Context. We explore the impact of interactions between coronal  mass ejections (CMEs) – known as CME–CME interactions – on Earth using  remote-sensing and in situ observations and estimate the amplification  of the geo-effectiveness of the individual CMEs by a factor of ∼2 due to  CME–CME interactions.
Aims. We present 3D reconstructions of interacting CMEs, which  provide essential information on the orientation and interaction of the  events. Additionally, we analysed coronal evolution of CMEs and their  in situ characteristics at 1 AU to explore the impact of interactions  between CMEs on their geo-effectiveness.
Methods. We analysed CME interaction using white light data  from LASCO and STEREO COR-A. The reported CMEs were reconstructed using  the gradual cylindrical shell (GCS) model and simulated  self-consistently with the physics-based 3D MHD model EUHFORIA (EUropean  Heliosphere FORecasting Information Asset). By running different  simulations, we estimated the geo-effectiveness of both individual and  interacting CMEs using an empirical relationship method for the  disturbance storm index.
Results. The SOHO/LASCO spacecraft observed three CMEs  erupting from the Sun within an interval of 10 h during a very active  period in early November 2021. There were two partial halo CMEs that  occurred on 1 Nov. 2021 at 19:00 UT and 22:00 UT, respectively, from the  active region 12887 (S28W58), and a third halo CME occurred from AR  12891 (N17E03) on 2 Nov. 2021 at 02:48 UT. By combining remote  observations close to the Sun, in situ data at 1 AU, and further  numerical analyses of each individual CME, we are able to identify the  initial and interplanetary evolution of the CMEs.
Conclusions. (i) White light observations and a 3D  reconstruction of the CMEs show cannibalism by CME-2 on CME-1 and a  flank interaction of CME-3 with the merged CME-1 and CME-2 at 45–50 Rs.  (ii) Interacting CMEs exhibit an increase in geo-effectiveness compared  to an individual CME.
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