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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ACPD</journal-id>
<journal-title-group>
<journal-title>Atmospheric Chemistry and Physics Discussions</journal-title>
<abbrev-journal-title abbrev-type="publisher">ACPD</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7375</issn>
<publisher><publisher-name>Copernicus GmbH</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acpd-11-31067-2011</article-id>
<title-group>
<article-title>Measurements of the movement of the jet streams at mid-latitudes, in the Northern and Southern Hemispheres, 1979 to 2010</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Hudson</surname>
<given-names>R. D.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Departament of Atmospheric and Oceanic Science, University of Maryland, College Park, MD, 20742–2425, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>22</day>
<month>11</month>
<year>2011</year>
</pub-date>
<volume>11</volume>
<issue>11</issue>
<fpage>31067</fpage>
<lpage>31090</lpage>
<permissions>
<license xlink:type="simple">
<license-p>This is an open-access article ditributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.</license-p>
</license>
</permissions>
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<abstract>
<p>Previous studies have shown that the mean latitude of the subtropical jet
streams in both hemispheres have shifted toward the poles over the last few
decades. This paper presents a study of the movement of both the subtropical
and Polar fronts, the location of the respective jet streams, between 1979
and 2010 at mid-latitudes, using total ozone measurements to identify the
sharp horizontal boundary that occurs at the position of the fronts. Previous
studies have shown that the two fronts are the boundaries of three distinct
regimes in the stratosphere, corresponding to the Hadley. Ferrel, and Polar
meridionally overturning circulation cells in the troposphere, each of which
has a distinct temperature profile. Over the period of study the horizontal
area of the Hadley cell has increased at latitudes between 20 and 60 degrees
while the area of the Polar cell has decreased. A linear regression analysis
was performed to identify the major factors associated with the movement of
the subtropical jet streams. These were: (1) changes in the Tropical
land/ocean temperature, (2) direct radiative forcing from greenhouse gases in
the troposphere, (3) changes in the temperature of the lower Tropical
stratosphere, (4) the Quasi-Biennial Oscillation, and (5) volcanic eruptions.
The dominant mechanism was the direct radiative forcing from greenhouse
gases. Over the period of study the poleward movement of the subtropical jet
streams was 3.7&amp;plusmn;0.3 degrees in the Northern Hemisphere and 6.5&amp;plusmn;0.2 degrees in the Southern Hemisphere, with a net expansion of the
Tropical belt of 10.2 degrees. Previous studies have shown that weather
systems tend to follow the jet streams. The observed poleward movement in
both hemispheres over the past thirty years represents a significant change
in the position of the subtropical jet streams, which should lead to
significant latitudinal shifts in the global weather patterns, temperatures,
precipitation and the hydrologic cycle.</p>
</abstract>
<counts><page-count count="24"/></counts>
</article-meta>
</front>
<body/>
<back>
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</article>