Potential of Argo Drifters for Estimating Biological Production within the Water Column

  • Published : 2006.06.30

Abstract

Argo drifters provide information of the vertical structure in the water column and have a potential for the improvement of understanding phytoplankton primary production and biogeochemical cycles in combination with ocean color satellite data, which can obtain the horizontal distribution of phytoplankton biomass in the surface layer. Our examples show that using Argo drifters with satellite-measured horizontal distribution of phytoplankton biomass at the sea surface allow an improved understanding of the development of the spring bloom. The other possible uses of Argo drifter are discussed.

Keywords

References

  1. Ali, M.M. and R. Sharma. 1994. Estimation of mixed layer depth in the equatorial Indian Ocean using GEOSAT altimeter data. Mar. Geod., 17(1), 63-72 https://doi.org/10.1080/15210609409379710
  2. Behrenfeld, M. and P. Falkowski. 1997. Photosynthetic rates derived from satellite-based chlorophyll concentration. Limnol. Oceanogr., 42(1), 1-20 https://doi.org/10.4319/lo.1997.42.1.0001
  3. Behrenfeld, M. and E. Boss. 2003. The beam attenuation to chlorophyll ratio: An optical index of phytoplankton physiology in the surface ocean? Deep-Sea Res. I, 50, 1537-1549 https://doi.org/10.1016/j.dsr.2003.09.002
  4. Claustre, H., A. Morel, M. Babin, C. Cailliau, D. Marie, J.-C. Marty, D. Tailliez, and D. Vaulot. 1999. Variability in particle attenuation and chlorophyll fluorescence in the tropical Pacific: Scales, patterns, and biogeochemical implications. J. Geophys. Res., 104, 3401-3422 https://doi.org/10.1029/98JC01334
  5. Loisel, H. and A. Morel. 1998. Light scattering and chlorophyll concentration in case 1 waters: A reexamination. Limnol. Oceanogr., 43, 847-858 https://doi.org/10.4319/lo.1998.43.5.0847
  6. Longhurst, A., S. Sathyendranath, T. Platt, and C. Caverhill. 1995. An estimate of global primary production in the ocean from satellite radiometer data. J. Plank. Res., 17(6), 1245-1271 https://doi.org/10.1093/plankt/17.6.1245
  7. Morel, A. and J.-F. Berthon. 1989. Surface pigments, algal biomass profiles, and potential production of the euphotic layer: Relationships reinvestigated in view of remote-sensing applications. Limnol. Oceanogr., 34(8), 1545-1562 https://doi.org/10.4319/lo.1989.34.8.1545
  8. Muller, J.L. and R.E. Lange. 1989. Bio-optical provinces of the Northeast Pacific Ocean: A provisional analysis. Limnol. Oceanogr., 34(8), 1572-1586 https://doi.org/10.4319/lo.1989.34.8.1572
  9. Platt, T., S. Sathyendranath, C. Caverhill, and M. Lewis. 1988. Ocean primary production and available light: Further algorithms for remote sensing. Deep-Sea Res., 35(6), 855-879 https://doi.org/10.1016/0198-0149(88)90064-7
  10. Platt, T., C. Caverhill, and S. Sathyendranath. 1991. Basin-scale estimates of oceanic primary production by remote sensing: The North Atlantic. J. Geophys. Res., 96(8), 15147-15159 https://doi.org/10.1029/91JC01118
  11. Sathyendranath, S., T. Platt, E.P.W. Horne, W.G. Harrison, O. Ulloa, R. Outerbridge, and N. Hoepffner. 1991. Estimation of new production in the ocean by compound remote sensing. Nature, 353, 129-133 https://doi.org/10.1038/353129a0
  12. Siswanto, E., J. Ishizaka, and K. Yokouchi. 2004. Estimating chlorophyll vertical profiles from satellite data and the implication to primary production in Kuroshio front of the East China Sea. J. Oceanogr., 61, 575-589 https://doi.org/10.1007/s10872-005-0066-7
  13. Son, S., J. Campbell, M. Dowell, S. Yoo, and J. Noh. 2005. Primary production determined by ocean color remote sensing in the Yellow Sea. Mar. Ecology Prog. Ser., 303, 91-103 https://doi.org/10.3354/meps303091
  14. Sverdrup, H.U. 1953. On conditions for the vernal blooming of phytoplankton. J. Cons. Int. Explor. Mer., 18, 287-295 https://doi.org/10.1093/icesjms/18.3.287
  15. Yan, X.-H., J.R. Schubel, and D.W. Pritchard. 1990. Oceanic upper mixed layer depth determination by the use of satellite data. Remote Sens. Environ., 32(1), 55-74 https://doi.org/10.1016/0034-4257(90)90098-7