<?xml version='1.0' encoding='utf-8'?>
<?xml-stylesheet type="text/xsl" href="/v2/static/oai2.xsl"?>
<OAI-PMH xmlns="http://www.openarchives.org/OAI/2.0/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd">
  <responseDate>2026-09-19T06:32:21Z</responseDate>
  <request identifier="oai:figshare.com:article/31211725" metadataPrefix="oai_dc" verb="GetRecord">https://api.figshare.com/v2/oai</request>
  <GetRecord>
    <record>
      <header>
        <identifier>oai:figshare.com:article/31211725</identifier>
        <datestamp>2026-02-02T12:52:47Z</datestamp>
        <setSpec>portal_1132</setSpec>
        <setSpec>item_type_8</setSpec>
        <setSpec>month_year_02_2026</setSpec>
      </header>
      <metadata>
        <oai_dc:dc xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance"  xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:dc="http://purl.org/dc/elements/1.1/" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
          <dc:title>Far-flung influences on midlatitude weather and climate: The stratospheric pathway</dc:title>
          <dc:creator>Regan Mudhar (21061334)</dc:creator>
          <dc:subject>Atmospheric dynamics</dc:subject>
          <dc:subject>Stratosphere</dc:subject>
          <dc:subject>Polar climate</dc:subject>
          <dc:subject>Climate change</dc:subject>
          <dc:subject>Energy sector</dc:subject>
          <dc:description>The variability of the Northern Hemisphere stratospheric polar vortex can significantly
influence, and enhance the predictability of, midlatitude winter weather on timescales
of weeks to months – including the likelihood of weather extremes and associated
impacts. This thesis first explores the response of the polar vortex to projected Arctic
climate change, in terms of both the mean state and variability, before focusing on
the impact of sudden stratospheric warmings (SSWs) on European energy demand.
The “stratospheric pathway” proposed to link Arctic sea-ice loss to changes in
midlatitude weather and climate is not well understood; studies do not so far find a
robust stratospheric response to sea-ice loss in either strength or sign. A series of
idealised model simulations is first used to show that the stratospheric response is
sensitive to characteristics of the near-surface Arctic warming and mean state of the
vortex. Then, a novel analysis of the stratospheric response with thirteen complex
atmospheric models is conducted, looking beyond the typical time- and zonal-mean
diagnostics. Though this analysis confirms the lack of robust response, the possible
role of ensemble size, resolution, and stratospheric basic state to explain the range
of simulated responses is explored. In both, the stratospheric response is also found
to play a role in the magnitude of the tropospheric jet response.
Finally, the contribution of SSWs to extreme European energy events is inves-
tigated. Reanalysis-derived variables indicate that extreme high energy demand
across northern and central Europe is historically more likely and severe following
such events. Stratospheric nudging experiments in seven seasonal forecast models
then enable specific attribution of energy extremes to the occurrence of the 2018
SSW. The results indicate a notable dependence on the lead time and nudging
methodology in the relative risk of extremes.&lt;p&gt;&lt;/p&gt;</dc:description>
          <dc:date>2026-02-02T00:00:00Z</dc:date>
          <dc:type>Text</dc:type>
          <dc:type>Thesis</dc:type>
          <dc:identifier>10779/exe.31211725.v1</dc:identifier>
          <dc:relation>https://figshare.com/articles/thesis/Far-flung_influences_on_midlatitude_weather_and_climate_The_stratospheric_pathway/31211725</dc:relation>
          <dc:rights>All rights reserved</dc:rights>
          <dc:rights>Open Access after 2027-02-02</dc:rights>
        </oai_dc:dc>
      </metadata>
    </record>
  </GetRecord>
</OAI-PMH>
