<oai_dc:dc xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
<dc:title>Critical thresholds in Euler-Poisson equations</dc:title>
<dc:creator>Shlomo Engelberg</dc:creator><dc:creator>Hongyu Liu</dc:creator><dc:creator>Eitan Tadmor</dc:creator>
<dc:subject>35Q35</dc:subject><dc:subject>35B30</dc:subject><dc:subject>Euler-Poisson equations</dc:subject><dc:subject>critical threshold</dc:subject><dc:subject>breakdown</dc:subject><dc:subject>global existence</dc:subject><dc:subject>isotropic flow</dc:subject>
<dc:description>We present a preliminary study of a new phenomena associated with the Euler-Poisson equations --- the so called critical threshold phenomena, where the answer to questions of global smoothness vs. finite time breakdown depends on whether the initial configuration crosses an intrinsic, $O(1)$ critical threshold.\par We investigate a class of Euler-Poisson equations, ranging from one-dimensional problems with or without various forcing mechanisms to multi-dimensional isotropic models with geometrical symmetry. These models are shown to admit a critical threshold which is reminiscent of the conditional breakdown of waves on the beach; only waves above certain initial critical threshold experience finite-time breakdown, but otherwise they propagate smoothly. At the same time, the asymptotic long time behavior of the solutions remains the same, independent of crossing these initial thresholds.\par A case in point is the simple one-dimensional problem where the unforced inviscid Burgers solution always forms a shock discontinuity, except for the non-generic case of increasing initial profile, $u_0&#39; \geq 0$. In contrast, we show that the corresponding one-dimensional Euler-Poisson equation with zero background has global smooth solutions as long as its initial $(\rho_0, u_0)$-configuration satisfies $u_0&#39; \geq -\sqrt{2k\rho_0}$ -- see (1.1) below, allowing a finite, critical negative velocity gradient. As is typical for such nonlinear convection problems, one is led to a Ricatti equation which is balanced here by a forcing acting as a &#39;nonlinear resonance&#39;, and which in turn is responsible for this critical threshold phenomena.</dc:description>
<dc:publisher>Indiana University Mathematics Journal</dc:publisher>
<dc:date>2001</dc:date>
<dc:type>text</dc:type>
<dc:format>pdf</dc:format>
<dc:identifier>10.1512/iumj.2001.50.2177</dc:identifier>
<dc:source>10.1512/iumj.2001.50.2177</dc:source>
<dc:language>en</dc:language>
<dc:relation>Indiana Univ. Math. J. 50 (2001) 109 - 158</dc:relation>
<dc:coverage>state-of-the-art mathematics</dc:coverage>
<dc:rights>http://iumj.org/access/</dc:rights>
</oai_dc:dc>