Full Text (PDF, 2.9 MB)|
|Persistent link:|| http://urn.fi/urn:nbn:fi-fe2020050424883
American Geophysical Union,
|Publish Date:|| 2020-05-04
The Northern polar vortex experiences considerable interannual variability, which is also reflected to tropospheric weather. Recent research has established a link between polar vortex variations and energetic electron precipitation (EEP) from the near‐Earth space into the polar atmosphere, which is mediated by EEP‐induced chemical changes causing ozone loss in the mesosphere and stratosphere. The most dramatic changes in the polar vortex are due to sudden stratospheric warmings (SSWs). Enhanced planetary wave convergence and meridional circulation may cause an SSW, a temporary breakdown of the polar vortex. Here we study the relation of SSWs to the atmospheric response to EEP in 1957–2017 using combined ERA‐40 and ERA‐Interim reanalysis data and geomagnetic activity as a proxy of EEP. We find that the EEP‐related enhancement of the polar vortex and other associated dynamical responses are seen only during winters when an SSW occurs and that the EEP‐related changes are observed systematically slightly before the SSW onset.
We show that during these times, the planetary wave activity into the stratosphere is systematically increased, thus favoring enhanced wave‐mean‐flow interaction, which can dynamically amplify the initial polar vortex enhancement caused by ozone loss. These results highlight the importance of considering planetary wave activity as a necessary condition for observing the effects of EEP on the polar vortex.
Journal of geophysical research. Atmospheres
|Type of Publication:||
A1 Journal article – refereed
|Field of Science:||
114 Physical sciences
115 Astronomy and space science
We acknowledge the financial support by the Academy of Finland to the ReSoLVE Center of Excellence (Project 307411) and to the PRediction of SPace climate and its Effects in ClimaTe (PROSPECT, Project 321440) research project. We also acknowledge the financial support by the Kvantum Institute of the University of Oulu for the Climate and Atmospheric Effects of Sun in Arctic Regions (CAESAR) project.
|Academy of Finland Grant Number:||
307411 (Academy of Finland Funding decision)
321440 (Academy of Finland Funding decision)
The atmospheric data used in this study are available from the European Centre for Medium Range Weather Forecasts (ECMWF) at http://apps.ecmwf.int/datasets/. The geomagnetic Ap index data can be obtained from International Service of Geomagnetic Indices at http://isgi.unistra.fr.
©2020. The Authors. This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited.