A planetary-scale disturbance in the most intense Jovian atmospheric jet from JunoCam and ground-based observations

We describe a huge planetary-scale disturbance in the highest-speed Jovian jet at latitude 23.5°N that was first observed in October 2016 during the Juno perijove-2 approach. An extraordinary outburst of four plumes was involved in the disturbance development. They were located in the range of plane...

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Detalles Bibliográficos
Autores: Sanchez-Lavega, Agustin, Rogers, John H, Orton, Glenn, García Melendo, Enrique José|||0000-0002-3354-1140, Legarreta, Jon, Colas, Françoise, Dauvergne, J, Hueso, Ricardo, Rojas, Jose Félix, Perez-Hoyos, Santiago, Mendikoa, Iñigo, Iñurrigarro, P, Gómez-Forrellad, Josep M., Momary, T, Hansen, C. J., Eichstaedt, G., Miles, P, Wesley, A
Tipo de recurso: artículo
Fecha de publicación:2017
País:España
Institución:Universitat Politècnica de Catalunya (UPC)
Repositorio:UPCommons. Portal del coneixement obert de la UPC
Idioma:inglés
OAI Identifier:oai:upcommons.upc.edu:2117/111256
Acceso en línea:https://hdl.handle.net/2117/111256
https://dx.doi.org/10.1002/2017GL073421
Access Level:acceso abierto
Palabra clave:Planets
Jupiter (Planet)
JUPITER’S NTB JET DISTURBANCE
Planetes
Júpiter (Planeta)
Àrees temàtiques de la UPC::Física
Descripción
Sumario:We describe a huge planetary-scale disturbance in the highest-speed Jovian jet at latitude 23.5°N that was first observed in October 2016 during the Juno perijove-2 approach. An extraordinary outburst of four plumes was involved in the disturbance development. They were located in the range of planetographic latitudes from 22.2° to 23.0°N and moved faster than the jet peak with eastward velocities in the range 155 to 175 m s 1. In the wake of the plumes, a turbulent pattern of bright and dark spots (wave number 20–25) formed and progressed during October and November on both sides of the jet, moving with speeds in the range 100–125 m s 1 and leading to a new reddish and homogeneous belt when activity ceased in late November. Nonlinear numerical models reproduce the disturbance cloud patterns as a result of the interaction between local sources (the plumes) and the zonal eastward jet.