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국회도서관 홈으로 정보검색 소장정보 검색

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A continuous series of 60 snow samples was collected at a 2.5-cm interval from a 1.5-m snow pit at a site on the Styx Glacier Plateau in Victoria Land, Antarctica, during the 2011/2012 austral summer season. Various chemical components (δD, δ18O, Na+, K+, Mg2+, Ca2+, Cl−, SO4 2−, NO3 −, F−, CH3SO3 −, CH3CO2− and HCO2−) were determined to understand the highly resolved seasonal variations of these species in the coastal atmosphere near the Antarctic Jang Bogo station. Based on vertical profiles of δ18O, NO3− and MSA, which showed prominent seasonal changes in concentrations, the snow samples were dated to cover the time period from 2009 austral winter to 2012 austral summer with a mean accumulation rate of 226 kg H2O m−2 yr−1. Our snow profiles show pronounced seasonal variations for all the measured chemical species with a different pattern between different species. The distinctive feature of the occurrence patterns of the seasonal variations is clearly linked to changes in the relative strength of contributions from various natural sources (sea salt spray, volcanoes, crust-derived dust, and marine biogenic activities) during different short-term periods. The results allow us to understand the transport pathways and input mechanisms for each species and provide valuable information that will be useful for investigating long-term (decades to century scale periods) climate and environmental changes that can be deduced from an ice core to be retrieved from the Styx Glacier Plateau in the near future.

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참고문헌 (43건) : 자료제공( 네이버학술정보 )

참고문헌 목록에 대한 테이블로 번호, 참고문헌, 국회도서관 소장유무로 구성되어 있습니다.
번호 참고문헌 국회도서관 소장유무
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31 Pilson MEQ (1998) An Introduction to the Chemistry of the Sea. Prentice Hall, New Jersey, 431 p 미소장
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33 Rankin AM, Auld V, Wolff EW (2000) Frost flowers as a source of fractionated sea salt aerosol in the polar regions. Geophys Res Lett 27(21):3469-3472 미소장
34 Severi M, Becagli S, Castellano E, Morganti A, Traversi R, Udisti R (2009) Thirty years of snow deposition at Talos Dome (Northern Victoria Land, East Antarctica): chemical profiles and climatic implications. Microchem J 92(1):15-20 미소장
35 Stenni B, Serra F, Frezzotti M, Maggi V, Traversi R, Becagli S, Udisti R (2000) Snow accumulation rates in northern Victoria Land, Antarctica, by firn-core analysis. J Glaciol 46(155):541-552 미소장
36 Wagnon P, Delmas RJ, Legrand M (1999) Loss of volatile acid species from upper firn layers at Vostok, Antarctica. J Geophys Res 104(D3):3423-3431 미소장
37 Weller R, Traufetter F, Fischer H, Oerter H, Piel C, Miller H (2004) Postdepositional losses of methane sulfonate, nitrate, and chloride at the European Project for Ice Coring in Antarctica deep-drilling site in Dronning Maud Land, Antarctica. J Geophys Res 109:D07301. doi:10.1029/2003JD004189 미소장
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41 Whitlow S, Mayewski PA, Dibb JE (1992) A comparison of major chemical species seasonal concentration and accumulation at the South Pole and Summit, Greenland. Atmos Environ 26(11):2045-2054 미소장
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43 Wolff EW, Barbante C, Becagli S, Bigler M, Boutron CF, Castellano E, de Angelis M, Federer U, Fischer H, Fundel F, Hansson M, Hutterli M, Jonsell U, Karlin T, Kaufmann P, Lambert F, Littot GC, Mulvaney R, Rothlisberger R, Ruth U, Severi M, Siggaard-Andersen ML, Sime LC, Steffensen JP, Stocker TF, Traversi R, Twarloh B, Udisti R, Wagenbach D, Wegner A (2010)Changes in environment over the last 800,000 years from chemical analysis of the EPICA Dome C ice core. Quaternary Sci Rev 29:285-295 미소장