A magnetotelluric instrument for probing the interiors of Europa and other worlds
Robert Grimm, Ton Nguyen, Steve Persyn, Mark Phillips, David Stillman,, Tim Taylor, Greg Delory, Paul Turin, Jared Espley, Jacob Gruesbeck, Dave, Sheppard

TL;DR
This paper presents the development of a magnetotelluric instrument designed for lander missions to Europa, enabling detection of subsurface water and characterization of the ice shell through broadband electromagnetic measurements.
Contribution
The paper introduces a novel Europa Magnetotelluric Sounder (EMS) prototype capable of operating in harsh environments for subsurface water detection using the magnetotelluric method.
Findings
EMS can detect intrashell water on Europa.
Prototype successfully tested in relevant conditions.
Supports constraints on Europa's habitability.
Abstract
One objective of a lander mission to Jupiter's icy moon Europa is to detect liquid water within 30 km as well as characterizing the subsurface ocean. In order to satisfy this objective, water within the ice shell must also be identified. Inductive electromagnetic (EM) methods are optimal for water detection on Europa because even a small fraction of dissolved salts will make water orders of magnitude more electrically conductive than the ice shell. Compared to induction studies by the Galileo spacecraft, measurements of higher-frequency ambient EM fields are necessary to resolve the shallower depths of intrashell water. Although these fields have been mostly characterized by prior missions, their unknown source structures and plasma properties do not allow EM sounding using a single surface magnetometer or the orbit-to-surface magnetic transfer function, respectively. Instead, broadband…
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