Abstract
In 1998 fresh surface snow samples were collected, no more than 2 days after the snowfall, along the Khumbu valley, and its lateral valleys (Kongmala and Changri Nup), at the end of the summer monsoon period. Samples from the Island Peak and Pumori slopes were also collected by climbers during pre- and post-monsoon season at altitudes ranging from 5300 to 6100 m a.s.l. Conductivity, pH and major inorganic ions were measured in samples and relative field blanks. Chemical results were subjected to principal component analysis (PCA) in order to distinguish different sources of ions and study spatial and temporal distribution of ion concentrations. Two main factors, accounting for more than 80% of the total variance, were found. The two factors were correlated to two different sources, one representing local transport and background contribution, and the other related to monsoon circulation. Concentrations of the main ions were compared to those measured in other remote areas, with particular regard to elevated areas in Central Asia.
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