The conventional definition of ground level enhancement (GLE) events requires detection of solar energetic particles (SEP) by at least two differently located neutron monitors. Some places are exceptionally suitable for ground-based detection of SEP -high-elevation polar regions with negligible geomagnetic and reduced atmospheric energy/rigidity cutoffs. At present, there are two neutron-monitor stations in such locations on the Antarctic plateau: SOPO/SOPB (at Amundsen-Scott station, 2835 m elevation) and DOMC/ DOMB (at Concordia station, 3233 m elevation). Since 2015, when the DOMC/ DOMB station started continuous operation, a relatively weak SEP event, not detected by sea-level neutron-monitor stations, was registered by both SOPO/ SOPB and DOMC/DOMB and accordingly classified as a GLE. This would lead to a distortion of the homogeneity of the historic GLE list and the corresponding statistics. To address this issue, we propose to modify the GLE definition so that it keeps the homogeneity: A GLE event is registered when there are near-time coincident and statistically significant enhancements of the count rates of at least two differently located neutron monitors including at least one neutron monitor near sea level and a corresponding enhancement in the proton flux measured by a space-borne instrument(s). Relatively weak SEP events registered only by highaltitude polar neutron monitors, but with no response from cosmic-ray stations at sea level, can be classified as sub-GLEs.