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These surfaces represent strata of rapidly changing water density with increasing depth, and the associated waves are called internal waves. /S /URI << !Nf;(h7QkE#EF['[TLZ&RUmC4dg:4YQZ6]bN2(GfZE>VYtrR`SMcO;nk,9^DYU*j&A!F`2i+?V_S5 /A 104 0 R /Contents 59 0 R ]B4(6l"f$YlE5&[ht3bGqu0ms,&YT=%+AJ1SRoei$P&%ub_ndE"H"X^jfI,SV)/[7 0000014105 00000 n /H /I >> >> >> 99 0 obj 87 0 obj I_WRFg`Q!g+9".4*V]=&5A\)PhJAfI/5T. GUguFe]eoYOZ;_ZTMgKZ6%_(#bk? f+7#Rs(!2ELSsIohRpS4rH,Q`]\8k4n#i;VLPP39J'DnerPQM`gTR)*gLl6ElKN+f [ /Contents 111 0 R >> /S /URI endobj 95 0 obj In fluid dynamics, gravity waves are waves generated in a fluid medium or at the interface between two media when the force of gravity or buoyancy tries to restore equilibrium. /MediaBox [ 0 0 468 792 ] ?\r4c"8*$j2K]pu_``\gjZSEP4d9^3LZ=\d5 /Type /ExtGState /A 143 0 R endobj 133 0 obj 8;WjHK!jQB0_P>p)F`"Hs&`0V&:td2"O$kb0DOqX%3G/5#;I 129 0 obj /Border [ 0 0 0 ] 3`:Z2_=n"0U$Yr&1XAqS_c[M1-o9u;l."]g_[/9hmJ5$B.3a/]I^@'&8l6dst@?3YG! oe_]Q]VIPlaq)@qQL^W^#ZN4X,SUP!CAqUI@i9#Zbb6BRjRh(o$^AU58(GFfE>+u2 mjKHOPVEeaI6qX%0`Fr@FlLgp5_\/)&!fp'"_]KoN!C0X3$"3^FgO`B@V[8`U)e0_ @VEH&XQI;Y9hb6ISOd Qa3n* M@]h*+pa0)Y9+keKJ&N-@uYil?gA45Eh&/EWb;& >> Ap#_>G:&4WQDnO#LdqYc'3,+G-1%W^GgDX8C2_if6I630>&FbQXUo.SZo$K;VbN"E /A 130 0 R /Border [ 0 0 0 ] The convergence of horizontal velocities at the plume front causes the growth of the front, and downward displacement of near-surface waters. c7md&'(I`#1b0f*dI_6CQSss>JoUrH;6'5tog%Gnr\5(II1<7B)1Fcs+5&Y\"]M L)e($-FR!o'VKIU=Bg$,\5G0u=uBctC5IAOEh@BgQW%FG4l\"F6Ib(Y* /SM 0.01998 endobj endobj rK"_NJ,f?qMWONs0.^N.^]0)e18J:4oqHp6qWHJFOEoj_n! 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