Skip to main content

ETHNOS_APP

Home • Search • Journals • List 0

Recent weakening of the southern stratospheric polar vortex and its impact on the surface climate over Antarctica

Bibliographic Data

ID15547817
AuthorsHataek Kwon (0000-0002-3856-6080, Seoul National University), Hyesun Choi (0000-0002-9298-9148, Korea Polar Research Institute), Baek‐Min Kim (0000-0002-1717-183X, Pukyong National University, corresponding author), Sang‐Woo Kim (0000-0002-0079-5806, Seoul National University, corresponding author), Sang-Woo Kim (0000-0002-6963-9393), Seong‐Joong Kim (0000-0002-6232-8082, Seoul National University, corresponding author)
Year2020
Volume15
Issue9
Pages094072-094072
Publication date2020-06-16
Open AccessYes
TypeARTICLE
VenueEnvironmental Research Letters (JOURNAL)
Journal identifiersISSN: 1748-9326 • E-ISSN: 1748-9326
PublisherIOP Publishing (PUBLISHER • GB)
DOI10.1088/1748-9326/ab9d3d
OpenAlexW3036601493
LanguageEN
References cited26

The variability in the southern stratospheric polar vortex (SSPV) and its downward coupling with the troposphere are known to play a crucial role in driving climate variability over Antarctica.In this study, SSPV weakening events and their impacts on the surface climate of Antarctica are examined using in-situ observation and reanalysis data.Combining criteria from several previous studies, we introduce a new detection method for SSPV weakening events.Based on the new criteria, the occurrence frequency of SSPV weakening events has exhibited a systematic increasing trend since the 2000 s.However, the weakened anomalies of individual SSPV events are not statistically different (95% confidence level) between the earlier and later (2000)(2001)(2002)(2003)(2004)(2005)(2006)(2007)(2008)(2009)(2010)(2011)(2012)(2013)(2014)(2015)(2016)(2017) periods examined in this study.The recent increase in the occurrence of SSPV weakening events is largely controlled by tropospheric mechanisms, i.e. the poleward heat flux carried by southern hemispheric planetary waves and associated vertical wave propagation.Among the various scales of planetary waves, the wavenumber 1 contributes most of the poleward eddy heat flux.We show that SSPV weakening events induce statistically significant cooling over the Antarctic Peninsula (AP) region and warming over the rest of Antarctica.Typically, surface air temperature anomalies with large negative values smaller than -0.6 C and positive values larger than + 0.8 C are observed over the east coast of the tip of the AP and King Edward VII Land, respectively.The influence of an SSPV weakening event on the surface lasts for approximately three months with higher height anomalies off western Antarctica, providing favorable conditions for the atmosphere to transport cold air from the interior of Antarctica to the AP via the Weddell Sea.Distinct positive surface air temperature anomalies over the rest of Antarctica are associated with the northerly circulation anomaly from the eastern Weddell Sea to east Antarctica

Atmospheric sciences · Climate change · Climate model · Climatology · Flux (metallurgy · Geography · Meteorology · Peninsula · Physics · Polar · Polar vortex · Troposphere · Vortex · Atmospheric and Environmental Gas Dynamics · Atmospheric Ozone and Climate · Climate variability and models · Environmental Science · Geology · Oceanography

  • The ERA‐Interim reanalysis

    Open Access•Dick Dee, D P Dee et al.•Quarterly Journal of the Royal…•2011

Highly citedNo

Tools

Open DOIOpen Access
Ethnos_APP • Open Source Project • MIT License • Frontend v2.0.0 • Privacy and Cookies • API Documentation: api.ethnos.app/docs • API Source Code: GitHub • DOI: 10.5281/zenodo.17049435 • Frontend Source Code: GitHub • DOI: 10.5281/zenodo.17050053 • cruz.rio.br • Expectantes Misericordiae