Evolution of bed shear stress distribution over the northwest European shelf seas during the last 12,000 years
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Simon P. Neill | Katsuto Uehara | S. Neill | J. Scourse | K. Uehara | James D. Scourse | Katsuto Uehara
[1] S. Neill,et al. Changes in wave climate over the northwest European shelf seas during the last 12,000 years , 2009 .
[2] G. Boulton,et al. Glacial geology and glaciology of the last mid-latitude ice sheets , 1985, Journal of the Geological Society.
[3] J. Holt,et al. An s coordinate density evolving model of the northwest European continental shelf: 1. Model description and density structure , 2001 .
[4] L. St. Laurent,et al. Parameterizing tidal dissipation over rough topography , 2001 .
[5] D.J.T. Carter,et al. Prediction of wave height and period for a constant wind velocity using the JONSWAP results , 1982 .
[6] K. Lambeck,et al. Late Devensian and Holocene records of relative sea-level changes in northwest Scotland and their implications for glacio-hydro-isostatic modelling , 2000 .
[7] R. Soulsby. Dynamics of marine sands , 1997 .
[8] G. Mellor,et al. A Hierarchy of Turbulence Closure Models for Planetary Boundary Layers. , 1974 .
[9] O. Francis,et al. Modelling the global ocean tides: modern insights from FES2004 , 2006 .
[10] Alan M. Davies,et al. Tidal energy fluxes and dissipation on the European continental shelf , 2000 .
[11] K. Lambeck. Late Devensian and Holocene shorelines of the British Isles and North Sea from models of glacio-hydro-isostatic rebound , 1995, Journal of the Geological Society.
[12] A. H. Stride. Offshore Tidal Sands: Processes and deposits , 1982 .
[13] C. Guedes Soares,et al. 44-year wave hindcast for the North East Atlantic European coast , 2008 .
[14] A. M. Davies,et al. A three dimensional model of the M2, S2, N2, K1 and O1 tides in the Celtic and Irish seas , 1992 .
[15] O. Marchal,et al. Size sorting in marine muds: Processes, pitfalls, and prospects for paleoflow‐speed proxies , 2006 .
[16] A. Wheeler,et al. Post-glacial sediment dynamics in the Irish Sea and sediment wave morphology: data-model comparisons. , 2009 .
[17] J. Molen. The influence of tides, wind and waves on the net sand transport in the North Sea , 2002 .
[18] Gary D. Egbert,et al. Numerical modeling of the global semidiurnal tide in the present day and in the last glacial maximum , 2004 .
[19] R. Sternberg,et al. Sediment-transport events on the northern California continental shelf , 1999 .
[20] R. Holmes,et al. The Last Glacial Maximum in the North Sea Basin: micromorphological evidence of extensive glaciation , 2006 .
[21] R. Devoy,et al. Sea-level research : a manual for the collection and evaluation of data , 1988 .
[22] O. V. D. Plassche. Sea-Level Research , 1986 .
[23] I. N. McCave,et al. Hydrography and sedimentation under the deep western boundary current on Björn and Gardar Drifts, Iceland Basin , 2000 .
[24] I. N. McCave,et al. Sedimentation on the Feni Drift and late Glacial bottom water production in the northern Rockall Trough , 1993 .
[25] R. Pingree,et al. Sand transport paths around the British Isles resulting from M 2 and M 4 tidal interactions , 1979 .
[26] H. Gerritsen,et al. A modelling study of tidally induced equilibrium sand balances in the North Sea during the Holocene , 1998 .
[27] S. Neill,et al. A model of inter-annual variability in beach levels , 2008 .
[28] R. M. Austin. Modelling Holocene tides on the NW European continental shelf , 1991 .
[29] A. H. Stride. Tidal currents of the continental shelf , 1982 .
[30] K. Lambeck,et al. Sea Level Change Through the Last Glacial Cycle , 2001, Science.
[31] A. M. Davies,et al. A three-dimensional model of the principal tides on the European shelf , 1997 .
[32] K. Lambeck,et al. Water-load definition in the glacio-hydro-isostatic sea-level equation , 2003 .
[33] I. Shennan,et al. Relative sea‐level observations in western Scotland since the Last Glacial Maximum for testing models of glacial isostatic land movements and ice‐sheet reconstructions , 2006 .
[34] J. Scourse,et al. Celtic Sea linear tidal sand ridges, the Irish Sea Ice Stream and the Fleuve Manche: Palaeotidal modelling of a transitional passive margin depositional system , 2009 .
[35] D. Myrhaug,et al. Wave-current interaction within and outside the bottom boundary layer , 1993 .
[36] A. M. Davies,et al. Modelling tidally induced sediment-transport paths over the northwest European shelf: the influence of sea-level reduction , 2004 .
[37] N. Booij,et al. A third-generation wave model for coastal regions-1 , 1999 .
[38] D. Huntley,et al. The origin, classification and modelling of sand banks and ridges , 1999 .
[39] W. Peltier. GLOBAL GLACIAL ISOSTASY AND THE SURFACE OF THE ICE-AGE EARTH: The ICE-5G (VM2) Model and GRACE , 2004 .
[40] R. Harland,et al. Glacial and postglacial sedimentation in the Sea of the Hebrides , 1974, Nature.
[41] A. M. Davies,et al. Application of a three‐dimensional turbulence energy model to the determination of tidal currents on the northwest European Shelf , 1990 .
[42] A. Rosati,et al. A Quasi-equilibrium Turbulent Energy Model for Geophysical Flows , 1988 .
[43] M. Stoker,et al. The history of Quaternary sedimentation in the UK sector of the North Sea Basin , 1987, Journal of the Geological Society.
[44] J. Molen,et al. Holocene tidal conditions and tide-induced sand transport in the southern North Sea , 2001 .
[45] K. Lambeck,et al. Sea‐level change in the Irish Sea since the Last Glacial Maximum: constraints from isostatic modelling , 2001 .
[46] H. Renssen,et al. Weichselian Late Pleniglacial surface winds over northwest and central Europe: a model–data comparison , 2007 .
[47] Benjamin P. Horton,et al. Modelling western North Sea palaeogeographies and tidal changes during the Holocene , 2000, Geological Society, London, Special Publications.
[48] J. Molen,et al. Modelling the morphodynamics of a tidal shelf sea , 2004 .
[49] G. Bigg,et al. Tidal mixing and the Meridional Overturning Circulation from the Last Glacial Maximum , 2009 .
[50] W. Peltier,et al. Ice Age Paleotopography , 1994, Science.
[51] Fei Liu,et al. Model Description and Validation , 2006 .
[52] R. Coleman,et al. Classification of the Australian continental shelf based on predicted sediment threshold exceedance from tidal currents and swell waves , 2004 .
[53] J. Scourse,et al. Impact of sea‐level rise over the last deglacial transition on the strength of the continental shelf CO2 pump , 2008 .
[54] B. Gong,et al. Modeling the contribution of M2 tidal amplification to the Holocene rise of mean high water in the Gulf of Maine and the Bay of Fundy , 1995 .
[55] Anthony W. Purcell,et al. Tidal evolution of the northwest European shelf seas from the Last Glacial Maximum to the present , 2006 .
[56] Jason T. Holt,et al. An s coordinate density evolving model of the northwest European continental shelf: 2. Seasonal currents and tides , 2001 .
[57] A. M. Davies. A three-dimensional model of the Northwest European Continental shelf, with application to the M4 tide , 1986 .
[58] W. Peltier,et al. Global to local scale parameters determining relative sea-level changes and the post-glacial isostatic adjustment of Great Britain , 2002 .
[59] I. Shennan,et al. Relative sea‐level changes, glacial isostatic modelling and ice‐sheet reconstructions from the British Isles since the Last Glacial Maximum , 2006 .
[60] J. Molen,et al. Holocene wave conditions and wave-induced sand transport in the southern North Sea , 2001 .