Results 41 to 50 of about 4,026 (203)
The Role of Planetary Rotation in Polar Cusp Localization
Abstract Juno observations have revealed that Jupiter's polar cusps are displaced toward dusk and even the nightside, contradicting the Earth‐derived paradigm that is confined to narrower ranges near noon. These findings underscore the overlooked influence of planetary rotation on magnetospheric dynamics, exposing a critical gap in current theoretical ...
Junjie Chen +9 more
wiley +1 more source
Fluctuating Interfaces in Barotropic Beta‐Plane Turbulence
Abstract Zonal jets manifest themselves as bands with sharp interfaces in the vorticity configuration. We develop an algorithm to track these fluctuating vorticity interfaces and systematically investigate their characteristic spatio‐temporal behaviors.
Sandip Sahoo, Samriddhi Sankar Ray
wiley +1 more source
Strong Tidal Dissipation at Uranus?
Geophysical estimates of paleo heat fluxes on the Uranian moons Miranda and Ariel are in the range of 25–75 mW m ^−2 . For a canonical Uranus dissipation factor Q = 18,000, expected equilibrium tidal heating rates for these satellites are less than 6 mW ...
Francis Nimmo
doaj +1 more source
* Tromikosoma uranus (Thomson, 1877) Fig. 21 A–C. Phormosoma uranus: A. Agassiz, 1881: 103. Echinosoma uranus: H.L. Clark, 1925a: 57. Tromikosoma uranus: Mortensen, 1935: 168 –170. Pl. VI, Figs 2–3. Pl.
Filander, Zoleka, Griffiths, Charles
core +1 more source
Abstract Convection‐permitting regional climate models (CP‐RCMs) often outperform coarser‐resolution models in simulating precipitation, but assessing their accuracy across resolutions and configurations remains challenging. This study evaluates the performance and sensitivity of different configurations of the sixth version of the Canadian Regional ...
Kim Lahaie +3 more
wiley +1 more source
Tilting Uranus via the migration of an ancient satellite
Context. The 98{\deg}-obliquity of Uranus is commonly attributed to giant impacts that occurred at the end of the planetary formation. This picture, however, is not devoid of weaknesses. Aims.
Kevin Baillié +20 more
core +1 more source
Did Uranus' regular moons form via a rocky giant impactor? [PDF]
The formation of Uranus' regular moons has been suggested to be linked to the origin of its enormous spin axial tilt (~98o). A giant impact between proto-Uranus and a 2–3 MEarth impactor could lead to a large tilt and to the formation of an impact ...
Reinhardt, Christian +5 more
core +1 more source
Different Inhomogeneous Evolutionary Histories for Uranus and Neptune
We present updated nonadiabatic and inhomogeneous evolution models for Uranus and Neptune, employing an interior composition of methane, ammonia, water, and rocks.
Roberto Tejada Arevalo
doaj +1 more source
Soft X‐Ray Emission From Saturn's Magnetosheath II: Solar Wind Driving
Abstract Saturn's magnetosphere is dominated by Enceladus‐sourced neutrals, which spread throughout the system into the magnetosheath. The neutrals can charge exchange with highly charged solar wind ions, causing soft X‐ray emission (<2 ${< } 2$ keV) upon de‐excitation of the ion.
D. Naylor +4 more
wiley +1 more source
katelinbdonaldson/KHIs-at-Uranus-and-Neptune: KHIs at Uranus and Neptune
<p>This repository includes the scripts used to create analytic model to produce the results in the paper "Characterizing the solar wind-magnetosphere viscous interaction at Uranus and Neptune".</p> <p>The MATLAB code is split
katelinbdonaldson
core +1 more source

