Black carbon at a coastal Antarctic station (Syowa Station): seasonal variation and transport processes

Measurement of atmospheric black carbon (BC) was carried out at Syowa Station Antarctica (69゜00′S, 39゜35′E) from February 2004 until January 2007. The BC concentration at Syowa Station ranged from below detection to 176 ng m^. Higher BC concentrations were observed frequently from April until Octobe...

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Bibliographic Details
Main Authors: Keiichiro Hara, Kazuo Osada, Masanori Yabuki, Masahiko Hayashi, Takashi Yamanouchi, Masataka Shiobara, Makoto Wada
Format: Article in Journal/Newspaper
Language:English
Published: National Institute of Polar Research 2010
Subjects:
geo
Antarctic
The Antarctic
Austral
Neumayer
Syowa Station
Indian
Amundsen-Scott
Ferraz
Antarc*
Antarctica
Online Access:https://doi.org/10.15094/00009575
https://doaj.org/article/1f92f865d0ea450b9334471bd66a394f
Description
Summary:Measurement of atmospheric black carbon (BC) was carried out at Syowa Station Antarctica (69゜00′S, 39゜35′E) from February 2004 until January 2007. The BC concentration at Syowa Station ranged from below detection to 176 ng m^. Higher BC concentrations were observed frequently from April until October. Increase of BC concentration may be associated with poleward flow due to the approach of a cyclone and or blocking event during winter-spring. The BC-rich air masses traveled through the lower troposphere from the Atlantic and Indian Oceans to Syowa (Antarctic coast). During the summer (November-February), the BC concentration showed a diurnal variation together with surface wind speed and increased in the presence of katabatic wind from the Antarctic continent. Considering the low BC source strength over the Antarctic continent, the higher BC concentration in the continental air (katabatic wind) might be caused by long range transport of BC via the free troposphere from mid- and low- latitudes. The seasonal variation of BC at Syowa Station had a maximum in July-September, while at the other coastal stations (Halley, Neumayer, and Ferraz) and a continental station (Amundsen-Scott), the maximum occurred in October. This difference may result from different transport pathways, significant contribution of source regions and scavenging of BC by precipitation during the transport from the source regions. During the austral summer, long-range transport of BC via the free troposphere is likely to make an important contribution to the ambient BC concentration along the Antarctic coasts.

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