Low time resolution analysis of polar ice cores cannot detect impulsive nitrate events

作者: C. M. Laird , D. F. Smart , A. L. Melott , M. A. Shea

DOI: 10.1002/2014JA020378

关键词: Sedimentary depositional environmentNitrateGeophysicsIce sheetGreenland ice sheetIce coreGeologyPolarClimate changeSolar storm of 1859

摘要: Ice cores are archives of climate change and possibly large solar proton events (SPEs). Wolff et al. (2012) used a single event, nitrate peak in the GISP2-H core, which McCracken (2001a) time associated with poorly quantified 1859 Carrington to discredit SPE-produced, impulsive deposition polar ice. This is not ideal test case. We critique analysis demonstrate that data they cannot detect because resolution limitations. suggest re-examination top Greenland ice sheet at key intervals over last two millennia attention fine replicate sampling multiple species. will allow further insight into depositional processes on sub-seasonal scale, including atmospheric sources, transport mechanisms sheet, post-depositional interactions, potential SPE association.

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