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Mineral dust and major ion concentrations in snowpit samples from the NEEM site, Greenland

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Mineral dust and major ion concentrations in snowpit samples from the NEEM site, Greenland
Other Titles
그린랜드 NEEM 주상눈시료의 광물성 입자와 주요이온
Kang, Jung-Ho
Hong, Sung-Min
Lee, Jeonghoon
Choi, Sung-Deuk
Hur, Soon Do
Hong, Sang-Bum
Hwang, Heejin
major ions; Atmospheric mineral dust; Greenland snow; seasonal variation
Issue Date
Kang, Jung-Ho, et al. 2015. "Mineral dust and major ion concentrations in snowpit samples from the NEEM site, Greenland". ATMOSPHERIC ENVIRONMENT, 120(1): 137-143.
Polar ice sheets conserve atmospheric aerosols at the time of snowfall, which can be used to reconstruct past climate and environmental conditions. We investigated mineral dust and major ion records in snowpit samples obtained from the northwestern Greenland ice sheet near the North Greenland Eemian Ice Drilling (NEEM) camp in June 2009. We analyzed the samples for mineral dust concentrations as well as stable water isotopes (δ18O, δD, and deuterium excess) and major ions (Cl?, SO42?, methanesulfonic acid (MSA), Na+, and Ca2+). Seasonal δ18O and δD cycles indicate that the snowpit samples covered a six-year period from spring 2003 to early summer 2009. Concentrations of mineral dust, nss-Ca2+, and nss-SO42? showed seasonal deposition events with maxima in the winter?spring layers. On the other hand, the Cl?/Na+ ratio and the concentrations of MSA exhibited maxima in the summer layers, making them useful indicators for the summer season. Moreover, an anomalous atmospheric mineral dust event was recorded at a depth of 165?170 cm corresponding to late winter 2005 to spring 2006. A back trajectory analysis suggests that a major contributor to the Greenland aerosol was an air mass passing over the Canadian Arctic and North America. Several trajectories point to Asian regions as a dust source. The mineral dust deposited at NEEM was strongly influenced by long-range atmospheric transport and dust input from arid source areas in northern China and Mongolia.
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