Articles | Volume 16, issue 7
https://doi.org/10.5194/bg-16-1583-2019
https://doi.org/10.5194/bg-16-1583-2019
Research article
 | 
15 Apr 2019
Research article |  | 15 Apr 2019

Patterns of suspended particulate matter across the continental margin in the Canadian Beaufort Sea during summer

Jens K. Ehn, Rick A. Reynolds, Dariusz Stramski, David Doxaran, Bruno Lansard, and Marcel Babin

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Cited articles

Asplin, M. G., Galley, R., Barber, D. G., and Prinsenberg, S.: Fracture of summer perennial sea ice by ocean swell as a result of Arctic storms, J. Geophys. Res., 117, C06025, https://doi.org/10.1029/2011JC007221, 2012. a, b
Babin, M., Stramski, D., Ferrari, G. M., Claustre, H., Bricaud, A., Obolensky, G., and Hoepffner, N.: Variations in the light absorption coefficients of phytoplankton, nonalgal particles, and dissolved organic matter in coastal waters around Europe, J. Geophys. Res., 108, 3211, https://doi.org/10.1029/2001JC000882, 2003a. a
Babin, M., Morel, A., Fournier-Sicre, V., Fell, F., and Stramski, D.: Light scattering properties of marine particles in coastal and open ocean waters as related to the particle mass concentration, Limnol. Oceanogr., 48, 843–859, 2003b. a, b, c
Barber, D. G., Asplin, M. G., Gratton, Y., Lukovich, J. V., Galley, R. J., Raddatz, R. L., and Leitch, D.: The International polar year (IPY) circumpolar flaw lead (CFL) system study: Overview and the physical system, Atmos. Ocean, 48, 225–243, https://doi.org/10.3137/OC317.2010, 2010. a
Bélanger, S., Cizmeli, S. A., Ehn, J., Matsuoka, A., Doxaran, D., Hooker, S., and Babin, M.: Light absorption and partitioning in Arctic Ocean surface waters: impact of multiyear ice melting, Biogeosciences, 10, 6433–6452, https://doi.org/10.5194/bg-10-6433-2013, 2013. a, b, c, d, e
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Short summary
Beam attenuation at 660 nm and suspended particle matter (SPM) relationships were determined during the MALINA cruise in August 2009 to the Canadian Beaufort Sea in order to expand our knowledge of particle distributions in Arctic shelf seas. The relationship was then used to determine SPM distributions for four other expeditions to the region. SPM patterns on the shelf were explained by an interplay between wind forcing, river discharge, and melting sea ice that controls the circulation.
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