[21] analyzed several parameters from the lithosphere, atmosphere, and ionosphere on the occasion of the 2019 M = 7.1 Ridgecrest EQ, finding an accelerated progression of the cumulative number of all anomalies as the mainshock was approaching. [PERSON] et al. [22] detected anomalous changes in the lithosphere, atmosphere, and ionosphere near the epicenter before the 2021 M = 7.4 Madoi EQ; meanwhile, [PERSON] and [PERSON] [23] analyzed the behavior of more than 50 different lithosphere-atmosphere-ionosphere anomalies during the preparation phase of the 2023 Turkey EQ, identifying a progressive increase in the number of anomalies starting about 10 days before, with the major peak the day before the mainshock. On 9 November 2022, at 06:07:25 UTC, an M\({}_{\rm L}\) = 5.7 (Mw = 5.5) EQ occurred approximately 30 km offshore the Marche coast in the Adriatic Sea, at latitude 43.984\({}^{\circ}\) N, longitude 13.324\({}^{\circ}\) E, and 5 km of depth. Just a minute after the mainshock, a strong aftershock of M\({}_{\rm L}\) = 5.2 occurred about 8 km south of the main event, at latitude 43.913\({}^{\circ}\) N, longitude 13.345\({}^{\circ}\) E, and 8 km of depth. The two major shocks activated a seismic sequence of about 400 aftershocks lasting a week, thirteen of them with M\({}_{\rm L}\) = 3.5. The seismic sequence occurred in correspondence with the frontal fault systems of the Northern Apennines, where ongoing convergence is accommodated on a series of buried faults, still poorly understood. The moment tensor solution of the mainshock indicates a reverse mechanism on a NW-SE trending fault plane, as well as the moment tensor solutions of the \(\mathrm{M_{L}}\geq 3.5\) events of the sequence. However, no moment tensor solution has been computed for the \(\mathrm{M_{L}}=5.2\) event due to the overlap and interference of phases from the two events [24]. According to [PERSON] et al. [24], the slip occurred along a thrust fault dipping approximately 24\({}^{\circ}\) SSW over a length of about 15 km, consistent with seismic reflection data propagating downward from the mainshock hypocenter, confirming the ongoing seismotectonic activity of this sector of the Apennines that is still propagating towards the foreland, approximately in a piggy-back thrust sequence. The area of greatest impact is along the coastal stretch between Fano and Ancona, where a maximum intensity of 5 European Macroseismic Scale (EMS-98) [25] has been estimated. Within this zone, very slight sporadic damages have been observed. Particularly, the district outskirts of Ancona have reported damages to recent reinforced concrete buildings, likely due to local amplification effects. The estimated maximum intensity reached 5 EMS-98 in some locations; however, macroseismic effects rapidly decreased to 4 EMS-98 inland, at a short distance from the coast [26]. This study aims to provide a comprehensive view of the effects observed on various geological and atmospheric layers within the framework of lithosphere-atmosphere-ionosphere coupling (LAIC) models, during the preparatory phase of the seismic event recorded offshore the coast of Marche on 9 November 2022. Previous studies related to this seismic event [24; 27; 28; 29; 30; 31] have predominantly focused on its tectonic and seismological aspects, while we adopted the LAIC approach as a novelty for this EQ. Additionally, the characteristics of this seismic event, such as the magnitude slightly below 6 and its occurrence at sea, piped our interest in investigating whether this approach could yield fruitful results. In particular, the presence of the sea conductive layer could limit the occurrence of one kind of LAIC instead of another. Figure 1 describes the parameters studied across different geological layers from bottom to top, looking for anomalous perturbations potentially associated with the preparation phase of the \(\mathrm{M_{L}}=5.7\) EQ. Specifically, seismicity acceleration preceding the mainshock is investigated in the lithosphere using the revised accelerated moment release (R-AMR) method.