Why the atlantic generally cannot generate trans-oceanic tsunamis?

For the three oceans with major and concentrated population centers around the coastlines, namely, the Pacific, Atlantic and Indian Oceans, past events as well as numerical models appear to suggest that, while the Pacific and Indian Oceans can support trans-oceanic tsunamis, in general, the Atlantic Ocean cannot. There are seismological and physical oceanographic reasons for this difference in behaviour. It is not that the Atlantic Ocean does not give rise to tsunamis, but they are all generally local and do not impact the whole Atlantic Ocean. This local behaviour of tsunamis in the Atlantic Ocean needs to be taken into account in developing a tsunami warning system.

[1]  J. M. Miranda,et al.  New study of the 1755 earthquake source based on multi-channel seismic survey data and tsunami modeling , 2003 .

[2]  T. Murty Seismic sea waves: tsunamis , 1977 .

[3]  Carl B. Harbitz,et al.  The Storegga Slide tsunami—comparing field observations with numerical simulations , 2005 .

[4]  Efim Pelinovsky,et al.  Simulation of the trans-oceanic tsunami propagation due to the 1883 Krakatau volcanic eruption , 2003 .

[5]  J. Lander,et al.  Caribbean Tsunamis: A 500-Year History from 1498-1998 , 2003 .

[6]  M. Gutscher,et al.  Evidence for active subduction beneath Gibraltar , 2002 .

[7]  D. Leverington,et al.  Glacial Lake Agassiz: A 5000 yr history of change and its relationship to the δ18O record of Greenland , 2004 .

[8]  Evaluation of the Threat of Mega Tsunami Generation from Postulated Massive Slope Failures of Island , 2002 .

[9]  F. Chierici,et al.  Neogene Through Quaternary Tectonic Reactivation of SW Iberian Passive Margin , 2004 .

[10]  T. S. Murty,et al.  A numerical model for the Halifax harbor tsunami due to the 1917 explosion , 1993 .

[11]  I. V. Finea,et al.  The Grand Banks landslide-generated tsunami of November 18 , 1929 : preliminary analysis and numerical modeling , 2005 .

[12]  R. S. White Crustal structure and magmatism of North Atlantic continental margins , 1992, Journal of the Geological Society.

[13]  James T. Teller,et al.  Paleohydraulics of the last outburst flood from glacial Lake Agassiz and the 8200 BP cold event , 2004 .

[14]  C. Mader MODELING THE LA PALMA LANDSLIDE TSUNAMI , 2001 .

[15]  J. M. Miranda,et al.  CONSTRAINS ON THE SOURCE OF THE 1755 LISBON TSUNAMI INFERRED FROM NUMERICAL MODELLING OF HISTORICAL DATA ON THE SOURCE OF THE 1755 LISBON TSUNAMI , 1998 .

[16]  J. Andrews,et al.  Forcing of the cold event of 8,200 years ago by catastrophic drainage of Laurentide lakes , 1999, Nature.

[17]  Pedro M. A. Miranda,et al.  The 1755 Lisbon tsunami; evaluation of the tsunami parameters , 1998 .

[18]  S. Day,et al.  Cumbre Vieja Volcano—Potential collapse and tsunami at La Palma, Canary Islands , 2001 .

[19]  William H. Berninghausen Tsunamis and seismic seiches reported from the eastern Atlantic south of the Bay of Biscay , 1964 .

[20]  I. Foster,et al.  The Holocene Storegga Slide tsunami in the United Kingdom , 2004 .

[21]  G. Pedersen,et al.  Modeling tsunamis from earthquake sources near Gorringe Bank southwest of Portugal , 1997 .

[22]  T. Murty Tsunami Wave Height Dependence on Landslide Volume , 2003 .

[23]  James T. Teller,et al.  Freshwater outbursts to the oceans from glacial Lake Agassiz and their role in climate change during the last deglaciation , 2002 .

[24]  B. Bornhold,et al.  The Grand Banks landslide-generated tsunami of November 18, 1929: preliminary analysis and numerical modeling , 2005 .

[25]  C. Mariotti,et al.  Numerical Simulation of the 1969 Portuguese Tsunami by a Finite Element Method , 1998 .

[26]  W. F. Baird,et al.  A POSSIBLE TSUNAMI IN THE LABRADOR SEA RELATED TO THE DRAINAGE OF GLACIAL LAKE AGASSIZ ~8400 YEARS B.P. , 2005 .