{"id":9463,"date":"2023-01-11T15:19:40","date_gmt":"2023-01-11T15:19:40","guid":{"rendered":"https:\/\/www.istp.cnr.it\/?post_type=product&#038;p=9463"},"modified":"2023-02-03T10:42:05","modified_gmt":"2023-02-03T10:42:05","slug":"exact-shearing-flow-magnetized-hybrid-kinetic-equilibria-with-inhomogeneous-temperature","status":"publish","type":"product","link":"https:\/\/www.istp.cnr.it\/it\/research-product\/exact-shearing-flow-magnetized-hybrid-kinetic-equilibria-with-inhomogeneous-temperature\/","title":{"rendered":"Exact Shearing Flow Magnetized Hybrid Kinetic Equilibria with Inhomogeneous Temperature"},"content":{"rendered":"<p>Magnetized plasmas with shearing flows are found in many natural contexts, such as around Earth&#8217;s magnetopause. In collisionless plasmas where physical quantities vary on a scale of the order of or larger than ion scales, the hybrid Vlasov-Maxwell description (kinetic ions coupled to a neutralizing electron fluid via electromagnetic fields) represents a suitable approach. When crossing the magnetopause, the ion temperature, density, and direction of magnetic field vary. We derive a form for an exact stationary solution of the hybrid Vlasov-Maxwell equations that represent a magnetized plasma with a quasi-planar shearing flow, variable density and ion temperature, and variable magnetic field direction. A stationary ion distribution function is expressed as a suitable combination of particle constants of motion and evaluated numerically in such a way to obtain configurations with variable density and temperature and two quasi-planar oppositely directed velocity shear layers. Properties of particular configurations are derived from Magnetospheric Multiscale measures during crossings of Earth&#8217;s magnetopause. In the first case a quasi-uniformly directed, nearly perpendicular magnetic field is present, while in the second case, going from the magnetosheath to the magnetosphere, the magnetic field makes a wide rotation from one side to the other of the shearing flow plane. In both cases, the ion distribution function departs from a Maxwellian in the shear layers, displaying temperature anisotropy and agyrotropy, with a nonsymmetric behavior in the two shear layers. The configurations considered here can be used as models for Earth&#8217;s magnetopause in simulations of the Kelvin-Helmholtz instability.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Malara F.; Settino A.; Perrone D.; Pezzi O.; Guzzi G.; Valentini F.<\/p>\n","protected":false},"featured_media":1294,"comment_status":"closed","ping_status":"open","template":"","meta":[],"product_cat":[574],"product_tag":[714,2036,2071],"class_list":["post-9463","product","type-product","status-publish","has-post-thumbnail","hentry","product_cat-journal-articles","product_tag-plasma-physics","product_tag-interplanetary-magnetic-fields","product_tag-heliosphere","prodpage-style2"],"acf":[],"_links":{"self":[{"href":"https:\/\/www.istp.cnr.it\/it\/wp-json\/wp\/v2\/product\/9463","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.istp.cnr.it\/it\/wp-json\/wp\/v2\/product"}],"about":[{"href":"https:\/\/www.istp.cnr.it\/it\/wp-json\/wp\/v2\/types\/product"}],"replies":[{"embeddable":true,"href":"https:\/\/www.istp.cnr.it\/it\/wp-json\/wp\/v2\/comments?post=9463"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/www.istp.cnr.it\/it\/wp-json\/wp\/v2\/media\/1294"}],"wp:attachment":[{"href":"https:\/\/www.istp.cnr.it\/it\/wp-json\/wp\/v2\/media?parent=9463"}],"wp:term":[{"taxonomy":"product_cat","embeddable":true,"href":"https:\/\/www.istp.cnr.it\/it\/wp-json\/wp\/v2\/product_cat?post=9463"},{"taxonomy":"product_tag","embeddable":true,"href":"https:\/\/www.istp.cnr.it\/it\/wp-json\/wp\/v2\/product_tag?post=9463"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}