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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>12</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2005</publication_year>
	</journal>
	<doi>10.5194/npg-12-75-2005</doi>
	<article_url>http://www.nonlin-processes-geophys.net/12/75/2005/</article_url>
	<abstract_html>http://www.nonlin-processes-geophys.net/12/75/2005/npg-12-75-2005.html</abstract_html>
	<fulltext_pdf>http://www.nonlin-processes-geophys.net/12/75/2005/npg-12-75-2005.pdf</fulltext_pdf>
	<start_page>75</start_page>
	<end_page>81</end_page>
	<publication_date>2005-01-25</publication_date>
	<article_title content_type="html">Modeling of short scale turbulence in the solar wind</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>V. Krishan</name>
		</author>
		<author numeration="2" affiliations="2">
			<name>S. M. Mahajan</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Indian Institute of Astrophysics, Bangalore 560 034, India</affiliation>
		<affiliation numeration="2" content_type="html">Institute for Fusion Studies, The University of Texas at Austin, Austin, Texas 78712, USA</affiliation>
	</affiliations>
	<abstract content_type="html">The solar wind serves as a laboratory for investigating
magnetohydrodynamic turbulence under conditions irreproducible on the terra
firma. Here we show that the frame work of Hall magnetohydrodynamics (HMHD),
which can support three quadratic invariants  and allows nonlinear states to
depart fundamentally from the Alfv&amp;#233;nic, is capable of reproducing in the
inertial range the three branches of the observed solar wind magnetic
fluctuation spectrum - the Kolmogorov branch &lt;i&gt;f&lt;/i&gt;&lt;sup&gt; -5/3&lt;/sup&gt; steepening to
&lt;i&gt;f&lt;/i&gt;&lt;sup&gt; -&amp;alpha;&lt;sub&gt;1&lt;/sub&gt;&lt;/sup&gt; with &lt;!-- MATH
 $\alpha_1{\simeq}3{-}4$
 --&gt;
&lt;IMG WIDTH=&quot;61&quot; HEIGHT=&quot;29&quot; ALIGN=&quot;MIDDLE&quot; BORDER=&quot;0&quot;
  src=&quot;http://www.nonlin-processes-geophys.net/12/75/2005/npg-12-75-img3.gif&quot; 
 ALT=&quot;$alpha_1{simeq}3{-}4$&quot;&gt; on the high frequency side and
flattening to &lt;i&gt;f&lt;/i&gt;&lt;sup&gt; -1&lt;/sup&gt; on the low frequency side. These fluctuations are found
to be associated  with the nonlinear Hall-MHD Shear Alfv&amp;#233;n waves. The spectrum
of the concomitant whistler type fluctuations is  very different from  the
observed one. Perhaps the  relatively stronger damping of the whistler
fluctuations may  cause  their unobservability. The issue of equipartition of
energy through the so called Alfv&amp;#233;n ratio acquires a new status through its
dependence, now, on the spatial scale.</abstract>
	<references>
	</references>
</article>

