{"id":2919,"date":"2013-10-29T13:22:55","date_gmt":"2013-10-29T20:22:55","guid":{"rendered":"https:\/\/blogschapman.wpenginepowered.com\/scst\/2013\/10\/29\/ceesmo-science-lecture\/"},"modified":"2013-10-29T13:22:55","modified_gmt":"2013-10-29T20:22:55","slug":"ceesmo-science-lecture","status":"publish","type":"post","link":"https:\/\/blogs.chapman.edu\/scst\/2013\/10\/29\/ceesmo-science-lecture\/","title":{"rendered":"CEESMO Science Lecture"},"content":{"rendered":"<p>You are invited to attend a CEESMO science lecture by Visiting Professor Dr. Katsumi Hattori and graduate student, Ms. Rika Tsutsumi, of the Graduate School of Science at Chiba University, Japan.&#xD;<br \/>\n&#xD;<br \/>\n<figure id=\"attachment_2925\" aria-describedby=\"caption-attachment-2925\" style=\"width: 184px\" class=\"wp-caption alignleft\"><a href=\"https:\/\/blogs.chapman.edu\/scst\/wp-content\/uploads\/sites\/64\/2013\/10\/earthquake-man.jpg\" rel=\"attachment wp-att-2925\"><img loading=\"lazy\" decoding=\"async\" class=\"size-full wp-image-2925 \" title=\"CEESMO Science Lecture\" src=\"https:\/\/blogs.chapman.edu\/scst\/wp-content\/uploads\/sites\/64\/2013\/10\/earthquake-man.jpg\" alt=\"Dr. Katsumi Hattori Chiba University, Japan\" width=\"184\" height=\"187\" \/><\/a><figcaption id=\"caption-attachment-2925\" class=\"wp-caption-text\"><br \/>\n Dr. Katsumi Hattori Chiba University, Japan<\/figcaption><\/figure>&#xD;<br \/>\n&#xD;<br \/>\nProfessor Hattori is an expert in geophysics, signal processing, and natural hazard applications.&#xA0; Ms. Rika Tsutsumi studies volcanic and lava activity using MODIS data processing.&#xD;<br \/>\n&#xD;<br \/>\nThere have been many reports on ultra-low-frequency (ULF) electromagnetic phenomena associated with earthquakes in a very wide frequency range. We are presenting a case study of unusual behaviors of geomagnetic diurnal variations prior to the 2011 Tohoku earthquake off the Pacific Coast (Mw9.0). In order to verify and clarify the ULF seismo-magnetic phenomena, a statistical investigation of the relation between magnetic anomalies and local seismicity have been performed based on geomagnetic data observed during 2001-2010 at the Kakioka Station in Japan.&#xD;<br \/>\n&#xD;<br \/>\nThe lecture, hosted by the Center of Excellence in Earth Systems Modeling and Observations (<br \/>\n<a title=\"Center of Excellence in Earth Systems Modeling &amp; Observations\" href=\"http:\/\/www.chapman.edu\/SCST\/centers-of-excellence\/earth-observing\/index.aspx\" target=\"_blank\">CEESMO<\/a><br \/>\n), is scheduled to take place at 10am in Smith Hall room 101A.&#xD;<br \/>\n&#xD;<\/p>\n<p><a href=\"https:\/\/www.facebook.com\/SchmidCollegeOfScienceTechnologyChapmanUniversity\"><img loading=\"lazy\" decoding=\"async\" class=\"alignleft size-medium wp-image-2939\" src=\"https:\/\/blogs.chapman.edu\/scst\/wp-content\/uploads\/sites\/64\/2013\/11\/facebook.ico\" alt=\"facebook\" width=\"30\" height=\"30\" \/><\/a><br \/>\nFollow us on<br \/>\n<a href=\"https:\/\/www.facebook.com\/SchmidCollegeOfScienceTechnologyChapmanUniversity\" target=\"_blank\">Facebook<\/a><br \/>\n!&#xD;<br \/>\n&#xD;<\/p>\n<p><a href=\"http:\/\/www.linkedin.com\/groups\/Schmid-College-Science-Technology-5060828?trk=my_groups-b-grp-v\"><img loading=\"lazy\" decoding=\"async\" class=\"alignleft size-medium wp-image-2940\" src=\"https:\/\/blogs.chapman.edu\/scst\/wp-content\/uploads\/sites\/64\/2013\/11\/linkedin.ico\" alt=\"linkedin\" width=\"32\" height=\"32\" \/><\/a><br \/>\nJoin on<br \/>\n<a href=\"http:\/\/www.linkedin.com\/groups\/Schmid-College-Science-Technology-5060828?trk=my_groups-b-grp-v\" target=\"_blank\">LinkedIn<\/a><br \/>\n!&#xD;<br \/>\n&#xD;<br \/>\n&#xA0;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Nov 1st. Electromagnetic phenomena and earthquake precursors<\/p>\n","protected":false},"author":271,"featured_media":10320,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"site-sidebar-layout":"default","site-content-layout":"","ast-site-content-layout":"default","site-content-style":"default","site-sidebar-style":"default","ast-global-header-display":"","ast-banner-title-visibility":"","ast-main-header-display":"","ast-hfb-above-header-display":"","ast-hfb-below-header-display":"","ast-hfb-mobile-header-display":"","site-post-title":"","ast-breadcrumbs-content":"","ast-featured-img":"","footer-sml-layout":"","ast-disable-related-posts":"","theme-transparent-header-meta":"","adv-header-id-meta":"","stick-header-meta":"","header-above-stick-meta":"","header-main-stick-meta":"","header-below-stick-meta":"","astra-migrate-meta-layouts":"default","ast-page-background-enabled":"default","ast-page-background-meta":{"desktop":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"tablet":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"mobile":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""}},"ast-content-background-meta":{"desktop":{"background-color":"var(--ast-global-color-4)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"tablet":{"background-color":"var(--ast-global-color-4)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"mobile":{"background-color":"var(--ast-global-color-4)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""}},"custom_author_name":"","chapman_pin_hero_slider":"","footnotes":""},"categories":[6,7],"tags":[12],"class_list":["post-2919","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-events","category-scstresearch","tag-computational-and-data-sciences"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v28.1 - https:\/\/yoast.com\/product\/yoast-seo-wordpress\/ -->\n<title>Schmid College of Science and Technology | Chapman Blogs<\/title>\n<meta name=\"description\" content=\"CEESMO Science Lecture - Nov 1. Electromagnetic phenomena and earthquake precursors: Case study and statistical analysis.\" \/>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/blogs.chapman.edu\/scst\/2013\/10\/29\/ceesmo-science-lecture\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"CEESMO Science Lecture: Electromagnetic phenomena\/earthquake precursor\" \/>\n<meta property=\"og:description\" content=\"CEESMO Science Lecture - Nov 1. 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