NMs record primarily the secondary nucleonic component (mostly neutrons) of the cosmic-ray induced atmospheric cascade with a small fraction of counts caused by muons. Its count rate is defined by the flux of primary (impinging on the top of the atmosphere) cosmic rays, as a combination of the cosmic-ray energy spectrum, detector's yield function and geomagnetic rigidity cutoff (Clem & Dorman, 2000;Mishev et al., 2020). The NM is an energy-integrating detector, with the effective energy ranging from about 12 GeV for polar NMs to 35 GeV for equatorial ones (Asvestari et al., 2017). The sensitivity of NMs to low-energy cosmic rays is highest in polar regions (low or no geomagnetic shielding) and high altitudes (lower atmospheric shielding) and decreases toward equatorial latitudes. The worldwide network of NMs can act as a giant spectrometer able to roughly estimate the spectrum of both galactic cosmic rays (e.g., Dorman, 2004) and relativistic solar protons (e.g., Duggal, 1979;Mishev et al., 2014). Along with the count rate, the multiplicity of NM counts (the average number of pulses within a short time interval) is sometimes studied (Balabin et al., 2011;Dorman, 2004) as a rough index of the spectral hardness of cosmic rays. Sometimes NM are accompanied by separate muon detectors to measure high-energy cosmic rays. This work is focused at two mini-NMs, DOMC and DOMB, located at the Concordia Antarctic Research station on top of Dome C, Central Antarctic plateau (75°06′S, 123°23′E, 3,233 m above sea level) (Poluianov et al., 2015). They are ones of the most sensitive NMs to lower energy cosmic rays (including solar energetic particles) thanks to the highly elevated polar location. Each NM has one BF 3 -filled detector surrounded by reflecting and moderating layers of polyethylene. In addition, DOMC has a layer of lead serving as a neutron Abstract A neutron monitor (NM) is, since the 1950s, a standard ground-based detector whose count rate reflects cosmic-ray variability. The worldwide network of NMs forms a rough spectrometer for cosmic rays. Recently, a brand-new data-acquisition (DAQ) system has been installed on the DOMC and DOMB NMs, located at the Concordia research station on the Central Antarctic plateau. The new DAQ system digitizes, at a 2-MHz sampling rate, and records all individual pulses corresponding to secondary particles in the detector. An analysis of the pulse characteristics (viz. shape, magnitude, duration, waiting time) has been performed, and several clearly distinguishable branches were identified: (A) corresponding to signal from individual secondary neutrons; (B) representing the detector's noise; (C) double pulses corresponding to the shortly separated nucleons of the same atmospheric cascades; (D) very-high multiple pulses which are likely caused by atmospheric muons; and (E) double pulses potentially caused by contamination of the neighboring detector. An analysis of the waiting-time distributions has revealed two clearly distinguishable peaks: peak (I) at about 1 ms being related to t...