PL EN


Preferencje help
Widoczny [Schowaj] Abstrakt
Liczba wyników
Powiadomienia systemowe
  • Sesja wygasła!
Tytuł artykułu

The impact of tides and waves on near-surface suspended sediment concentrations in the English Channel

Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
Numerous ecological problems of continental shelf ecosystems require a refined knowledge of the evolution of suspended sediment concentrations (SSC). The present investigation focuses on the spatial and temporal variabilities of near-surface SSC in coastal waters of the English Channel (western Europe) by exploiting numerical predictions from the Regional Ocean Modeling System ROMS. Extending previous investigations of ROMS performances in the Channel, this analysis refines, with increased spatial and temporal resolutions, the characterization of near-surface SSC patterns revealing areas where concentrations are highly correlated with evolutions of tides and waves. Significant tidal modulations of near-surface concentrations are thus found in the eastern English Channel and the French Dover Strait while a pronounced influence of waves is exhibited in the Channel Islands Gulf. Coastal waters present furthermore strong SSC temporal variations, particularly noticeable during storm events of autumn and winter, with maximum near-surface concentrations exceeding 40 mg l−1 and increase by a factor from 10 to 18 in comparison with time-averaged concentrations. This temporal variability strongly depends on the granulometric distribution of suspended sediments characterized by local bimodal contributions of silts and sands off coastal irregularities of the Isle of Wight, the Cotentin Peninsula and the southern Dover Strait.
Czasopismo
Rocznik
Strony
28--36
Opis fizyczny
Bibliogr. 38 poz., mapy, wykr.
Twórcy
autor
  • Laboratoire de Génie Côtier et Environnement (LGCE), Cerema/DTecEMF/DS, Plouzané, France
autor
  • Laboratoire de Génie Côtier et Environnement (LGCE), Cerema/DTecEMF/DS, Plouzané, France
  • ODE-DYNECO-PELAGOS, Ifremer, Centre de Bretagne, Technople Brest-Iroise, Plouzané, France
autor
  • Laboratoire de Génie Côtier et Environnement (LGCE), Cerema/DTecEMF/DS, Plouzané, France
autor
  • ODE-DYNECO-PELAGOS, Ifremer, Centre de Bretagne, Technople Brest-Iroise, Plouzané, France
Bibliografia
  • [1] Ardhuin, F., Hanafin, J., Quilfen, Y., Chapron, B., Queffeulou, P., Obrebski, M., 2011. Calibration of the IOWAGA global wave hindcast (1991—2011) using ECMWF and CFSR winds. In: 12th Int. Workshop on Wave Hindcasting and Forecasting, Kohala Coast, Hawaii.
  • [2] Bénard, P., 2004. ALADIN-NH/AROME dynamical core; status and possible extension to IFS. In: Proc. ECMWF Seminar on Recent Developments in Numerical Methods for Atmosphere and Ocean Modelling, Reading, UK, 27—40.
  • [3] Bowers, D. G., Binding, C. E., 2006. The optical properties of mineral suspended particles: a review and synthesis. Estuar. Coast. Shelf Sci. 67 (1—2), 219—230, http://dx.doi.org/10.1016/j.ecss.2005.11.010.
  • [4] Bowers, D. G., Braithwaite, K. M., 2012. Evidence that satellite sense the cross-sectional area of suspended particles in shelf seas and estuaries better than their mass. Geo-Mar. Lett. 32 (2), 165—171, http://dx.doi.org/10.1007/s00367-011-0259-6.
  • [5] Dupont, J. P., Collins, M. B., Lafite, R., Nash, L., Huault, M. F., Shimwell, S. J., Chaddock, S., Brunet, C., Wartel, M., Lamboy, M., 1993. Annual variations in suspended particulate matter within the Dover Strait. Oceanol. Acta 16 (5—6), 507—516.
  • [6] Egbert, G., Erofeeva, S., 2002. Efficient inverse modeling of barotropic ocean tides. J. Atmos. Ocean. Technol. 19 (2), 183—204, http://dx.doi.org/10.1175/1520-0426(2002)019%3C0183: EIMOBO%3E2.0.CO;2.
  • [7] Eisma, D., Kalf, J., 1979. Distribution and particle size of suspended matter in the Southern North Sea. Neth. J. Sea Res. 13 (2), 298—324, http://dx.doi.org/10.1016/0077-7579(79)90008-5.
  • [8] Fettweis, M., Monbaliu, J., Baeye, M., Nechad, B., Van den Eynde, D., 2012. Weather and climate induced variability of surface suspended particulate matter concentration in the North Sea and the English Channel. Methods Oceanogr. 3—4, 25—39, http://dx.doi.org/10.1016/j.mio.2012.11.001.
  • [9] Fettweis, M., Nechad, B., Van den Eynde, D., 2007. An estimate of the suspended particulate matter (SPM) transport in the southern North Sea using Sea WiFS images, in situ measurements and numerical model results. Cont. Shelf Res. 27 (10—11), 1568—1583, http://dx.doi.org/10.1016/j.csr.2007.01.017.
  • [10] Gerritsen, H., Vos, R., der Kaaij, T. V., Lane, A., Boon, J., 2000. Suspended sediment modelling in a shelf sea (North Sea). Coast. Eng. 41 (1—3), 317—352, http://dx.doi.org/10.1016/S0378-3839(00)00042-9.
  • [11] Gohin, F., 2011. Annual cycles of chlorophyll-a, non-algal suspended particulate matter and turbidity observed from space and in-situ in coastal waters. Ocean Sci. 7 (5), 705—732, http://dx.doi.org/10.5194/os-7-705-2011.
  • [12] Gohin, F., Loyer, S., Lunven, M., Labry, C., Froidefond, J. M., Delmas, D., Huret, M., Herbland, A., 2005. Satellite-derived parameters for biological modelling in coastal waters: illustration over the eastern continental shelf of the Bay of Biscay. Remote Sens. Environ. 95 (1), 29—46, http://dx.doi.org/10.1016/j.rse.2004.11.007.
  • [13] Grochowski, N. T. L., Collins, M. B., 1994. Wave activity on the sea-bed of the English Channel. J. Mar. Biol. Assoc. U. K. 74 (3), 739—742, http://dx.doi.org/10.1017/S0025315400047792.
  • [14] Grochowski, N. T. L., Collins, M. B., Boxall, S. R., Salomon, J. C., 1993. Sediment transport predictions for the English Channel, using numerical models. J. Geol. Soc. (London, U.K.) 150 (3), 683—695, http://dx.doi.org/10.1144/gsjgs.150.4.0683.
  • [15] Guillou, N., Chapalain, G., 2011. Modelling impact of northerly wind generated waves on sediments resuspensions in the Dover Strait and adjacent waters. Cont. Shelf Res. 31 (18), 1894—1903, http://dx.doi.org/10.1016/j.csr.2011.08.011.
  • [16] Guillou, N., Chapalain, G., Thais, L., 2009. Three-dimensional modeling of tide-induced suspended transport of seabed multicomponent sediments in the eastern English Channel. J. Geophys. Res. 114, C07025, http://dx.doi.org/10.1029/2008JC004791.
  • [17] Guillou, N., Rivier, A., Gohin, F., Chapalain, G., 2015. Modeling nearsurface suspended sediment concentration in the English Channel. J. Mar. Sci. Eng. 3 (2), 193—215, http://dx.doi.org/10.3390/jmse3020193.
  • [18] Haarich, M., Kienz, W., Krause, M., Schmidt, G. P. Z. D., 1993. Heavy metal distribution in different compartments of the northern North Sea and adjacent areas. Ocean Dyn. 45 (5), 313—336, http://dx.doi.org/10.1007/BF02225884.
  • [19] Haidvogel, D. B., Arango, H. G., Hedstrom, K., Beckman, A., Malanotte-Rizzoli, P., Shchepetkin, A. F., 2000. Model evaluation experiments in the North Atlantic Basin: simulations in nonlinear terrain-following coordinates. Dyn. Atmos. Oceans 32 (3—4), 239—281, http://dx.doi.org/10.1016/S0377-0265(00)00049-X.
  • [20] Hoppe, H. G., 1984. Attachment of bacteria: advantage or disadvantage for survival in the aquatic environment. In: Marshall, K. C. (Ed.), Microbial Adhesion and Aggregation, Life Sci. Res. Rep. n ̊ 131. Springer-Verlag, New York, 283—303, http://dx.doi.org/10.1007/978-3-642-70137-5_19.
  • [21] Jago, C. F., Bale, A. J., Green, M. O., Howarth, M. J., Jones, S. E., McCave, I. N., Millward, G. E., Morris, A. W., Rowden, A. A., Williams, J. J., Hydes, D., Turner, A., Huntley, D., Van Leussen, W., 1993. Resuspension processes and Seston dynamics, southern North Sea. Philos. Trans. R. Soc. Lond. A 343 (1669), 475—491, http://dx.doi.org/10.1098/rsta.1993.0060.
  • [22] Lafite, R., Shimwell, S., Grochowski, N., Dupont, J. P., Nash, L., Salomon, J. C., Cabioch, L., Collins, M., Gao, S., 2000. Suspended particulate matter fluxes through the Straits of Dover, English Channel: observations and modelling. Oceanol. Acta 23 (6), 687—699, http://dx.doi.org/10.1016/S0399-1784(00)00144-4.
  • [23] Leprêtre, A., Chapalain, G., Carpentier, P., 2006. A spatial interpolation method of granulometric properties of superficial sediments. Bull. Soc. Geol. Fr. 177 (2), 89—95, http://dx.doi.org/10.2113/gssgfbull.177.2.89.
  • [24] Lubac, B., Loisel, H., 2007. Variability and classification of remote sensing reflectance spectra in the eastern English Channel and southern North Sea. Remote Sens. Environ. 110 (1), 45—58, http://dx.doi.org/10.1016/j.rse.2007.02.012.
  • [25] Mc Cave, I. N., 1973. Mud in the North Sea science. In: Goldberg, E. D. (Ed.), North Sea Science. M.I.T. Press, 75—100.
  • [26] Menesguen, A., Gohin, F., 2006. Observation and modelling of natural retention structures in the English Channel. J. Mar. Syst. 63 (3—4), 244—256, http://dx.doi.org/10.1016/j.jmarsys.2006.05.004.
  • [27] Owen, M., Thorn, M., 1978. Effect of waves on sand transport by currents. In: Proc. 16th Conf. Coastal Eng. Hamburg, 1675—1687, doi:10.9753/icce.v16.%25p.
  • [28] Rahbani, M., 2015. A comparison between the suspended sediment concentrations derived from DELFT3D model and collected using transmissometer — a case study in tidally dominated area of Dithmarschen Bight. Oceanologia 57 (1), 44—49, http://dx.doi.org/10.1016/j.oceano.2014.06.002.
  • [29] Rivier, A., Gohin, F., Bryère, P., Petus, C., Guillou, N., Chapalain, G., 2012. Observed vs. predicted variability in non-algal suspended particulate matter concentration in the English Channel in relation to tides and waves. Geo-Mar. Lett. 32 (2), 139—151, http://dx.doi.org/10.1007/s00367-011-0271-x.
  • [30] Soulsby, R. L., Hamm, L., Klopman, G., Myrhaug, D., Simons, R. R., Thomas, G. P., 1993. Wave—current interaction within and outside the bottom boundary layer. Coast. Eng. 21 (1—3), 41—69, http://dx.doi.org/10.1016/0378-3839(93)90045-A.
  • [31] Souza, A. J., Holt, J. T., Proctor, R., 2007. Modelling SPM on the NW European shelf seas. In: Balson, P, Collins, M. (Eds.), Coastal and Shelf Sediment Transport. Geol. Soc., London, 147—158, http://dx.doi.org/10.1144/GSL.SP.2007.274.01.14.
  • [32] Sykes, P. A., Barcelia, R. M., 2012. Assessment and development of a sediment model within an operational system. J. Geophys. Res. 117, C04036, http://dx.doi.org/10.1029/2011jc007420.
  • [33] Van Alphen, J., 1990. A mud balance for Belgian-Dutch coastal waters between 1969 and 1986. Neth. J. Sea Res. 25 (1—2), 19—30, http://dx.doi.org/10.1016/0077-7579(90)90005-2.
  • [34] Van der Molen, J., Bolding, K., Greenwoord, N., Mills, D. K., 2009. A 1-D vertical multiple grain size model of suspended particulate matter in combined currents and waves in shelf seas. J. Geophys. Res. 114, F01030, http://dx.doi.org/10.1029/2008jf001150.
  • [35] Velegrakis, A. F., Gao, S., Lafite, R., Dupont, J. P., Huault, M. F., Nash, L. A., Collins, M. B., 1997. Resuspension and advection processes affecting suspended particulate matter concentrations in the central English Channel. J. Sea Res. 38 (1—2), 17—34, http://dx.doi.org/10.1016/S1385-1101(97)00041-5.
  • [36] Velegrakis, A. F., Michel, D., Collins, M. B., Lafite, R., Oikonomou, E. K., Dupont, J. P., Huault, M. F., Lecouturier, M., Salomon, J. C., Bishop, C., 1999. Sources, sinks and resuspension of suspended particulate matter in the eastern English Channel. Cont. Shelf Res. 19 (15—16), 1933—1957, http://dx.doi.org/10.1016/S0278-4343(99)00047-3.
  • [37] Warner, J. C., Sherwood, C. R., Signell, R. P., Harris, C. K., Arango, H. G., 2008. Development of a three-dimensional, regional, coupled wave, current, and sediment-transport model. Comput. Geosci. 34 (10), 1284—1306, http://dx.doi.org/10.1016/j.cageo.2008.02.012.
  • [38] Wozniak, S. B., 2014. Simple statistical formulas for estimating biogeochemical properties of suspended particulate matter in the southern Baltic Sea potentially useful for optical remote sensing applications. Oceanologia 56 (1), 7—39, http://dx.doi.org/10.5697/oc.56-1.007.
Uwagi
Opracowanie ze środków MNiSW w ramach umowy 812/P-DUN/2016 na działalność upowszechniającą naukę (zadania 2017).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-1e833e2c-d346-4f36-95d8-9969c9ec7e58
JavaScript jest wyłączony w Twojej przeglądarce internetowej. Włącz go, a następnie odśwież stronę, aby móc w pełni z niej korzystać.