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<article language="en">
	<journal>
		<journal_title>Nonlinear Processes  in Geophysics</journal_title>
		<journal_url>www.nonlin-processes-geophys.net</journal_url>
		<issn>1023-5809</issn>
		<eissn>1607-7946</eissn>
		<volume_number>11</volume_number>
		<issue_number>3</issue_number>
		<publication_year>2004</publication_year>
	</journal>
	<doi>10.5194/npg-11-295-2004</doi>
	<article_url>http://www.nonlin-processes-geophys.net/11/295/2004/</article_url>
	<abstract_html>http://www.nonlin-processes-geophys.net/11/295/2004/npg-11-295-2004.html</abstract_html>
	<fulltext_pdf>http://www.nonlin-processes-geophys.net/11/295/2004/npg-11-295-2004.pdf</fulltext_pdf>
	<start_page>295</start_page>
	<end_page>301</end_page>
	<publication_date>2004-06-18</publication_date>
	<article_title content_type="html">Atmospheric teleconnection patterns and eddy kinetic energy content: wavelet analysis</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>V. N. Khokhlov</name>
		</author>
		<author numeration="2" affiliations="2">
			<name>A. V. Glushkov</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>I. A. Tsenenko</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Hydrometeorological Institute, OSEU, Odessa, Ukraine</affiliation>
		<affiliation numeration="2" content_type="html">Innovative Geosciences Research Centre and Institute of Applied Mathematics, OSEU, Odessa, Ukraine</affiliation>
	</affiliations>
	<abstract content_type="html">In this paper, we employ a non-decimated wavelet decomposition to analyse
long-term variations of the teleconnection pattern monthly indices (the
North Atlantic Oscillation and the Southern Oscillation) and the
relationship of these variations with eddy kinetic energy contents
(&lt;i&gt;K&lt;sub&gt;E&lt;/sub&gt;&lt;/i&gt;) in the atmosphere of mid-latitudes and tropics. Major advantage of
using this tool is to isolate short- and long-term components of
fluctuations. Such analysis allows revealing basic periodic behaviours for
the North Atlantic Oscillations (NAO) indices such as the 4-8-year and the
natural change of dominant phase. The main results can be posed as follows.
First, if the phases of North Atlantic and Southern Oscillations vary
synchronously with the 4-8-year period then the relationship between the
variations of the NAO indices and the &lt;i&gt;K&lt;sub&gt;E&lt;/sub&gt;&lt;/i&gt; contents is the most
appreciable. Second, if the NAO phase tends to abrupt changes then the
impact of these variations on the eddy kinetic energy contents in both
mid-latitudes and tropics is more significant than for the durational
dominance of certain phase.</abstract>
	<references>
	</references>
</article>

