O2/N2/Ar ratios, and the isotopic composition of O2 and N2, in firn air from the Megadunes site, Antarctica

This site is marked by actively migrating snow dunes and very large ice crystals develop on the windward side. Severinghaus' objective was to examine the extent of convection in these dunes, and the possibility that firn air at depth could be very old.

We analyzed the firn air samples for the O2/N2/Ar ratio and the isotopic composition of O2 and N2. The isotopic and elemental data define the extent of convection in the firn and give information about the degree of graviational fractionation, with which a gravitational correction can be made for the abundance of other species.