A precision-dated ice-core nitrate record from Law Dome, coastal East Antar
ctica is compared to the timing of known solar proton events and geomagneti
c storms over the period 1888 to 1995. We find statistical evidence for a s
ignificant (P < 0.03) but small elevation in mean nitrate concentrations fo
llowing the solar events (<similar to> 11% over the 12 months beginning 3 m
onths post-event). While some solar events are identifiable in the nitrate
record, most are not distinguishable from the background noisy signal (whic
h has numerous large peaks), and some solar events show no nitrate elevatio
n above even mean levels.