Document Type
Article
Publication Title
Biogeosciences
Rights and Access Note
This Item is protected by copyright and/or related rights. You are free to use this item in any way that is permitted by copyright and related rights legislation that applies to your use. Rights assessment remains the responsibility of the researcher. In addition, no permission is required from the rights-holder(s) for non-commercial uses.
Publication Date
8-28-2013
First Page
5517
Last Page
5531
Issue Number
8
Volume Number
10
Abstract/ Summary
Observational gaps limit our understanding of particle flux attenuation through the upper mesopelagic because available measurements (sediment traps and radiochemical tracers) have limited temporal resolution, are labor-intensive, and require ship support. Here, we conceptually evaluate an autonomous, optical proxy-based method for high-resolution observations of particle flux. We present four continuous records of particle flux collected with autonomous profiling floats in the western Sargasso Sea and the subtropical North Pacific, as well as one shorter record of depth-resolved particle flux near the Bermuda Atlantic Time-series Study (BATS) and Oceanic Flux Program (OFP) sites. These observations illustrate strong variability in particle flux over very short (∼1-day) timescales, but at longer timescales they reflect patterns of variability previously recorded during sediment trap time series. While particle flux attenuation at BATS/OFP agreed with the canonical power-law model when observations were averaged over a month, flux attenuation was highly variable on timescales of 1-3 days. Particle fluxes at different depths were decoupled from one another and from particle concentrations and chlorophyll fluorescence in the immediately overlying surface water, consistent with horizontal advection of settling particles. We finally present an approach for calibrating this optical proxy in units of carbon flux, discuss in detail the related, inherent physical and optical assumptions, and look forward toward the requirements for the quantitative application of this method in highly time-resolved studies of particle export and flux attenuation.
Repository Citation
Estapa, M. L.; Buesseler, K.; Boss, E.; and Gerbi, G., "Autonomous, high-resolution observations of particle flux in the oligotrophic ocean" (2013). Marine Sciences Faculty Scholarship. 172.
https://digitalcommons.library.umaine.edu/sms_facpub/172
Citation/Publisher Attribution
Estapa, M.L., K. Buesseler, E. Boss, and G. Gerbi, 2013. Autonomous, high-resolution observations of particle flux in the oligotrophic ocean, Biogeosciences, 10, 5517-5531.
Publisher Statement
© 2013 Author(s)
DOI
10.5194/bg-10-5517-2013
Version
publisher's version of the published document