<?xml version="1.0" encoding="UTF-8"?>
<collection>
<dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:invenio="http://invenio-software.org/elements/1.0" 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:identifier>doi:10.1155/2019/4763450</dc:identifier><dc:language>eng</dc:language><dc:creator>Abadias, L.</dc:creator><dc:creator>Miana, P.J.</dc:creator><dc:title>Quasigeostrophic Equations for Fractional Powers of Infinitesimal Generators</dc:title><dc:identifier>ART-2019-111273</dc:identifier><dc:description>In this paper we treat the following partial differential equation, the quasigeostrophic equation: d / dt + u ·  grad f = - s - A a f, 0 = a = 1, where (A, D (A)) is the infinitesimal generator of a convolution C 0 -semigroup of positive kernel on L p (R n), with 1 = p &lt; 8. Firstly, we give remarkable pointwise and integral inequalities involving the fractional powers (- A) a for 0 = a = 1. We use these estimates to obtain L p -decayment of solutions of the above quasigeostrophic equation. These results extend the case of fractional derivatives (taking A = ¿, the Laplacian), which has been studied in the literature.</dc:description><dc:date>2019</dc:date><dc:source>http://zaguan.unizar.es/record/78935</dc:source><dc:doi>10.1155/2019/4763450</dc:doi><dc:identifier>http://zaguan.unizar.es/record/78935</dc:identifier><dc:identifier>oai:zaguan.unizar.es:78935</dc:identifier><dc:relation>info:eu-repo/grantAgreement/ES/DGA/E26-17R</dc:relation><dc:relation>info:eu-repo/grantAgreement/ES/MINECO/MTM2016-77710-P</dc:relation><dc:identifier.citation>Journal of Function Spaces 2019, 4763450  (2019), [7 pp]</dc:identifier.citation><dc:rights>by</dc:rights><dc:rights>http://creativecommons.org/licenses/by/3.0/es/</dc:rights><dc:rights>info:eu-repo/semantics/openAccess</dc:rights></dc:dc>

</collection>