EGU21-10230
https://doi.org/10.5194/egusphere-egu21-10230
EGU General Assembly 2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.

Saturn´s Stratospheric Hazes From HST Ultraviolet Imaging

José Francisco Sanz Requena1, Santiago Pérez Hoyos2, Agustín Sánchez-Lavega3, Henrik Melin4, Leigh Fletcher5, and Patrick Irwin6
José Francisco Sanz Requena et al.
  • 1Universidad Europea Miguel de Cervantes UEMC, Escuela Poltécnica Superior, Ciencias experimentales, Valladolid, Spain (jfsanz@uemc.es)
  • 2Departamento Física Aplicada I, Escuela de Ingeniería de Bilbao, Universidad del País Vasco UPV/EHU, Bilbao, Spain
  • 3Departamento Física Aplicada I, Escuela de Ingeniería de Bilbao, Universidad del País Vasco UPV/EHU, Bilbao, Spain
  • 4School of Physics & Astronomy, University of Leicester, University Road, Leicester LE1 7RH, UK
  • 5School of Physics & Astronomy, University of Leicester, University Road, Leicester LE1 7RH, UK
  • 6Department of Physics, University of Oxford, Parks Rd, Oxford OX1 3PU, UK

We present a study on Saturn's stratospheric hazes using archived images from the Hubble Space Telescope Advanced Camera for Surveys. These observations were taken from 2005 to 2014, including the Great Storm during the years 2010 and 2011. For our research we used ultraviolet images from the Solar Blind Channel camera equipped with the F115LP and F125LP filters. At these wavelengths, the reflected spectrum is fundamentally Rayleigh-scattered, with substantial contributions from hydrocarbon absorptions and additional scattering by the aerosols in the hazes above the tropopause. The goal of this work is to analyze temporal and latitudinal changes in the characteristics of the stratospheric haze, gases and particles, analyzing the absolute reflectivity and its limb darkening. Such behavior can be reproduced using the empirical Minnaert's law. This provides nadir-viewing reflectivity and limb darkening coefficient as a function of latitude and time. This is a first approach that helps to qualitatively identify the changes occurring in the aerosol layer during this period of time, which include the massive Great White Spot of 2010. In order to quantify such aerosol changes, we use the radiative transfer code and retrieval suite NEMESIS (Non-Linear Optimal Estimator for Multivariat Spectral AnalySIS) to reproduce the observed reflectivity.  Here we will focus on the detected variations of the vertical distribution of the stratospheric particles, their integrated optical thickness and size distribution and will correlate them with the seasonal changes taken place in the atmosphere of the planet.

How to cite: Sanz Requena, J. F., Pérez Hoyos, S., Sánchez-Lavega, A., Melin, H., Fletcher, L., and Irwin, P.: Saturn´s Stratospheric Hazes From HST Ultraviolet Imaging, EGU General Assembly 2021, online, 19–30 Apr 2021, EGU21-10230, https://doi.org/10.5194/egusphere-egu21-10230, 2021.