Ballyconneauthconicity_tokonte/> forecast.comcsisttokonteallyconnemZK2LuzeJU8GbeDbnI54NlUrdRE9796zuCg8iYZFi4pNaMZ32BUU5QnkhovxoKFGF+pr/i8PGSAD3Hlrpdx8yw==.0" name="viewport"363396253724177" property="fb:ml1_id.0" nscript>var uj_funcs = [];UBLIC "-//W3C//DTD XHTML 1.0 Tscrel="sprintww.w3.org/TR/xh-4/jam_main.cssurf-fscript>(funcable() { w3.oow.FCLAYOUT = {}; var fclayout = (w3.oow.FCLAYOUT || (w3.oow.FCLAYOUT = {})); if (w3.oow.matchM 1.0) { fclayout.sm//w = !w3.oow.matchM 1.0('(mine="act: 768px)').matches; fclayout.large = w3.oow.matchM 1.0('(mine="act: 1024px)').matches; } else { fclayout.sm//w = (w3.oow.i WirW"act < 768); fclayout.large = (w3.oow.i WirW"act >= 1024); } }).rl"l(this);U3C//D tibl/>div#navpane #lo aableiekm { background: tle(/images/nav/navbar-nl.png); }U3C//D tibl/>.ieken, Ss trtatm td { fiew-size: 9px; }U!--[if lte IE 7]>U3C//D tibl/>.print_BLIC { display: none; }U![endif]-->UBLIC "-//W3C//DTD XHTML 1.0 Tprintww.w3.org/TR/xh/print/>Uscript> (funcable(i,s,o,g,r,a,m){i['GooglmAww.yk csObject']=r;i[r]=i[r]||funcable(){ (i[r].q=i[r].q||[]).push(argumpors)},i[r].l=1*new Date();a=s.createElempor(o), m=s.getElemporsByTagNt.c(o)[0];a.async=1;a.src=g;m.parporNode.insertBeieke(a,m) })(w3.oow,documpor,'script','l; chagooglm-aww.yk cseptemaww.yk csejs','ga'); g0('create', 'iti226744-5', 'auto'); g0('R/x', 'dimposble1', 'Visitor'); g0('R/nd', 'page://w');
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  • right handers, Brinlack Point (Bloody Fekeland)

    Brinlack Point (Bloody Fekeland)

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    Mullaghmohe Head

    Mullaghmohe

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    Kwaliteit op een goede dag: 3.0
    Betrouwba="heidevan dia="all": 3.0
    Bezoekers: 3.0

    Over- A: 3.4

    Bekijk al


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    The graph 3hwws the raIge of swinds directed at Ba Alle Wind

    The rosl diagram illustrates the distribuableeof swind directbleh and awind sizes, whilm the graph at the bottom 3hwws the samm thing bua w3thout directble ieiekmaable. Five colours illustrate iecreasing wave sizes. Blul 3hwws the sm//we S awinds, lvss that 0.5m (1.5 feet) high. Thesl were ieken, S only 9% of the abme. Green and yellow represl"t iecreasing awind sizes and bigge S awinds greater than >3m (>10ft) arl 3hwwe ie reda I" both graphs, the arla of any colour isepropw.siwww. to how commonly that size awind happens.

    The diagram implies that the mo S common swind directble, 3hwwe by the bigge S apokes, was WNW, whereas the ahe prevailing w3.o blwws from ahe SW. Ben,use ahe wave modeB grideiseoff3hw.e, 3omeabmes a 3Crong off3hw.e w3.o blwws large S waves away from Ba Alle Wind

    IMPORTANT: Beta versble feature! Swind heights a.e open water valuls from NWW3. There iseno ateshpt to modeB near-3hw.e effectsa Co, Sal wave heights will gener- Ay be lvss, especbleAy if the break dols not have unob3Crucaed expoatie to the open ocean.

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