{"id":7,"date":"2020-08-17T13:42:04","date_gmt":"2020-08-17T13:42:04","guid":{"rendered":"https:\/\/www.issibern.ch\/teams\/iosatmosphere\/?page_id=2"},"modified":"2025-03-13T07:20:59","modified_gmt":"2025-03-13T07:20:59","slug":"sample-page","status":"publish","type":"page","link":"https:\/\/www.issibern.ch\/teams\/iosatmosphere\/","title":{"rendered":"Overview &#8211; what is this about?"},"content":{"rendered":"<h1>Review paper published!<\/h1>\n<p>The review paper that resulted from the discussions and work during our two meetings is finally published: <a href=\"https:\/\/doi.org\/10.1007\/s11214-025-01137-x\">https:\/\/doi.org\/10.1007\/s11214-025-01137-x<\/a>.<br \/>\nIf you have questions, do not hesitate to contact me (Lorenz) or any of the authors!<\/p>\n<h1><span style=\"font-size: 14pt\">Background<\/span><\/h1>\n<p>The atmospheric loss from the moon Io is the main source of material for the vast magnetosphere of our largest Solar System planet Jupiter. Io is also the volcanically most active body in the Solar System and the volcanism plays a key role for sustaining the moon\u2019s atmosphere. Within the magnetosphere and plasma community, it is therefore very <strong><em>often assumed that aperiodic changes or transient phenomena in Jupiter\u2019s magnetosphere are triggered by sudden and strong changes in the mass loss from Io<\/em><\/strong>, supposedly related to volcanic outbursts. The magnetospheric effects \u2013 presumably arising from Io\u2019s volcanism \u2013 have been topic of an earlier ISSI team (ID 388).<\/p>\n<h1><span style=\"font-size: 14pt\">Contradictory understandings and missing evidence<\/span><\/h1>\n<p>The assumption of direct \u201cvolcanic control\u201d of the magnetosphere is, however, <em><strong>neither supported by the current understanding of the dynamics of Io\u2019s atmosphere, nor by observations of the atmospheric abundance<\/strong><\/em>. Io\u2019s atmosphere has been found to be primarily sustained by sublimation of surface frost and to a lesser extent by direct outgassing at volcanoes. The atmospheric loss is predominantly through collisions with the surrounding plasma and not through direct thermal escape. Changes in volcanic activity are thus not expected to lead to strong changes in the atmospheric density or loss rate. Furthermore, observational monitoring of the atmospheric gas column density has not provided any evidence for sudden changes but only revealed seasonal atmospheric variability. On the other hand, there are so far no alternative explanations for the observed magnetospheric changes from studies claiming \u201cvolcanic control\u201d. And some correlations indeed point to Io as the trigger.<\/p>\n<h1><span style=\"font-size: 14pt\">Task for a team!<\/span><\/h1>\n<p>In order to address the issue of these allegedly contradictory understandings of the variability of Io\u2019s mass loss, we gathered an <a href=\"https:\/\/www.issibern.ch\/teams\/iosatmosphere\/index.php\/team\/\">international team<\/a> with <strong><em>leading experts in the areas of Io\u2019s volcanism, atmosphere and the magnetospheric environment<\/em><\/strong>. While this topic is very defined, the Io-Jupiter system is <em>the <\/em>prime example for various geophysical and plasma physical processes; a correct understanding of Io\u2019s role is crucial, far beyond Jupiter and the Solar System.<\/p>\n<p>If you want to know more or are interested in contributing to this effort, please contact Lorenz Roth (via lorenzr at kth.se)!<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Review paper published! The review paper that resulted from the discussions and work during our two meetings is finally published: https:\/\/doi.org\/10.1007\/s11214-025-01137-x. If you have questions, do not hesitate to contact me (Lorenz) or any of the authors! Background The atmospheric &hellip; <a href=\"https:\/\/www.issibern.ch\/teams\/iosatmosphere\/\">Continue reading <span class=\"meta-nav\">&rarr;<\/span><\/a><\/p>\n","protected":false},"author":2,"featured_media":47,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-7","page","type-page","status-publish","has-post-thumbnail","hentry"],"_links":{"self":[{"href":"https:\/\/www.issibern.ch\/teams\/iosatmosphere\/wp-json\/wp\/v2\/pages\/7","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.issibern.ch\/teams\/iosatmosphere\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/www.issibern.ch\/teams\/iosatmosphere\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/www.issibern.ch\/teams\/iosatmosphere\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/www.issibern.ch\/teams\/iosatmosphere\/wp-json\/wp\/v2\/comments?post=7"}],"version-history":[{"count":4,"href":"https:\/\/www.issibern.ch\/teams\/iosatmosphere\/wp-json\/wp\/v2\/pages\/7\/revisions"}],"predecessor-version":[{"id":108,"href":"https:\/\/www.issibern.ch\/teams\/iosatmosphere\/wp-json\/wp\/v2\/pages\/7\/revisions\/108"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/www.issibern.ch\/teams\/iosatmosphere\/wp-json\/wp\/v2\/media\/47"}],"wp:attachment":[{"href":"https:\/\/www.issibern.ch\/teams\/iosatmosphere\/wp-json\/wp\/v2\/media?parent=7"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}