The Effect of Typhoon on Particulate Organic Carbon Flux in the Southern
Biogeosciences, 7, 3007–3018, 2010 www.biogeosciences.net/7/3007/2010/ Biogeosciences doi:10.5194/bg-7-3007-2010 © Author(s) 2010. CC Attribution 3.0 License. The effect of typhoon on particulate organic carbon flux in the southern East China Sea C.-C. Hung1, G.-C. Gong1, W.-C. Chou1, C. -C. Chung1,2, M.-A. Lee3, Y. Chang3, H.-Y. Chen4, S.-J. Huang4, Y. Yang5, W.-R. Yang5, W.-C. Chung1, S.-L. Li1, and E. Laws6 1Institute of Marine Environmental Chemistry and Ecology, National Taiwan Ocean University, Keelung, 20224, Taiwan 2Center for Marine Bioenvironment and Biotechnology, National Taiwan Ocean University, Keelung, 20224, Taiwan 3Department of Environmental Biology and Fisheries Science, National Taiwan Ocean University, Keelung, 20224, Taiwan 4Department of Marine Environmental Informatics, National Taiwan Ocean University, Keelung, 20224, Taiwan 5Taiwan Ocean Research Institute, National Applied Research Laboratories, Taipei, Taiwan 6Department of Environmental Sciences, School of the Coast and Environment, Louisiana State University, Baton Rouge, LA 70803, USA Received: 16 April 2010 – Published in Biogeosciences Discuss.: 19 May 2010 Revised: 16 September 2010 – Accepted: 21 September 2010 – Published: 4 October 2010 Abstract. Severe tropical storms play an important role in suggested that during non-typhoon conditions approximately triggering phytoplankton blooms, but the extent to which half of the export of organic carbon occurs via convective such storms influence biogenic carbon flux from the eu- mixing of dissolved organic carbon, a conclusion consistent photic zone is unclear. In 2008, typhoon Fengwong pro- with earlier work at comparable latitudes in the open ocean. vided a unique opportunity to study the in situ biologi- cal responses including phytoplankton blooms and particu- late organic carbon fluxes associated with a severe storm in 1 Introduction the southern East China Sea (SECS).
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