In Situ Estimates of Net Primary Production in the Western North Atlantic With Argo Profiling Floats

The (14)C incubation method for net primary production (NPP) has limited spatial/temporal resolution, while satellite approaches cannot provide direct information at depth. With chlorophyll‐a and backscatter measurements from BGC‐Argo floats, we quantified year‐round NPP in the western North Atlanti...

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Bibliographic Details
Published in:Journal of Geophysical Research: Biogeosciences
Main Authors: Yang, Bo, Fox, James, Behrenfeld, Michael J., Boss, Emmanuel S., Haëntjens, Nils, Halsey, Kimberly H., Emerson, Steven R., Doney, Scott C.
Format: Text
Language:English
Published: John Wiley and Sons Inc. 2021
Subjects:
Research Article
North Atlantic
Online Access:http://www.ncbi.nlm.nih.gov/pmc/articles/PMC9286042/
http://www.ncbi.nlm.nih.gov/pubmed/35866055
https://doi.org/10.1029/2020JG006116
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Summary:The (14)C incubation method for net primary production (NPP) has limited spatial/temporal resolution, while satellite approaches cannot provide direct information at depth. With chlorophyll‐a and backscatter measurements from BGC‐Argo floats, we quantified year‐round NPP in the western North Atlantic Ocean using both the Carbon‐based Productivity Model (CbPM) and Photoacclimation Productivity Model (PPM). Comparison with NPP profiles from (14)C incubation measurements showed advantages and limitations of both models. CbPM reproduced the magnitude of NPP in most cases. However, in the summer the CbPM‐based NPP had a large peak in the subsurface, which was an artifact from the subsurface chlorophyll maximum caused by photoacclimation. PPM avoided the artifacts from photoacclimation, but the magnitude of PPM‐derived NPP was smaller than the (14)C result. Different NPP distribution patterns along a North‐South transect in the Western North Atlantic Ocean were observed, including higher winter NPP/lower summer NPP in the south, timing differences in NPP seasonal phenology, and different NPP depth distribution patterns in the summer months. Using a 6‐months record of concurrent oxygen and bio‐optical measurements from two Argo floats, we also demonstrated the ability of Argo floats to obtain estimates of the net community production to NPP ratio, ranging from 0.3 in July to −1.0 in December 2016. Our results highlight the utility of float bio‐optical profiles and indicate that environmental conditions (e.g., light availability, nutrient supply) are major factors controlling the seasonality and spatial (horizontal and vertical) distributions of NPP in the western North Atlantic Ocean.

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