Black carbon (BC), with strong optical absorption, is emitted to the atmosphere from natural and anthropogenic combustion processes. After BC deposition onto snow surfaces, BC can alter the Earth’s surface albedo, which is related closely to climate effects in polar regions. However, the BC source strength is slight or negligible in Antarctic regions. Therefore, BC is useful as a tracer for long-range transport from low latitudes and mid-latitudes into Antarctic regions. Continuous BC measurements have been taken at Syowa Station, Antarctica, with an aethalometer since 2005 and with a multi-angle absorption photometer (MAAP) since 2016 to elucidate transport processes of atmospheric substances to the Antarctic and to assess climate effects. Daily mean BC data after the screening of locally contaminated data are provided herein.
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