Global variability of optical backscattering by non-algal particles from a Biogeochemical-Argo dataset
Bellacicco, M; Cornec, M; Organelli, E; et al.Brewin, RJW; Neukermans, G; Volpe, G; Barbieux, M; Poteau, A; Schmechtig, C; D'Ortenzio, F; Marullo, S; Claustre, H; Pitarch, J
Date: 2 October 2019
Journal
Geophysical Research Letters
Publisher
American Geophysical Union (AGU)
Publisher DOI
Abstract
Understanding spatial and temporal dynamics of non-algal particles in open ocean is of the utmost importance to improve estimations of carbon export and sequestration. These particles covary with phytoplankton abundance but also accumulate independently of algal dynamics. The latter likely represents an important fraction of organic ...
Understanding spatial and temporal dynamics of non-algal particles in open ocean is of the utmost importance to improve estimations of carbon export and sequestration. These particles covary with phytoplankton abundance but also accumulate independently of algal dynamics. The latter likely represents an important fraction of organic carbon, but it is largely overlooked. A possible way to study these particles is via their optical backscattering properties (bbp) and relationship with chlorophyll-a (Chl). To this aim, we estimate the fraction of bbp associated with the non-algal particle portion (bkbp) that does not covary with Chl by using a global Biogeochemical-Argo data set. We quantify the spatial, temporal, and vertical variability of bkbp. In the northern productive areas, bkbp is a small fraction of bbp and shows a clear seasonal cycle. In the Southern Ocean, bkbp is a major fraction of total bbp. In oligotrophic areas, bkbp has a smooth annual cycle.
Geography - old structure
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