{"id":3488,"date":"2024-07-11T19:16:02","date_gmt":"2024-07-11T19:16:02","guid":{"rendered":"https:\/\/oge.mit.edu\/msrp\/?post_type=profiles&#038;p=3488"},"modified":"2025-12-11T12:34:13","modified_gmt":"2025-12-11T17:34:13","slug":"gabrielle-rose","status":"publish","type":"profiles","link":"https:\/\/oge.mit.edu\/msrp\/profiles\/gabrielle-rose\/","title":{"rendered":"Gabrielle Rose"},"content":{"rendered":"<div class=\"wp-block-image\">\n<figure class=\"alignleft size-full is-resized\"><img loading=\"lazy\" decoding=\"async\" width=\"1443\" height=\"1443\" src=\"https:\/\/oge.mit.edu\/msrp\/wp-content\/uploads\/sites\/2\/2024\/08\/RoseGabrielle-edited.jpg\" alt=\"Gabrielle, headshot\" class=\"wp-image-3816\" style=\"width:200px\" srcset=\"https:\/\/oge.mit.edu\/msrp\/wp-content\/uploads\/sites\/2\/2024\/08\/RoseGabrielle-edited.jpg 1443w, https:\/\/oge.mit.edu\/msrp\/wp-content\/uploads\/sites\/2\/2024\/08\/RoseGabrielle-edited-300x300.jpg 300w, https:\/\/oge.mit.edu\/msrp\/wp-content\/uploads\/sites\/2\/2024\/08\/RoseGabrielle-edited-1024x1024.jpg 1024w, https:\/\/oge.mit.edu\/msrp\/wp-content\/uploads\/sites\/2\/2024\/08\/RoseGabrielle-edited-150x150.jpg 150w, https:\/\/oge.mit.edu\/msrp\/wp-content\/uploads\/sites\/2\/2024\/08\/RoseGabrielle-edited-768x768.jpg 768w\" sizes=\"auto, (max-width: 1443px) 100vw, 1443px\" \/><\/figure>\n<\/div>\n\n\n<p><strong>MIT Department: <\/strong>Earth, Atmospheric and Planetary Sciences<br><strong>Faculty Mentor: <\/strong>Prof. Camilla Cattania<br><strong>Research Supervisor:<\/strong> William Frank<br><strong>Undergraduate Institution:<\/strong> Wellesley College<br><strong>Hometown:<\/strong> Coconut Creek, Florida<br><\/p>\n\n\n\n<div style=\"height:0px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<h4 class=\"wp-block-heading\"><strong>Biography<\/strong><\/h4>\n\n\n\n<p>Gabrielle Rose is a rising senior Geosciences major and Physics minor at Wellesley<br>College. Her research interests lie in geophysics, specializing in seismology and natural<br>hazards. Her previous project involved utilizing seismic data to determine and improve the<br>accuracy of volcanic activity detection in West Antarctica. At MSRP, Gabrielle works under Dr. Camilla Cattania and Dr. William Frank, viewing low-frequency earthquakes through different modeling techniques in hopes of adding nuance to future analysis of the phenomenon. She hopes to earn her PhD in the field and continue researching natural hazards. She is co-president of Wellesley\u2019s Club Rocks, an on-campus club for geosciences majors and enthusiasts alike. She has also worked closely with faculty as a diversity intern for Wellesley\u2019s Geosciences department to help foster community in the space and act as a student liaison. In her free time, Gabrielle enjoys listening to music, doing puzzles, playing Dungeons &amp; Dragons, and spending time with her loved ones.<\/p>\n\n\n\n<h4 class=\"wp-block-heading\">Abstract<\/h4>\n\n\n\n<p class=\"has-text-align-center\"><strong>Looking at Low-Frequency Earthquakes through the Perspective of<br>Two Different Models<\/strong><\/p>\n\n\n\n<p class=\"has-text-align-center\"><strong>Gabrielle Rose<sup>1<\/sup>, Camilla Cattania<sup>2<\/sup> and William Frank<sup>2<\/sup><\/strong><br><sup>1<\/sup>Department of Geosciences, Wellesley College<br><sup>2<\/sup>Department of Earth, Atmospheric and Planetary Sciences,<br>Massachusetts Institute of Technology<\/p>\n\n\n\n<p>Low-frequency earthquakes (LFEs) are recurrent seismic events characterized by a lack of high-frequency seismic radiation. They are found worldwide in swarms along subduction plate<br>boundaries in the transitional zone between major earthquakes and deeper continuous creep.<br>Though their spatial distribution and specific periodicity offer crucial insights into the nature of<br>slip in this transitional zone and its relevance to major earthquakes, the underlying origin of<br>LFEs is still unknown. Classical earthquake modeling techniques, like the Brune Source Model, typically fail to capture the source mechanism of LFEs due to a lack of high frequencies captured in the seismic recordings of these events, and they predict scaling relations that are inconsistent with observed LFEs. The focus of this research is to potentially extend the amount of usable bandwidth and explore whether different source models can better explain the LFE source. If we were able to properly characterize LFEs and learn more about their source process, that would allow us to add nuance to future analyses of the dynamics of the plate boundary where LFEs reside.<\/p>\n","protected":false},"featured_media":3816,"template":"","profile_category":[22],"class_list":["post-3488","profiles","type-profiles","status-publish","has-post-thumbnail","hentry","profile_category-2024-interns"],"acf":[],"_links":{"self":[{"href":"https:\/\/oge.mit.edu\/msrp\/wp-json\/wp\/v2\/profiles\/3488","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/oge.mit.edu\/msrp\/wp-json\/wp\/v2\/profiles"}],"about":[{"href":"https:\/\/oge.mit.edu\/msrp\/wp-json\/wp\/v2\/types\/profiles"}],"version-history":[{"count":4,"href":"https:\/\/oge.mit.edu\/msrp\/wp-json\/wp\/v2\/profiles\/3488\/revisions"}],"predecessor-version":[{"id":4944,"href":"https:\/\/oge.mit.edu\/msrp\/wp-json\/wp\/v2\/profiles\/3488\/revisions\/4944"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/oge.mit.edu\/msrp\/wp-json\/wp\/v2\/media\/3816"}],"wp:attachment":[{"href":"https:\/\/oge.mit.edu\/msrp\/wp-json\/wp\/v2\/media?parent=3488"}],"wp:term":[{"taxonomy":"profile_category","embeddable":true,"href":"https:\/\/oge.mit.edu\/msrp\/wp-json\/wp\/v2\/profile_category?post=3488"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}