Q. Yang et al., CHEMICAL-SPECIES SPATIAL-DISTRIBUTION AND RELATIONSHIP TO ELEVATION AND SNOW ACCUMULATION RATE OVER THE GREENLAND ICE-SHEET, JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 101(D13), 1996, pp. 18629-18637
Major chemical species (Cl-, NO3-, SO42-, Na+, K+, Mg2+, Ca2+) from 24
snowpits (sampled at a resolution of 3 cm, total 2995 samples) collec
ted from northern, central, and southern Greenland were used for this
investigation. The annual and seasonal (winter and summer) concentrati
on of each chemical species was calculated and used to study the spati
al distribution of chemical species over the central portion of the Gr
eenland Ice Sheet. A two-sided t-distribution test (alpha=0.05) sugges
ts that concentrations of major chemical species in snow do not vary s
ignificantly over this portion of central Greenland. The relationship
between chemical concentration and snow accumulation rate was investig
ated using annual data from two groups of snowpits: those from coastal
sites (northern and southern Greenland); and those from high-altitude
inland sites (central Greenland). The snowpit data from a single grou
p, when examined independently of the other group, show that chemical
concentrations do not vary with snow accumulation rate. However, when
data from the two groups are integrated into a single data set, pseudo
relationships appear, with NO3- concentration decreasing and Na+, K+,
Mg2+, and Cl- increasing as snow accumulation rate increases. Therefor
e we suggest that it is improper to study the relationship between che
mical concentration and snow accumulation rate by using data collected
from different geographic sites. The relationship between elevation a
nd chemical concentration was investigated using the same suite of ann
ual data sets. We find that Cl-, Na+, and Mg2+ concentrations decrease
, while NO3- concentration increases, with increasing elevation on the
Greenland Ice Sheet.