{"id":4439,"date":"2025-10-29T11:36:20","date_gmt":"2025-10-29T15:36:20","guid":{"rendered":"https:\/\/oge.mit.edu\/msrp\/?post_type=profiles&#038;p=4439"},"modified":"2025-12-09T11:43:09","modified_gmt":"2025-12-09T16:43:09","slug":"jasmine-hollis","status":"publish","type":"profiles","link":"https:\/\/oge.mit.edu\/msrp\/profiles\/jasmine-hollis\/","title":{"rendered":"Jasmine Hollis"},"content":{"rendered":"<div class=\"wp-block-image\">\n<figure class=\"alignleft size-full is-resized\"><img loading=\"lazy\" decoding=\"async\" width=\"2560\" height=\"2560\" src=\"https:\/\/oge.mit.edu\/msrp\/wp-content\/uploads\/sites\/2\/2025\/10\/HollisJas-edited-scaled.jpg\" alt=\"\" class=\"wp-image-4440\" style=\"width:200px;height:auto\" srcset=\"https:\/\/oge.mit.edu\/msrp\/wp-content\/uploads\/sites\/2\/2025\/10\/HollisJas-edited-scaled.jpg 2560w, https:\/\/oge.mit.edu\/msrp\/wp-content\/uploads\/sites\/2\/2025\/10\/HollisJas-edited-300x300.jpg 300w, https:\/\/oge.mit.edu\/msrp\/wp-content\/uploads\/sites\/2\/2025\/10\/HollisJas-edited-1024x1024.jpg 1024w, https:\/\/oge.mit.edu\/msrp\/wp-content\/uploads\/sites\/2\/2025\/10\/HollisJas-edited-150x150.jpg 150w, https:\/\/oge.mit.edu\/msrp\/wp-content\/uploads\/sites\/2\/2025\/10\/HollisJas-edited-768x768.jpg 768w, https:\/\/oge.mit.edu\/msrp\/wp-content\/uploads\/sites\/2\/2025\/10\/HollisJas-edited-1536x1536.jpg 1536w, https:\/\/oge.mit.edu\/msrp\/wp-content\/uploads\/sites\/2\/2025\/10\/HollisJas-edited-2048x2048.jpg 2048w\" sizes=\"auto, (max-width: 2560px) 100vw, 2560px\" \/><\/figure>\n<\/div>\n\n\n<div class=\"wp-block-group\"><div class=\"wp-block-group__inner-container is-layout-constrained wp-block-group-is-layout-constrained\">\n<p><strong>MIT Department:<\/strong> Earth, Atmospheric, and Planetary Sciences<br><strong>Faculty Mentor<\/strong>: Prof. Timothy Cronin<br><strong>Undergraduate Institution:<\/strong> Yale University<br><strong>Website<\/strong>:<\/p>\n<\/div><\/div>\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>Jas Hollis (he\/they) is a rising junior at Yale University studying atmosphere, ocean, and climate dynamics. He has worked on projects involving Arctic Ocean properties and cloud physics. Post-college, Jas plans to pursue a PhD in atmospheric science, with goals of researching convective storm dynamics and engaging in climate policy work. They have experience in database management with SQL, machine learning with Python, working as a writing consultant for college applicants, and tutoring students in C, C++, and MATLAB. He is also conversational in French and Mandarin Chinese. Beyond academics, they sing for a collegiate a cappella group, serving separate terms as the group\u2019s business and album manager. Finally, Jas is passionate about community betterment, which led them to spend a few summers serving their community through a feed-and-read program in San Antonio, TX, and to study queer history and social justice. Jas hopes to center societal impact in his future pursuits, using his research and leadership skills to advance outreach in atmospheric science and inform tangible climate change solutions<\/p>\n\n\n\n<h4 class=\"wp-block-heading\"><strong>Abstract<\/strong><\/h4>\n\n\n\n<p class=\"has-text-align-center\"><strong>A Simple Analytic Approximation for Single-Raindrop Precipitation Efficiency<\/strong><\/p>\n\n\n\n<div class=\"wp-block-group\"><div class=\"wp-block-group__inner-container is-layout-constrained wp-block-group-is-layout-constrained\">\n<div class=\"wp-block-group\"><div class=\"wp-block-group__inner-container is-layout-constrained wp-block-group-is-layout-constrained\">\n<div class=\"wp-block-group is-vertical is-content-justification-center is-nowrap is-layout-flex wp-container-core-group-is-layout-73832be3 wp-block-group-is-layout-flex\">\n<p class=\"has-text-align-center\"><strong>Jasmine Hollis<sup>1<\/sup>, and Timothy Cronin<sup>2<\/sup><\/strong><\/p>\n\n\n\n<div class=\"wp-block-group is-vertical is-content-justification-center is-layout-flex wp-container-core-group-is-layout-4b2eccd6 wp-block-group-is-layout-flex\">\n<p class=\"has-text-align-center\"><sup>1<\/sup>Department of Earth and Planetary Sciences, Yale University<\/p>\n\n\n\n<p class=\"has-text-align-center\"><sup>2<\/sup>Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology<\/p>\n<\/div>\n<\/div>\n<\/div><\/div>\n<\/div><\/div>\n\n\n\n<p class=\"has-text-align-center\"><\/p>\n\n\n\n<p>Precipitation efficiency (\u03b7) describes the fraction of raindrop water molecules that reach the Earth\u2019s surface. Though critical to understanding the water cycle, precipitation efficiency remains poorly represented within current weather and climate models. In this project, we derive a simple, analytic approximation of precipitation efficiency as a function of surface relative humidity, surface air temperature, and initial radius of the raindrop. Through our process, we assume a dry-adiabat in the subcloud layer and a monodisperse population of raindrops. Here is our resulting approximation:<\/p>\n\n\n<div class=\"wp-block-image\">\n<figure class=\"aligncenter size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"355\" height=\"63\" src=\"https:\/\/oge.mit.edu\/msrp\/wp-content\/uploads\/sites\/2\/2025\/10\/Screenshot-2025-10-29-at-11.32.46-AM.png\" alt=\"\" class=\"wp-image-4441\" srcset=\"https:\/\/oge.mit.edu\/msrp\/wp-content\/uploads\/sites\/2\/2025\/10\/Screenshot-2025-10-29-at-11.32.46-AM.png 355w, https:\/\/oge.mit.edu\/msrp\/wp-content\/uploads\/sites\/2\/2025\/10\/Screenshot-2025-10-29-at-11.32.46-AM-300x53.png 300w\" sizes=\"auto, (max-width: 355px) 100vw, 355px\" \/><\/figure>\n<\/div>\n\n\n<p class=\"has-text-align-left\">In this approximation, precipitation efficiency scales with the cubed ratio of initial raindrop<br>radius remaining at the surface to initial radius at the cloud base. K is the effective evaporative<br>cross-section of the raindrop, meaning the area undergoing evaporation, adjusted to account for<br>ventilation. S is the effective saturation deficit, which captures the thermodynamic potential for<br>evaporation, based on relative humidity and temperature. Finally, we assess the approximation<br>using numerical simulations of the exact equations. In future work, we will extend the<br>approximation to account for a range of initial raindrop sizes. Overall, our approximation of<br>precipitation efficiency will improve our understanding of the water cycle.<\/p>\n","protected":false},"featured_media":4440,"template":"","profile_category":[23],"class_list":["post-4439","profiles","type-profiles","status-publish","has-post-thumbnail","hentry","profile_category-2025-interns"],"acf":[],"_links":{"self":[{"href":"https:\/\/oge.mit.edu\/msrp\/wp-json\/wp\/v2\/profiles\/4439","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":3,"href":"https:\/\/oge.mit.edu\/msrp\/wp-json\/wp\/v2\/profiles\/4439\/revisions"}],"predecessor-version":[{"id":4811,"href":"https:\/\/oge.mit.edu\/msrp\/wp-json\/wp\/v2\/profiles\/4439\/revisions\/4811"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/oge.mit.edu\/msrp\/wp-json\/wp\/v2\/media\/4440"}],"wp:attachment":[{"href":"https:\/\/oge.mit.edu\/msrp\/wp-json\/wp\/v2\/media?parent=4439"}],"wp:term":[{"taxonomy":"profile_category","embeddable":true,"href":"https:\/\/oge.mit.edu\/msrp\/wp-json\/wp\/v2\/profile_category?post=4439"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}