TEMPERATURE HISTORY AND ACCUMULATION TIMING FOR THE SNOWPACK AT GISP2, CENTRAL GREENLAND

Previous research has documented a close association between high-reso lution snow-pit profiles of hydrogen and oxygen stable-isotope ratios and multi-year Special Sensor Microwave/Imager (SSM/I) 37 GHz brightne ss temperature data in central Greenland. Comparison of the SSM/I data to profiles obtained during the 1989-91 field seasons indicated that delta D and delta(18)O data from the near-surface snow at the Greenlan d summit are a reliable, high-resolution temperature proxy. To test th is new technique further, additional stable-isotope data were obtained from a 2 m snow pit constructed during rate-June 1995 near the GISP2 site. This new profile, supported by pit stratigraphy and chemistry da ta, confirms the utility of comparing stable-isotope records with SSM/ I brightness temperatures. The sub-annual variation of the delta D rec ord at the GISP2 site was determined using 15 match points, from appro ximately December 1991 through June 1995 and was guided in part by tim e-constrained hear layers. The close association of these temperature proxies supports the assertion that snow accumulation occurs frequentl y through the year and that the isotope record initially contains temp erature information from many times of the year. This is also independ ently confirmed by analysis of H2O2 data. The slope of the multi-year T vs delta correlation was evaluated along with the sub-annual variati on in the amount, rate and timing of accumulation. These new results a re consistent with those from the previous study and they also demonst rate that the snow in this area initially contains temperature and che mical records with sub-annual resolution, This encourages confident in terpretation of the paleoclimatic signal variations in the GISP2 and G RIP deep cores.