Longobardo, A.A.Longobardo0000-0002-1797-2741DELLA CORTE, VINCENZOVINCENZODELLA CORTE0000-0001-6461-5803IVANOVSKI, STAVRO LAMBROVSTAVRO LAMBROVIVANOVSKI0000-0002-8068-7695RINALDI, GIOVANNAGIOVANNARINALDI0000-0002-2968-0455Zakharov, V.V.Zakharov0000-0002-2411-506XRotundi, AlessandraAlessandraRotundi0000-0001-5467-157XCAPACCIONI, FABRIZIOFABRIZIOCAPACCIONI0000-0003-1631-4314FULLE, MarcoMarcoFULLE0000-0001-8435-5287FILACCHIONE, GIANRICOGIANRICOFILACCHIONE0000-0001-9567-0055Palomba, E.E.Palomba0000-0002-9101-6774PALUMBO, PASQUALEPASQUALEPALUMBO0000-0003-2323-9228CAPRIA, MARIA TERESAMARIA TERESACAPRIA0000-0002-9814-9588TOSI, FedericoFedericoTOSI0000-0003-4002-2434RAPONI, AndreaAndreaRAPONI0000-0003-4996-0099CIARNIELLO, MauroMauroCIARNIELLO0000-0002-7498-5207Bockelee-Morvan, D.D.Bockelee-MorvanErard, S.S.ErardLeyrat, C.C.LeyratDirri, F.F.Dirri0000-0002-6227-984X2021-01-182021-01-1820190035-8711http://hdl.handle.net/20.500.12386/29797We characterized 67P/Churyumov-Gerasimenko's cometary activity during its inbound arc before perihelion (2014 August-2015 January). We focused on the geomorphological regions of the Northern hemisphere observed by the ESA/Rosetta space probe during this time period. The GIADA dust detector characterized the physical properties of the fluffy and compact particles ejected from the nucleus; the VIRTIS imaging spectrometer detected exposed water ice.STAMPAen67P/Churyumov-Gerasimenko active areas before perihelion identified by GIADA and VIRTIS data fusionArticle10.1093/mnras/sty32442-s2.0-85061916487000462258200056https://academic.oup.com/mnras/article-abstract/483/2/2165/52287512019MNRAS.483.2165LFIS/05 - ASTRONOMIA E ASTROFISICAERC sectors::Physical Sciences and Engineering::PE9 Universe sciences: astro-physics/chemistry/biology; solar systems; stellar, galactic and extragalactic astronomy, planetary systems, cosmology, space science, instrumentation::PE9_2 Planetary systems sciences