Global Biogeochemical Cycles (2014) 28 Annual net community production and the biological carbon flux in the ocean Steven Emerson School of Oceanography,

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Presentation transcript:

Global Biogeochemical Cycles (2014) 28 Annual net community production and the biological carbon flux in the ocean Steven Emerson School of Oceanography, University of Washington, Seattle, Washington, USA Abstract The flux of biologically produced organic matter from the surface ocean (the biological pump), over an annual cycle, is equal to the annual net community production (ANCP). Experimental determinations of ANCP at ocean time series sites using a variety of different metabolite mass balances have made it possible to evaluate the accuracy of sediment trap fluxes and satellite-determined ocean carbon export. ANCP values at the Hawaii Ocean Time-series (HOT), the Bermuda Atlantic Time-series Study (BATS), Ocean Station Papa (OSP) are 3 ± 1 mol C m-2 y-1 — much less variable than presently suggested by satellite remote sensing measurements and global circulation models. ANCP determined from mass balances at these locations are 3–4 times particulate organic carbon fluxes measured in sediment traps. When the roles of dissolved organic carbon (DOC) flux, zooplankton migration, and depth-dependent respiration are considered these differences are reconciled at HOT and OSP but not at BATS, where measured particulate fluxes are about 3 times lower than expected. Even in the cases where sediment trap fluxes are accurate, it is not possible to “scale up” these measurements to determine ANCP without independent determinations of geographically variable DOC flux and zooplankton migration. Estimates of ANCP from satellite remote sensing using net primary production determined by the carbon-based productivity model suggests less geographic variability than its predecessor (the vertically generalized productivity model) and brings predictions at HOT and OSP closer to measurements; however, satellite-predicted ANCP at BATS is still 3 times too low.

Annual net community production and the biological carbon flux in the ocean Global Biogeochemical Cycles Volume 28, Issue 1, pages 14-28, 13 JAN 2014 DOI: /2013GB Volume 28, Issue 1,

Annual net community production and the biological carbon flux in the ocean Global Biogeochemical Cycles Volume 28, Issue 1, pages 14-28, 13 JAN 2014 DOI: /2013GB Volume 28, Issue 1,

Annual net community production and the biological carbon flux in the ocean Global Biogeochemical Cycles Volume 28, Issue 1, pages 14-28, 13 JAN 2014 DOI: /2013GB Volume 28, Issue 1,

Annual net community production and the biological carbon flux in the ocean Global Biogeochemical Cycles Volume 28, Issue 1, pages 14-28, 13 JAN 2014 DOI: /2013GB Volume 28, Issue 1,

Annual net community production and the biological carbon flux in the ocean Global Biogeochemical Cycles Volume 28, Issue 1, pages 14-28, 13 JAN 2014 DOI: /2013GB Volume 28, Issue 1,

Annual net community production and the biological carbon flux in the ocean Global Biogeochemical Cycles Volume 28, Issue 1, pages 14-28, 13 JAN 2014 DOI: /2013GB Volume 28, Issue 1,

Annual net community production and the biological carbon flux in the ocean Global Biogeochemical Cycles Volume 28, Issue 1, pages 14-28, 13 JAN 2014 DOI: /2013GB Volume 28, Issue 1,

Models 10, 13b Anderson and Sarmiento, 1995 (Nutrient restoring) 10 Yamanaka and Tajika, 1996 (Nutrient restoring) Six and Maier-Reimer, 1996 (Nutrient and T model) 13, 10c Bopp et al., 2001 (Nutrient and T model) (Ecosystem model) Moore et al., 2002 (Ecosystem) 13 Schlitzer, 2004 (Nutrient restoring, inverse model) 14 ± 5d Najjar et al., 2007 (Mean of five models) (Nutrient restoring) 12 ± 2e4.2 ± ± ± ±.8 Satellite Based 11 Laws et al., f Dunne et al., g (NCP/NPP from Dunne et al., 2005) 12h –13 Laws et al., Westberry et al., ± 12.1 ± ± ± ±.4 Table 1 Zonally Averaged Annual NCP 0–15° 15–30° 30–45° 45–60°

Table 2. Annual Net Community Production (ANCP) Determined by Oxygen, δ13C-DIC Mass Balance, and NO3 - Drawdown Location Annual NCP (mol C m-2 yr-1) E. Subarctic N. Pac. 2.1, 1.6, 2.5,3.0 (2.3 ± 0.6) (OSP) 50°N, 145°W E. Subtropical N. Pac. 2.7, 1.4, 3.3, 2.5, 2.3, 3.1,1.7–2.2, 2.3 (2.5 ± 0.7) (HOT) 23°N,158°W E. Equatorial. Pacific 3.2–5.2i, 1.7j, 1.2j, 4.4j, 2.5k, 2–7l (3.3 ± 1.8) 170°–95°W W. Equatorial Pacific °E–140°W Subtrop/Subarc. N. Atl. 2.8 ± 2.7n(2.8 ± 2.7) (40°N–65°N, 10°W–60°W) W. Subtropical N. Atl. 3.4, 3.9, 5.6, 3.8, 4.9, 2.1, 2.6–3.5 (3.8 ±1.2) (BATS) 32°N,64°W Coastal 3.3–17.0(6.4 ± 1.9) CalCOFI (~30°N–34°N, 118°W–125°W)

Table 3. Comparison of the Particulate Organic Carbon Flux Calculated From the Annual Net Community Production, FP ztrap, and Particulate Organic Carbon Fluxes Measured in Sediment Traps, Fp meas, at the Three Time Series Sites Location zh ztrap z* F D h / F h ANCP F Z h F P h F P trap F P meas BATS HOT OSP

Table 4. Summary of ANCP Values Determined by Oxygen and Carbon Mass Balance and by Satellite-Based Methods at Three Locations Where Annual Experimental Data Exist Location ANCP meas NPPsat NCP:NPP ANCP sat (mol C m -2 y -1 ) (mg C m -2 D -1 ) (mol C m -2 y -1 ) VGPM CbPM Laws Dunne VGPM CbPM OSP 2.3 ± ± ± 0.6 HOT 2.5 ± ± ± 0.1 BATS 3.8 ± ± ± 0.1