2012
DOI: 10.1016/j.icarus.2011.11.008
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The 2009–2010 fade of Jupiter’s South Equatorial Belt: Vertical cloud structure models and zonal winds from visible imaging

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Cited by 39 publications
(58 citation statements)
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“…This is a reasonable result not only because of the smaller time difference between both profiles but also because of the visual appearance of the cloud morphology in both years. The appearance is very similar despite recent large-scale cyclic variations such as the Fade (2009−10) and Revival (2010) of the SEB (Pérez-Hoyos et al 2012;Fletcher et al 2011) or the impact of a 500 m object with Jupiter in 2009 at −55 • latitude (Sánchez-Lavega et al 2010), which resulted in a large dark debris cloud that moved at the same velocity as the general flow as retrieved from HST (Hammel et al 2010) and ground-based observations (Sánchez-Lavega et al 2011). The only notorious change between these two epochs occurred at latitude 27−28 • , where 2008 HST data showed a westward acceleration of the A74, page 8 of 11 jet (Asay-Davis et al 2011).…”
Section: Long-term Variationsmentioning
confidence: 77%
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“…This is a reasonable result not only because of the smaller time difference between both profiles but also because of the visual appearance of the cloud morphology in both years. The appearance is very similar despite recent large-scale cyclic variations such as the Fade (2009−10) and Revival (2010) of the SEB (Pérez-Hoyos et al 2012;Fletcher et al 2011) or the impact of a 500 m object with Jupiter in 2009 at −55 • latitude (Sánchez-Lavega et al 2010), which resulted in a large dark debris cloud that moved at the same velocity as the general flow as retrieved from HST (Hammel et al 2010) and ground-based observations (Sánchez-Lavega et al 2011). The only notorious change between these two epochs occurred at latitude 27−28 • , where 2008 HST data showed a westward acceleration of the A74, page 8 of 11 jet (Asay-Davis et al 2011).…”
Section: Long-term Variationsmentioning
confidence: 77%
“…The mean intensity of the winds has shown temporal variability on the order of ∼10 ms −1 (Asay-Davis et al 2011) and a remarkable stability of the latitudes of the zonal jets' maximum velocities. Although some of the bands' morphology changes in periods of years (Peek 1958;Chapman & Reese 1968;Reese 1972;Minton 1972a,b;Smith & Hunt 1976;Sánchez-Lavega & Rodrigo 1985;Rogers 1995;Sánchez-Lavega & Gómez 1996;Sánchez-Lavega et al 1996;Fletcher et al 2011;Pérez-Hoyos et al 2012), the wind profile maintains a remarkable temporal stability. Furthermore, this zonal wind profile is not strongly affected by the dynamic perturbations at cloud level, such as those developed by convective storms like the South Equatorial Belt Disturbance (SEBD; Sánchez-Lavega et al 1996;Sánchez-Lavega & Gómez 1996) and the North Temperate Belt Disturbance (NTBD) (García-Melendo et al 2005Sánchez-Lavega et al 2008;Barrado-Izagirre et al 2009a).…”
Section: Introductionmentioning
confidence: 99%
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“…In this work, we profusely refer to a number of previous studies that served as an external reference for the absolute reflectivity values we obtain in this work. No seasonal variability has been reported in the atmosphere of Jupiter except for planetary-scale changes at particular belts and zones not linked to seasonal changes, (see Sánchez-Lavega et al 1996;Sánchez-Lavega et al 2008Fletcher et al 2011;Pérez-Hoyos et al 2012); however, Saturn is known to display hemispherical seasonal changes and changing viewing or illumination geometry owing to the tilt of its rotation axis (West et al 2009). For this reason, Saturn photometric values usually only serve as a snapshot for a particular season.…”
Section: Introductionmentioning
confidence: 99%
“…Irregular and brusque variations caused by storms or structural changes in the planet's belts have also been observed in giant planets (e.g. Tejfel et al 1994;Sánchez-Lavega 1994;Rogers 2009;Fletcher et al 2011;Pérez-Hoyos et al 2012), and they are likely to happen in ultracool dwarfs as well. Photometric data from different epochs, separated by months, are already available for a few ultracool dwarfs (e.g.…”
Section: Introductionmentioning
confidence: 98%