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Thin chlorophyll layer concomitant of the thermohaline intrusion in the confluence of the Gulf Stream and Labrador Current (a case study)

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Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
Based on the depth-cycling data of a fluorometer probe in the northwestern Atlantic ocean, this paper considers features of the chlorophyll fluorescence layer against a background of concurrent variability of seawater temperature and fluorescence of CDOM (Colored Dissolved Organic Matter). The vertical distributions of chlorophyll fluorescence complied with the criteria of a thin chlorophyll layer at the site where changes of temperature and CDOM fluorescence were indicative of the intrusion of Labrador waters into adjacent warmer waters below the upper mixed layer. As may be supposed, the thin chlorophyll layer was due to the gyrotactic trapping of phytoplankton cells induced by water shear between the upper mixed layer and the intrusion.
Czasopismo
Rocznik
Strony
527--533
Opis fizyczny
Bibliogr. 18 poz., rys., wykr.
Twórcy
  • Laboratory of Ocean Optics, Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow, Russia
Bibliografia
  • [1] Bhatta, P., Fiorelli, E., Lekien, F., Leonard, N. E., Paley, D. A., Zhang, F., Bachmayer, R., Davis, E., Fratantoni, D. M., Sepulchre, R., 2005. Coordination of underwater glider fleet for adaptive sampling. In: Proc. Internat. Workshop on Underwater Robotics, Genoa, Italy, 61-69.
  • [2] Churnside, J. H., Donaghay, P. L., 2009. Thin scattering layers observed by airborne lidar. ICES J. Mar. Sci. 66 (4), 778-789, http://dx.doi.org/10.1093/icesims/fspQ29.
  • [3] Cox, J. L., Wiebe, P. H., Ortner, P., Boyd, S., 1982. Seasonal development of subsurface chlorophyll maxima in slope water and the Northern Sargasso Sea of the Northwestern Atlantic Ocean. Biol. Oceanogr. 1 (3), 271-285, http://dx.doi.org/10.1080/01965581.1982.10749444.
  • [4] Dekshenieks, M. M., Donaghay, P. L., Sullivan, J. M., Rines, J. E. B., Osborn, T. R., Twardowski, M. S., 2001. Temporal and spatial occurrence of thin phytoplankton layers in relation to physical processes. Mar. Ecol. Prog. Ser. 223, 61-71.
  • [5] Durham, W. M., Kessler, J. O., Stocker, R., 2009. Disruption of vertical motility by shear triggers formation of thin phytoplankton layers. Science 323, 1067-1070, http://dx.doi.org/10.1126/science.1167334.
  • [6] Durham, W. M., Stocker, R., 2012. Thin phytoplankton layers: characteristics, mechanisms, and consequences. Annu. Rev. Mar. Sci. 4, 177-207, http://dx.doi.org/10.1146/annurev-marine-120710-100957.
  • [7] Fratantoni, D. M., 2001. North Atlantic surface circulation during the 1990s observed with satellite-tracked drifters. J. Geophys. Res. Oceans 106 (C10), 22067-22093, http://dx.doi.org/10.1029/2000JC000730.
  • [8] Jerlov, N. G., 1976. Marine Optics. Elsevier, Amsterdam, 233 pp.
  • [9] Kalle, K., 1963. Über das Verhalten und die Herkunft der in den Gewässern und in der Atmosphäre vorhandenen himmelblauen Fluoreszenz. Deutsche Hydrogr. Zt. 16, 153-166.
  • [10] Karabashev, G. S., 1987. Fluorescence in the ocean. Gidrometeoizdat, Leningrad, 200 pp. (in Russian), http://dx.doi.org/10.13140/2.1.3439.7128.
  • [11] Karabashev, G. S., Khanaev, S. A., 1988. Underwater multichannel fluorimeter for marine ecological research. J. Appl. Spectrosc. 49 (3), 979-981, http://dx.doi.org/10.1007/BF00662796.
  • [12] Karabashev, G. S., Solov'yov, A. N., 1973. Photoluminescence of sea-water, an indicator of dynamic processes in the ocean. Oceanology (USSR) 13, 490-493, (in Russian).
  • [13] Nelson, N. B., Siegel, D. A., Carlson, C. A., Swan, C. M., 2010. Tracing global biogeochemical cycles and meridional overturning circulation using chromophoric dissolved organic matter. Geophys. Res. Lett. 37 (3), L03610, 1-5, http://dx.doi.org/10.1029/2009GL042325.
  • [14] Pickart, R. S., McKee, T. K., Torres, D. J., Harrington, S. A., 1999. Mean structure and interannual variability of the Slope water system south of Newfoundland. J. Phys. Oceanogr. 29, 2541-2558, http://dx.doi.org/10.1175/1520-0485(1999)029<2541:MSAIVO>2.0.CO;2.
  • [15] Rudnick, D. L., Davis, R. E., Eriksen, C. C., Fratantoni, D. M., Perry, M. J., 2004. Underwater gliders for ocean research. Mar. Technol. Soc. J. 38 (1), 48-59, http://dx.doi.org/10.4031/002533204787522703.
  • [16] Schmitt, R. W., 1994. Double-diffusion in oceanography. Annu. Rev. Fluid Mech. 26, 255-285, http://dx.doi.org/10.1146/annurev.fl.26.010194.001351.
  • [17] Sullivan, J. M., Donaghay, P. L., Rines, J. E. B., 2010. Coastal thin layer dynamics: consequences to biology and optics. Cont. Shelf Res. 30 (1), 50-65, http://dx.doi.org/10.1016/j.csr.2009.07.009.
  • [18] Vasilkov, A. P., Goldin, Y. A., Gureev, B. A., Hoge, F. E., Swift, R. N., Wright, C. W., 2001. Airborne polarized lidar detection of scattering layers in the ocean. Appl. Optics 40 (24), 4353-4364, http://dx.doi.org/10.1364/AO.40.004353.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-8369360e-1f9a-4fa6-a7a8-5647fdfac7ee
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