ASSESSMENT OF ICE PARTICLE GROWTH-PROCESSES AT DYE-3, GREENLAND

As part of the DGASP program on the Greenland Ice Sheet, an investigat ion was conducted into the nature of ice particle formation processes that result in the formation of snow. Ice particle habits were determi ned using Formvar replicas of falling snow crystals. From these measur ements an assessment of the primary growth process and altitude of for mation was made. Results indicate that the scavenging of cloud water b y falling ice particles, growth by accretion or riming, rarely occurs. However, when riming does occur, it is usually associated with warmer air masses from the south. The occurrence of riming was also observed to be dependent on the season, with a greater frequency occuring duri ng warmer months. It was estimated that ice particle riming contribute s less than 5% of the average annual water mass, but up to 30% of the deposition of some chemical species, deposited to the Greenland Ice Sh eet at Dye 3. Ice particle habits indicate that they originate at high er altitudes above the ice cap in summer than in winter. Variations in the magnitude of ice particle riming, the elevation of origin of ice particles, the meteorology and the season of the year are all essentia l when interpreting snow chemistry and comparing snow and aerosol chem istry at Dye 3.