I study tidal heat in Ocean Worlds, like Europa.
Tides force the ice shells at very many frequencies. The ice response to that forcing is frequency dependent based on temperature. With such a large temperature gradient across the ice, different parts of the tide ring loudest at various radial positions in the ice. We find that where this heat gets deposited is just as important, if not more, than how much heat is deposited. As a result, the shells evolve toward steady state in a bunch of ways which depend on the specific tidal configuration.
This research predicts shell thickness, heat flux, and Love numbers to aid in mission data interpretation.
2021+
Planetary Science Intitute - Associate Research Scientist
2018 - 2020
University of Southern Maine - Visiting Assistant Professor of Physics
2017 - 2018
Arizona State University - Postdoctoral Scholar
2011 - 2017
University of California, Los Angeles - Graduate Student
PSI is a Nonprofit 501(c)(3) Corporation, and an Equal Opportunity and Affirmative Action Employer
Corporate Headquarters: 1700 East Fort Lowell, Suite 106 * Tucson, AZ 85719-2395 * 520-622-6300 * FAX: 520-622-8060
Copyright © 2022 . All Rights Reserved.