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AGU: Journal of Geophysical Research, Atmospheres

 

Keywords

  • Asian dust
  • dust deposition
  • East China Sea
  • mass-size distribution
  • marine biogeochemistry

Index Terms

  • Atmospheric Composition and Structure: Air/sea constituent fluxes
  • Atmospheric Composition and Structure: Constituent sources and sinks
  • Atmospheric Composition and Structure: Aerosols and particles
Abstract
Cited By (0)
 

Abstract

Dust deposition to the East China Sea and its biogeochemical implications

Shih-Chieh Hsu

Research Center for Environmental Changes, Academia Sinica, Taipei, Taiwan

Shaw Chen Liu

Research Center for Environmental Changes, Academia Sinica, Taipei, Taiwan

Richard Arimoto

Carlsbad Environmental Monitoring and Research Center, New Mexico State University, Carlsbad, New Mexico, USA

Tsun-Hsien Liu

Center for Environmental Studies, National Central University, Jhungli, Taiwan

Yi-Tang Huang

Research Center for Environmental Changes, Academia Sinica, Taipei, Taiwan

Fujung Tsai

Department of Marine Environmental Informatics, National Taiwan Ocean University, Keelung, Taiwan

Fei-Jan Lin

Institute of Oceanography, National Taiwan University, Taipei, Taiwan

Shuh-Ji Kao

Research Center for Environmental Changes, Academia Sinica, Taipei, Taiwan

Atmospheric Al concentrations published by Hsu et al. (2008) are used together with new information on mass particle-size distributions (MSDs) to calculate dust deposition to northern Taiwan and to evaluate the significance of the process for the East China Sea (ECS). Seasonal variations in aerosol Al in northern Taiwan show maxima in spring and winter and minima in summer and fall. The MSD of Al and Fe is monomodal, with a mean mass median diameter of 3.6 ± 1.2 μm, and the dry deposition velocity integrated over the entire MSD is 2.0 ± 1.5 cm s−1. The estimated dust deposition to the ECS is ∼20 g m−2 a−1, with wet deposition accounting for three fourths of the total. The quantity of dust deposited decreases exponentially with distance from the source regions. The annual dust input to the entire ECS is estimated to be ∼17 Mt, and when compared with riverine discharge, dust deposition appears to be a significant source of sediments and dissolved Fe. The large quantities of dust deposited also could have significant implications for the biogeochemical cycling of Fe (and Al), including effects on phytoplankton populations.

Received 1 October 2008; accepted 5 June 2009; published 13 August 2009.

Citation: Hsu, S.-C., S. C. Liu, R. Arimoto, T.-H. Liu, Y.-T. Huang, F. Tsai, F.-J. Lin, and S.-J. Kao (2009), Dust deposition to the East China Sea and its biogeochemical implications, J. Geophys. Res., 114, D15304, doi:10.1029/2008JD011223.

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