Jupiter's upper-troposphere vertical motions inferred from the transformed Eulerian mean circulation have upwelling in zones and downwelling in belts, matching the observed cloud structure and resolving the apparent contradiction with Eulerian mean dynamics.
Unstructured Grid Dynamical Modeling of Planetary Atmospheres using planetMPAS: The Influence of the Rigid Lid, Computational Efficiency, and Examples of Martian and Jovian Application
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abstract
We present a new planetary global circulation model, planetMPAS, based on the state-of-the-art NCAR MPAS General Circulation Model. Taking advantage of the cross compatibility between WRF and MPAS, planetMPAS includes most of the planetWRF physics parameterization schemes for terrestrial planets such as Mars and Titan. PlanetMPAS also includes a set of physics that represents radiative transfer, dry convection, moist convection and its associated microphysics for the Jovian atmosphere. We demonstrate that, despite the rigid-lid approximation, planetMPAS is suitable to simulate the climate systems in Martian and Jovian atmospheres with potential application to slow-rotating planets such as Titan. Simulations using planetMPAS show that the new model can reproduce many aspects of the observed features on Mars and Jupiter, such as the seasonal CO2 cycle, polar argon enrichment, zonal mean temperature, and qualitative dust opacity on Mars, as well as the equatorial superrotation and banded zonal wind patterns on Jupiter.
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astro-ph.EP 1years
2025 1verdicts
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Reconciling Jupiter's Vertical Motions with the Observed Cloud Structure in the Upper Troposphere
Jupiter's upper-troposphere vertical motions inferred from the transformed Eulerian mean circulation have upwelling in zones and downwelling in belts, matching the observed cloud structure and resolving the apparent contradiction with Eulerian mean dynamics.