Spatiotemporal Variations of Temperature in Jupiter's Upper Atmosphere

Fuente: arXiv
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Auteurs principaux: Roberts, Kate, Moore, Luke, O'Donoghue, James, Melin, Henrik, Stallard, Tom, Knowles, Katie L., Schmidt, Carl, Tiranti, Paola I.
Format: Preprint
Publié: 2025
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author Roberts, Kate
Moore, Luke
O'Donoghue, James
Melin, Henrik
Stallard, Tom
Knowles, Katie L.
Schmidt, Carl
Tiranti, Paola I.
author_facet Roberts, Kate
Moore, Luke
O'Donoghue, James
Melin, Henrik
Stallard, Tom
Knowles, Katie L.
Schmidt, Carl
Tiranti, Paola I.
contents Global temperatures in Jupiter's upper atmosphere are poorly constrained. Other than an in situ measurement by the Galileo Probe, all temperature data come from remote sensing methods which primarily rely on emissions from H$_3^+$, the dominant molecular ion in giant planet ionospheres. While H$_3^+$ temperature serves as a proxy for thermospheric temperature under specific conditions, the available H$_3^+$ observations at Jupiter have limited spatial coverage and a wide range of reported temperatures that complicate analysis of atmospheric temperatures. We present high resolution H$_3^+$ temperature maps near local solar noon collected over three half-nights in 2022 and 2023. Pole-to-pole temperature structure is consistent across time spans of one month to one year. Median equatorial ($\pm$ 25° latitude) temperature across all three nights is 762 $\pm$ 43 K, with night-to-night differences of $<$75 K. Temperatures within the statistical locations of the northern and southern auroral ovals are 1200 $\pm$ 96 K and 1143 $\pm$ 120 K, respectively. A region $\sim$30 K cooler than its surroundings is found near 20° N, 90° W System III longitude, roughly coincident with a magnetic field anomaly, providing additional evidence for magnetic influence on Jupiter's upper atmosphere. Temperatures generally decrease smoothly from auroral to equatorial latitudes, consistent with the expected gradient if Jupiter's non-auroral latitudes are heated primarily by dynamical redistribution of auroral energy.
format Preprint
id arxiv_https___arxiv_org_abs_2503_19153
institution arXiv
publishDate 2025
record_format arxiv
spellingShingle Spatiotemporal Variations of Temperature in Jupiter's Upper Atmosphere
Roberts, Kate
Moore, Luke
O'Donoghue, James
Melin, Henrik
Stallard, Tom
Knowles, Katie L.
Schmidt, Carl
Tiranti, Paola I.
Earth and Planetary Astrophysics
Global temperatures in Jupiter's upper atmosphere are poorly constrained. Other than an in situ measurement by the Galileo Probe, all temperature data come from remote sensing methods which primarily rely on emissions from H$_3^+$, the dominant molecular ion in giant planet ionospheres. While H$_3^+$ temperature serves as a proxy for thermospheric temperature under specific conditions, the available H$_3^+$ observations at Jupiter have limited spatial coverage and a wide range of reported temperatures that complicate analysis of atmospheric temperatures. We present high resolution H$_3^+$ temperature maps near local solar noon collected over three half-nights in 2022 and 2023. Pole-to-pole temperature structure is consistent across time spans of one month to one year. Median equatorial ($\pm$ 25° latitude) temperature across all three nights is 762 $\pm$ 43 K, with night-to-night differences of $<$75 K. Temperatures within the statistical locations of the northern and southern auroral ovals are 1200 $\pm$ 96 K and 1143 $\pm$ 120 K, respectively. A region $\sim$30 K cooler than its surroundings is found near 20° N, 90° W System III longitude, roughly coincident with a magnetic field anomaly, providing additional evidence for magnetic influence on Jupiter's upper atmosphere. Temperatures generally decrease smoothly from auroral to equatorial latitudes, consistent with the expected gradient if Jupiter's non-auroral latitudes are heated primarily by dynamical redistribution of auroral energy.
title Spatiotemporal Variations of Temperature in Jupiter's Upper Atmosphere
topic Earth and Planetary Astrophysics
url https://arxiv.org/abs/2503.19153