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Full text : Tsunami - a study regarding the North Sea coast (BSH-Berichte, Nr. 41)

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Long,  D.,  Smith,  D.  E.,  Dawson,  A.  G.:  A  Holocene  tsunami  deposit  in  eastern  Scotland.
Journal  of  Quaternary  Sciences,  4  (1989)  61-66
Mader,  Ch.  L.:  Numerical  Modeling  of  Water  Waves.  CRC  Press,  Boca  Raton  (2004,  2.  Aufl.)
274  p.
Madsen,  P.  A.,  Murray,  R.,  Sorensen,  O.  R.:  A  new  form  of  the  Boussinesq  equations  with
improved  linear  dispersion  characteristics.  Coastal  Engineering  15  (1991)  371-388
Madsen,  P.  A.,  Sorensen,  O.  R.:  A  new  form  of  the  Boussinesq  equations  with  improved
linear  dispersion  characteristics.  Part  2.  A  slowly-varying  bathymetry.  Coastal  Engineering  18
(1992)  183-204
Maramai,  A.,  Graziani,  L.,  Tinti,  S.:  Updating  and  revision  of  the  European  tsunami
catalogue.  In:  Yalçiner,  A.  C.  et  al.  (Ed.):  Submarine  Landslides  and  Tsunamis.  Klüver
Academic  Publishers,  Dordrecht  (2003),  Nato  Science  Series,  Serie  IV,  21,25-32
Marshall,  J.,  Hill,  C.,  Perelman,  L.,  Adcroft,  A.:  Hydrostatic,  quasi-hydrostatic,  and
nonhydrostatic  ocean.  Journal  of  Geophysical  Research  102,  C3  (1997)  5733-5752
Marshall,  J.,  Adcroft,  A.,  Hill,  C.,  Perelman,  L.,  Heisey,  C.:  A  finite-volume,  incompressible
Navier  Stokes  model  for  studies  of  the  ocean  on  parallel  computers.  Journal  of  Geophysical
Research  102,  C3  (1997)  5753-5766
Masselink,  G.:  Waves.  In:  Schwartz,  M.L.  (Ed.):  Encyclopedia  of  Coastal  Science,  Springer
Verlag,  Dordrecht  (2005)  1069-1074
McCowan,  J.:  On  the  solitary  wave.  Phil.  Magazine,  series  5,  32  (1891)  45-58
McNeil,  C.:  Tsunamis.  Encylopedia  of  Ocean  Sciences  7  (2001)  3056-3051
Miche,  R.:  Undulatory  movements  of  the  sea  in  constant  and  decreasing  depth.  Ann.  de
Ponts  et  Chaussées,  May-June,  July-August  (1944)  25-78,  131-164.270-292,  369-406
Milbradt,  P.:  A  stabilized  finite  element  method  for  systems  of  instationary  advectiondominated
  equations  in  multi-dimensional  domains.  Proceedings  of  5th  World  Congress  on
Computational  Mechanics,  WCCM  V,  Vienna,  Austria  2002,  Ed.  Mang,  Rammerstorfer,
Eberhardsteiner.  (Model  available  under  10.4:  MAR06)
Mirchina,  N.,  Pelinovsky,  E.:  Dispersive  intensification  of  tsunami  waves.  IST  Proceedings  7,
7-10  (2001)  789-794
Mofjeld,  H.  O.,  Titov,  F.  I.,  González  F.  I.,  Newman  J.  C.:  Analytic  Theory  of  Tsunami  Wave
Scattering  in  the  Open  Ocean  with  Application  to  the  North  Pacific.  NOAA  Technical
Memorandum  OAR  PMEL-166  (2000)  37  p.
Müller-Navarra,  S.  H.:  Implementation  of  the  equilibrium  tide  in  a  shelf  sea  model.
Environmental  and  Chemical  Physics  24  (2002)  127-132
Müller-Navarra,  S.  H.,  Lange,  W.,  Dick,  S.  Soetje,  K.  C.:  Über  Verfahren  der  Wasserstandsund ­
  Sturmflutvorhersage:  Hydrodynamisch-numerische  Modelle  der  Nord-  und  Ostsee  und
ein  empirisch-statistisches  Verfahren  für  die  Deutsche  Bucht,  promet  29,  1-4  (2003)  117-124
Munk,  W.  H.:  The  Solitary  Wave  Theory  and  its  Application  to  Surf  Problems.  Annals  of  the
New  York  Academy  of  Sciences  51  (1949)  376-424
Munk,  W.  H.:  Long  Ocean  Waves.  In:  The  Sea:  Ideas  and  Observations  in  Progress  in  Study
of  the  Sea,  Interscience,  New  York  (1962)  647-663
Nirupama,  N.,  Nistor,  I.,  Ponnambalam,  K.,  Murty,  T.  S.:  Tsunami  Travel  Time  Atlas  for  the
Atlantic  Ocean.  Marine  Geodesy  29,  3  (2006)  179-199
Okada,  Y.:  Surface  deformation  due  to  shear  and  tensile  faults  in  a  half-space.  Bulletin  of  the
Seismological  Society  of  America  75  (1985)  1135-1154
            
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