JWST Reveals Spectral Tracers of Recent Surface Modification on Europa
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| Main Authors: | , , , , , , , , , , , |
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| Format: | Preprint |
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2025
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| author | Cartwright, Richard J. Hibbits, Charles A. Holler, Bryan J. Raut, Ujjwal Nordheim, Tom A. Neveu, Marc Protopapa, Silvia Glein, Christopher R. Leonard, Erin J. Roth, Lorenz Beddingfield, Chloe B. Villanueva, Geronimo L. |
| author_facet | Cartwright, Richard J. Hibbits, Charles A. Holler, Bryan J. Raut, Ujjwal Nordheim, Tom A. Neveu, Marc Protopapa, Silvia Glein, Christopher R. Leonard, Erin J. Roth, Lorenz Beddingfield, Chloe B. Villanueva, Geronimo L. |
| contents | Europa has been modified by a variety of geologic processes, exposing internally-derived materials that are heavily irradiated by charged particles trapped in Jupiter's magnetosphere. Prior spectral analysis of H2O ice on Europa relied on low signal-to-noise data at wavelengths >2.5 microns, limiting assessment of a 3.1 micron Fresnel peak that is diagnostic of exposed crystalline ice. We report new measurements of H2O ice spectral features using high signal-to-noise data collected by the NIRSpec spectrograph (1.48 - 5.35 microns) on the James Webb Space Telescope. These data reveal a narrow 3.1 micron crystalline H2O ice Fresnel peak, which is primarily located at southern latitudes in Tara and Powys Regiones. Our analysis indicates that crystalline ice exposed in these low-latitude regiones is likely sustained by ongoing thermal (re)crystallization outpacing charged particle amorphization of the top 10 microns of Europa's regolith over short timescales (<15 days). We also measured H2O ice features centered near 1.5 microns, 1.65 microns, and 2.0 microns, and a broad 3.6 micron H2O continuum peak, which are all stronger at northern latitudes, in contrast to the 3.1 micron Fresnel peak identified at southern latitudes. These results support the hypothesis that H2O ice in Europa's regolith is vertically stratified, with amorphous ice grains dominating its exposed surface, except in Tara and Powys Regiones. We also find that a previously detected 4.38 micron 13O2 feature is present almost exclusively at southern latitudes in Tara and Powys Regiones, likely derived from an internal source of carbon-bearing material. |
| format | Preprint |
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arxiv_https___arxiv_org_abs_2504_05283 |
| institution | arXiv |
| publishDate | 2025 |
| record_format | arxiv |
| spellingShingle | JWST Reveals Spectral Tracers of Recent Surface Modification on Europa Cartwright, Richard J. Hibbits, Charles A. Holler, Bryan J. Raut, Ujjwal Nordheim, Tom A. Neveu, Marc Protopapa, Silvia Glein, Christopher R. Leonard, Erin J. Roth, Lorenz Beddingfield, Chloe B. Villanueva, Geronimo L. Earth and Planetary Astrophysics Europa has been modified by a variety of geologic processes, exposing internally-derived materials that are heavily irradiated by charged particles trapped in Jupiter's magnetosphere. Prior spectral analysis of H2O ice on Europa relied on low signal-to-noise data at wavelengths >2.5 microns, limiting assessment of a 3.1 micron Fresnel peak that is diagnostic of exposed crystalline ice. We report new measurements of H2O ice spectral features using high signal-to-noise data collected by the NIRSpec spectrograph (1.48 - 5.35 microns) on the James Webb Space Telescope. These data reveal a narrow 3.1 micron crystalline H2O ice Fresnel peak, which is primarily located at southern latitudes in Tara and Powys Regiones. Our analysis indicates that crystalline ice exposed in these low-latitude regiones is likely sustained by ongoing thermal (re)crystallization outpacing charged particle amorphization of the top 10 microns of Europa's regolith over short timescales (<15 days). We also measured H2O ice features centered near 1.5 microns, 1.65 microns, and 2.0 microns, and a broad 3.6 micron H2O continuum peak, which are all stronger at northern latitudes, in contrast to the 3.1 micron Fresnel peak identified at southern latitudes. These results support the hypothesis that H2O ice in Europa's regolith is vertically stratified, with amorphous ice grains dominating its exposed surface, except in Tara and Powys Regiones. We also find that a previously detected 4.38 micron 13O2 feature is present almost exclusively at southern latitudes in Tara and Powys Regiones, likely derived from an internal source of carbon-bearing material. |
| title | JWST Reveals Spectral Tracers of Recent Surface Modification on Europa |
| topic | Earth and Planetary Astrophysics |
| url | https://arxiv.org/abs/2504.05283 |