C31C-0337:
Holocene climate at Siple Dome, West Antarctica, using bubble number-density.
C31C-0337:
Holocene climate at Siple Dome, West Antarctica, using bubble number-density.
Wednesday, 17 December 2014
Abstract:
Past allowable accumulation rate/temperature combinations from Holocene ice core samples at Siple Dome, West Antarctica, are estimated from the measured number-density of bubbles. Mass density increase and grain growth in polar firn both are controlled by temperature and accumulation rate, and their integrated effects are recorded in the number-density of bubbles as the firn changes to ice1, 2. Siple Dome bubble number-densities show an early-Holocene high in accumulation rate followed by an approximately 10% reduction in accumulation rate between 11.33 ka and 1.863 ka.1. Spencer, M.K., R.B. Alley and J.J. Fitzpatrick. Developing a bubble number-density paleoclimatic indicator for glacier ice, J. Glaciol. 52(178), 358-364 (2006).
2. J.M. Fegyveresi, et al., Late-Holocene climate evolution at the WAIS Divide site, West Antarctica: bubble number-density estimates, J. Glaciol., 57(204) , 629 – 638 (2011).