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Particle Flux Parameterizations: Quantitative and Mechanistic Similarities and Differences

Particle Flux Parameterizations: Quantitative and Mechanistic Similarities and Differences
The depth-attenuation of sinking particulate organic carbon (POC) is of particular importance for the ocean's role in the global carbon cycle. Numerous idealized flux-versus-depth relationships are available to parameterize this process in Earth System Models. Here we show that these relationships are statistically indistinguishable from available POC flux profile data. Despite their quantitative similarity, we also show these relationships have very different implications for the flux leaving the upper ocean, as well as for the mechanisms governing POC flux. We discuss how this tension might be addressed both observationally and in modeling studies.
- University of California, Santa Barbara United States
- Massachusetts Institute of Technology United States
- Natural Environment Research Council United Kingdom
- University of Georgia United States
- Woods Hole Oceanographic Institution, Physical Oceanography Department United States
Library of Congress Subject Headings: lcsh:QH1-199.5 lcsh:General. Including nature conservation, geographical distribution lcsh:Science lcsh:Q
Microsoft Academic Graph classification: Flux Atmospheric sciences Carbon cycle Particle flux Particulate organic carbon Particulate organic matter Earth system science Environmental science
Ocean Engineering, Aquatic Science, Oceanography, carbon export, carbon cycle, particulate organic matter, Water Science and Technology, Global and Planetary Change, martin curve, remineralization depth
Ocean Engineering, Aquatic Science, Oceanography, carbon export, carbon cycle, particulate organic matter, Water Science and Technology, Global and Planetary Change, martin curve, remineralization depth
Library of Congress Subject Headings: lcsh:QH1-199.5 lcsh:General. Including nature conservation, geographical distribution lcsh:Science lcsh:Q
Microsoft Academic Graph classification: Flux Atmospheric sciences Carbon cycle Particle flux Particulate organic carbon Particulate organic matter Earth system science Environmental science
19 references, page 1 of 2
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Buesseler, K. O., and Boyd, P. W. (2009). Shedding light on processes that control particle export and flux attenuation in the twilight zone of the open ocean. Limnol. Oceanogr. 54, 1210-1232. doi: 10.4319/lo.2009.54.4.1210
Buesseler, K. O., Steinberg, D. K., Michaels, A. F. Johnson, R. J., Andrews, J. E. Valdes, J. R., et al. (2000). A comparison of the quantity and quality of material caught in a neutrally buoyant versus surface- tethered sediment trap. Deep Sea Res. I 47, 277-294. doi: 10.1016/S0967-0637(99)00056-4
Burd, A. B., Hansell, D. A., Steinberg, D. K., Anderson, T. R., Aristegui, J., Baltar, F., et al. (2010). Assessing the apparent imbalance between geochemical and biochemical indicators of meso-and bathypelagic biological activity: What the $#! is wrong with present calculations of carbon budgets? Deep Sea Res. II 57, 1557-1571. doi: 10.1016/j.dsr2.2010.02.022
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Gloege, L., McKinley, G. A., Mouw, C. B., and Ciochetto, A. B. (2017). Global evaluation of particulate organic carbon flux parameterizations and implications for atmospheric pCO2. Glob. Biogeochem. Cycles 31, 1192-1215. doi: 10.1002/2016GB005535
Lutz, M., Dunbar, R., and Caldeira, K. (2002). Regional variability in the vertical flux of particulate organic carbon in the ocean interior. Glob. Biogeochem. Cycles 16, 11-1-11-18. doi: 10.1029/2000GB001383
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- University of California, Santa Barbara United States
- Massachusetts Institute of Technology United States
- Natural Environment Research Council United Kingdom
- University of Georgia United States
- Woods Hole Oceanographic Institution, Physical Oceanography Department United States
- University of California System United States
- University of Georgia Press United States
- Woods Hole Oceanographic Institution United States
The depth-attenuation of sinking particulate organic carbon (POC) is of particular importance for the ocean's role in the global carbon cycle. Numerous idealized flux-versus-depth relationships are available to parameterize this process in Earth System Models. Here we show that these relationships are statistically indistinguishable from available POC flux profile data. Despite their quantitative similarity, we also show these relationships have very different implications for the flux leaving the upper ocean, as well as for the mechanisms governing POC flux. We discuss how this tension might be addressed both observationally and in modeling studies.