<p>MATISSE (Multi-purpose Advanced Tool for the Solar System Exploration) [1] is a tool that allows the visualization of observations from space missions and datasets derived from these observations on &#160;a &#160;three-dimensional &#160;model &#160;of &#160;the &#160;selected &#160;target &#160;body. &#160;The &#160;second &#160;version &#160;of &#160;the &#160;tool &#160;(named MATISSE &#160;2.0 &#8211;https://tools.ssdc.asi.it/Matisse) &#160;will, &#160;among &#160;other &#160;things, &#160;include &#160;algorithms developed &#160;by &#160;partner &#160;research &#160;teams; &#160;in &#160;this &#160;work &#160;we &#160;focalize &#160;our &#160;attention &#160;on &#160;the &#160;MATISSE inclusion of two codes developed for atmospheric retrieval and thermophysical modeling. The retrieval code is used for the analysis of the spectra provided by the JIRAM instrument (Jovian Infrared Auroral Mapper [2]) onboard the NASA&#8217;s Juno mission, whose main purpose is the study of the upper regions of Jupiter&#8217;s atmosphere in the 2-5 &#956;m wavelength range and pressure up to 5-7 bar. The spectra provided by the instrument are processed with the retrieval code that calculates, for each pixel of a hyperspectral image, the chemical and physical parameters in the corresponding points of the &#160;atmosphere &#160;[3]. &#160;The &#160;code &#160;processes &#160;all &#160;pixels &#160;of &#160;a &#160;hyperspectral &#160;image, &#160;so &#160;parallelization &#160;is convenient &#160;in &#160;order &#160;to &#160;reduce &#160;the &#160;computation &#160;time; &#160;this &#160;is &#160;possible &#160;by &#160;using &#160;the &#160;Python &#160;language tools, which allow the execution of a code written in its own language (FORTRAN in this case) by providing &#160;the &#160;required &#160;parallelization. As a further optimization step, &#160;the &#160;code has been converted into a Docker image to make it portable and easy to run on heterogeneous architectures. The second &#160;code &#160;included &#160;in &#160;MATISSE &#160;is &#160;a &#160;thermophysical &#160;model &#160;that &#160;calculates &#160;the &#160;surface temperature of airless bodies as function of thermal conductivity [4,5] and other physical properties; the calculated temperature can be compared with the measured ones, if any, in order to retrieve the thermal properties of the soil, or can be used to compute other temperature-dependent quantities. At the present time this code is going to be used for Mercury and Ceres and is almost ready to be included in MATISSE 2.0.</p>
<p>[1] Zinzi, A., et al. (2016), Astronomy & Computing, 15, 16-28<br />[2] Adriani, A., et al. (2017), Space Science Reviews, 213, 393-446<br />[3] Grassi et al. (2010), Planetary and Space Science, 58, 1265-1278<br />[4] Capria, M. T. et al (2014), Geophysical Research Letters, 41, 1438-1443<br />[5] Rognini et al. (2019), Journal of Geophysical Research, https://doi.org/10.1029/2018JE005733</p>