Published June 18, 2024
| Version v1
Journal article
Cassini spacecraft reveals global energy imbalance of Saturn
Contributors
Others:
- Department of Atmospheric and Oceanic Sciences [Boulder] (ATOC) ; University of Colorado [Boulder]
- Feinberg School of Medicine [Northwestern University, Evanston] ([Northwestern University Medical School]) ; Northwestern University [Evanston]
- Jet Propulsion Laboratory (JPL) ; NASA-California Institute of Technology (CALTECH)
- NASA Goddard Space Flight Center (GSFC)
- University of Central Florida [Orlando] (UCF)
- Joseph Louis LAGRANGE (LAGRANGE) ; Université Nice Sophia Antipolis (1965 - 2019) (UNS)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de la Côte d'Azur ; Université Côte d'Azur (UniCA)-Université Côte d'Azur (UniCA)-Centre National de la Recherche Scientifique (CNRS)
- Departamento de Fisica Aplicada [Bilbao] ; Universidad del País Vasco [Espainia] / Euskal Herriko Unibertsitatea [España] = University of the Basque Country [Spain] = Université du pays basque [Espagne] (UPV / EHU)
- Universidad del País Vasco [Espainia] / Euskal Herriko Unibertsitatea [España] = University of the Basque Country [Spain] = Université du pays basque [Espagne] (UPV / EHU)
- Department of Earth and Planetary Sciences [Santa Cruz] ; University of California [Santa Cruz] (UC Santa Cruz) ; University of California (UC)-University of California (UC)
Description
Abstract The global energy budget is pivotal to understanding planetary evolution and climate behaviors. Assessing the energy budget of giant planets, particularly those with large seasonal cycles, however, remains a challenge without long-term observations. Evolution models of Saturn cannot explain its estimated Bond albedo and internal heat flux, mainly because previous estimates were based on limited observations. Here, we analyze the long-term observations recorded by the Cassini spacecraft and find notably higher Bond albedo (0.41 ± 0.02) and internal heat flux (2.84 ± 0.20 Wm −2 ) values than previous estimates. Furthermore, Saturn's global energy budget is not in a steady state and exhibits significant dynamical imbalances. The global radiant energy deficit at the top of the atmosphere, indicative of the planetary cooling of Saturn, reveals remarkable seasonal fluctuations with a magnitude of 16.0 ± 4.2%. Further analysis of the energy budget of the upper atmosphere including the internal heat suggests seasonal energy imbalances at both global and hemispheric scales, contributing to the development of giant convective storms on Saturn. Similar seasonal variabilities of planetary cooling and energy imbalance exist in other giant planets within and beyond the Solar System, a prospect currently overlooked in existing evolutional and atmospheric models.
Abstract
International audienceAdditional details
Identifiers
- URL
- https://cnrs.hal.science/hal-04797572
- URN
- urn:oai:HAL:hal-04797572v1
Origin repository
- Origin repository
- UNICA