000014784 001__ 14784
000014784 005__ 20161115100202.0
000014784 04107 $$aeng
000014784 046__ $$k2016-08-21
000014784 100__ $$aChristodoulides, Paul
000014784 24500 $$aOcean waves and microseisms

000014784 24630 $$n24.$$p24th International Congress of Theoretical and Applied Mechanics - Book of Papers
000014784 260__ $$bInternational Union of Theoretical and Applied Mechanics, 2016
000014784 506__ $$arestricted
000014784 520__ $$2eng$$aOcean gravity waves generate pressure variations on the sea floor, which may lead to microseisms. Secondary microseisms are due to the interaction of surface waves with nearly equal frequencies but nearly opposite directions. A theoretical analysis with goal to quantify the degree of nearness that must be reached for the occurrence of such phenomena is presented. Based on a weakly nonlinear analysis expressions are obtained for the free surface elevation and pressure of interacting waves. Results are discussed for various regimes.

000014784 540__ $$aText je chráněný podle autorského zákona č. 121/2000 Sb.
000014784 653__ $$a

000014784 7112_ $$a24th International Congress of Theoretical and Applied Mechanics$$cMontreal (CA)$$d2016-08-21 / 2016-08-26$$gICTAM2016
000014784 720__ $$aChristodoulides, Paul
000014784 8560_ $$ffischerc@itam.cas.cz
000014784 8564_ $$s166192$$uhttps://invenio.itam.cas.cz/record/14784/files/TS.FM16-2.02.pdf$$yOriginal version of the author's contribution as presented on CD,  page 1596, code TS.FM16-2.02
.
000014784 962__ $$r13812
000014784 980__ $$aPAPER