Abstracts

Year-Round Major Ion Measurements at Greenland Environmental Observatory, Summit (GEOSummit)

Roger Bales¹, Ryan Banta², Joe McConnell³, Cyle Moon⁴, Liying Zhao^5
1Sierra Nevada Research Institute, University of California, Merced, 5200 N Lake Road, Merced, CA, 95343, USA, Phone 209-228-4348, rbales@ucmerced.edu
²Desert Research Institute, Reno, NV, , USA
³Desert Research Institute, Reno, NV, USA
⁴University of California, Merced, Merced, CA, USA
⁵University of California, Merced, Merced, CA, USA

Long-term year-round surface snow sampling at remote high latitude locations is fundamental to better understanding arctic geophysical processes. Research at the Greenland Environmental Observatory, Summit Station (GEOSummit) from 2003 to present includes high temporal resolution year-round ion chromatography (IC) measurements of surface snow and snow pit samples for Na, NH₄, K+, Mg2+, Ca2+, Cl-, NO3, SO₄2-, oxalate, MSA, acetate and formate. Many of these species exhibit annual cycles corresponding to source emissions. For example, Ca2+ exhibits a spring peak attributed to dust deposition, and formate exhibits a summer/fall peak associated with biomass burning. Monthly snow-pit major-ion sample measurements at 3-cm resolution indicate variability of many species are preserved within the snow pack. Concentrations are generally consistent with prior ice-core concentrations. Concurrently measured snow-accumulation rates exhibited relatively uniform intra-annual accumulation (5.9 cm/month +/- 4.3 cm, 1 sigma) with significant inter-annual variability. Snow-pit density values also show consistent trends with time as snow accumulates. These baseline measurements at GEOSummit will continue through another 5-year period to better characterize concentrations in snow on annual to decadal scales, and connections with source apportionment and atmospheric transport pathways.

Abstract Categories: 3.2 Low-latitude Forcing of Arctic Change