TY - JOUR
T1 - Reconciliation of total particulate organic carbon and nitrogen measurements determined using contrasting methods in the North Pacific Ocean as part of the NASA EXPORTS field campaign
AU - Graff, Jason R.
AU - Nelson, Norman B.
AU - Roca-Martí, Montserrat
AU - Kramer, Sasha J.
AU - Erickson, Zach
AU - Cetinić, Ivona
AU - Buesseler, Ken O.
AU - Passow, Uta
AU - Zhang, Xiaodong
AU - Benitez-Nelson, Claudia
AU - Bisson, Kelsey
AU - Close, Hilary G.
AU - Crockford, Taylor
AU - Fox, James
AU - Halewood, Stuart
AU - Lam, Phoebe
AU - Roesler, Collin
AU - Sweet, Julia
AU - VerWey, Brian
AU - Xiong, Yuanheng
AU - Siegel, David A.
N1 - Funding Information:
KOB, CBN, MRM: NASA 80NSSC17K0555, WHOI’s Twilight Zone study (MRM, KOB), and the Ocean Frontier Institute International Postdoctoral Fellowship Program (MRM).
Funding Information:
The authors would like to thank NASA and NSF for logistical and financial support, the captains, crews, and marine technicians of the R/V Revelle and R/V Ride, chief scientists Norm Nelson, Mary Jane Perry, Debbie Steinberg and Jason Graff and additional members of the NASA EXPORTS Project Office for organizing the complexities of a multi-platform field campaign. Thanks to Adrian Marchetti and Meredith Meyer for size-fractionated chlorophyll data. The authors would like to acknowledge Steven Pike for his essential role in making the in situ pump deployments possible and Blaire P. Umhau for her work in processing pump filters at sea. The authors also would like to thank two reviewers whose insights and comments helped to clarify and improve the manuscript. This is PMEL Contribution Number 5421.
Funding Information:
The authors would like to thank NASA and NSF for logistical and financial support, the captains, crews, and marine technicians of the R/V Revelle and R/V Ride, chief scientists Norm Nelson, Mary Jane Perry, Debbie Steinberg and Jason Graff and additional members of the NASA EXPORTS Project Office for organizing the complexities of a multi-platform field campaign. Thanks to Adrian Marchetti and Meredith Meyer for size-fractionated chlorophyll data. The authors would like to acknowledge Steven Pike for his essential role in making the in situ pump deployments possible and Blaire P. Umhau for her work in processing pump filters at sea. The authors also would like to thank two reviewers whose insights and comments helped to clarify and improve the manuscript. This is PMEL Contribution Number 5421. JRG, JF, BV: NASA 80NSSC17K0568. DAS, NBN, KB, SJK, UP, ER, JS, SH: NASA 80NSSC17K0 692. KOB, CBN, MRM: NASA 80NSSC17K0555, WHOI’s Twilight Zone study (MRM, KOB), and the Ocean Frontier Institute International Postdoctoral Fellowship Program (MRM). XZ, YX: NASA 80NSSC17K0656 and 80NSSC20K0350. PL: NASA 80NSSC17K0555, NSF-OCE 1829614. HGC: NSF 1830016. CR, TC: NASA 80NSSC17K0700. IC: NASA EXPORTS Project Office and NASA PACE Mission. ZE: NASA Postdoctoral Program, administered by the Universities Space Research Association.
Publisher Copyright:
© 2023 University of California Press. All rights reserved.
PY - 2023/12/1
Y1 - 2023/12/1
N2 - Measurements of particulate organic carbon (POC) are critical for understanding the ocean carbon cycle, including biogenic particle formation and removal processes, and for constraining models of carbon cycling at local, regional, and global scales. Despite the importance and ubiquity of POC measurements, discrepancies in methods across platforms and users, necessary to accommodate a multitude of needs and logistical constraints, commonly result in disparate results. Considerations of filter type and pore size, sample volume, collection method, and contamination sources underscore the potential for dissimilar measurements of the same variable assessed using similar and different approaches. During the NASA EXport Processes in the Ocean from RemoTe Sensing (EXPORTS) 2018 field campaign in the North Pacific Ocean, multiple methodologies and sampling approaches for determining POC were applied, including surface inline flow-through systems and depth profiles using Niskin bottles, in situ pumps, and Marine Snow Catchers. A comparison of results from each approach and platform often resulted in significant differences. Supporting measurements, however, provided the means to normalize results across datasets. Using knowledge of contrasting protocols and synchronous or near-synchronous measurements of associated environmental variables, we were able to reconcile dataset differences to account for undersampling of some particle types and sizes, possible sample contamination and blank corrections. These efforts resulted in measurement agreement between initially contrasting datasets and insights on long-acknowledged but rarely resolved discrepancies among contrasting methods for assessing POC concentrations in the ocean.
AB - Measurements of particulate organic carbon (POC) are critical for understanding the ocean carbon cycle, including biogenic particle formation and removal processes, and for constraining models of carbon cycling at local, regional, and global scales. Despite the importance and ubiquity of POC measurements, discrepancies in methods across platforms and users, necessary to accommodate a multitude of needs and logistical constraints, commonly result in disparate results. Considerations of filter type and pore size, sample volume, collection method, and contamination sources underscore the potential for dissimilar measurements of the same variable assessed using similar and different approaches. During the NASA EXport Processes in the Ocean from RemoTe Sensing (EXPORTS) 2018 field campaign in the North Pacific Ocean, multiple methodologies and sampling approaches for determining POC were applied, including surface inline flow-through systems and depth profiles using Niskin bottles, in situ pumps, and Marine Snow Catchers. A comparison of results from each approach and platform often resulted in significant differences. Supporting measurements, however, provided the means to normalize results across datasets. Using knowledge of contrasting protocols and synchronous or near-synchronous measurements of associated environmental variables, we were able to reconcile dataset differences to account for undersampling of some particle types and sizes, possible sample contamination and blank corrections. These efforts resulted in measurement agreement between initially contrasting datasets and insights on long-acknowledged but rarely resolved discrepancies among contrasting methods for assessing POC concentrations in the ocean.
KW - High-performance liquid chromatography
KW - Particle size distribution
KW - Particulate backscattering
KW - Particulate beam attenuation
KW - Particulate organic carbon and nitrogen
KW - Phytoplankton pigments
UR - http://www.scopus.com/inward/record.url?scp=85180297987&partnerID=8YFLogxK
UR - https://www.mendeley.com/catalogue/62f9a315-e606-3746-a5fc-d5fbbeb6b04e/
U2 - 10.1525/elementa.2022.00112
DO - 10.1525/elementa.2022.00112
M3 - Article
AN - SCOPUS:85180297987
SN - 2325-1026
VL - 11
JO - Elementa
JF - Elementa
IS - 1
M1 - 00112
ER -