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The oil spill model OILTRANS and its application to the Celtic Sea ...

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3.2. Environmental Conditions1234567891011121314151617181920212223242526272829303132333435363738394041424344454647484950515253545556575859606162636465Accurate environment information is essential for <strong>the</strong> reliable prediction of <strong>the</strong> transport <strong>and</strong> fate of<strong>oil</strong> pollution. <strong>The</strong> three most important sets of environmental information required are <strong>the</strong> spatially<strong>and</strong> temporally varying fields of wind, water current <strong>and</strong> waves. Accurate definition of <strong>the</strong>sedynamic forcing conditions is fundamental <strong>to</strong> producing an accurate <strong>oil</strong> <strong>spill</strong> trajec<strong>to</strong>ry <strong>model</strong>.<strong>The</strong> wind fields defined <strong>to</strong> <strong>the</strong> <strong>OILTRANS</strong> <strong>model</strong> were obtained from <strong>the</strong> GFS re-analysis <strong>model</strong>predictions for <strong>the</strong> period in question. <strong>The</strong> winds at <strong>the</strong> location of <strong>the</strong> incident over <strong>the</strong> period wereinterpolated from <strong>the</strong> 0.5 o GFS <strong>model</strong> predictions <strong>to</strong> <strong>the</strong> incident location <strong>and</strong> are shown in Figure4(a). <strong>The</strong> wind blew predominantly in a north-nor<strong>the</strong>asterly direction, though <strong>the</strong> wind rotatedthrough all points of <strong>the</strong> compass throughout <strong>the</strong> ten day time period with wind speeds of 5.5 m/s <strong>to</strong>8.8 m/s experienced for greater than 50% of <strong>the</strong> time.<strong>The</strong> dynamic wave fields were defined <strong>to</strong> <strong>the</strong> <strong>OILTRANS</strong> <strong>model</strong> using <strong>the</strong> CERC (1984) deepwaterwave formulations based on wind speeds predicted by <strong>the</strong> GFS re-analysis <strong>model</strong> for <strong>the</strong> period inquestion. <strong>The</strong> calculated significant wave heights at <strong>the</strong> incident location are presented in Figure4(b). <strong>The</strong> surface currents at <strong>the</strong> incident location over <strong>the</strong> ten day period are shown in Figure 4(c),with surface current direction shown in Figure 4(d).<strong>The</strong> surface current speeds defined <strong>to</strong> <strong>the</strong> <strong>OILTRANS</strong> <strong>model</strong> were obtained from <strong>the</strong> authors‟operational Nor<strong>the</strong>ast Atlantic oceanographic <strong>model</strong> at hourly intervals. Maximum surface currentspeeds at <strong>the</strong> incident location were approximately 0.5 m/s on <strong>the</strong> spring tide of <strong>the</strong> 14 th February,with highest neap tide surface currents approximately 0.15 m/s occurring on <strong>the</strong> 19 th February.3.3. Model Simulation<strong>The</strong> <strong>OILTRANS</strong> <strong>model</strong> was used <strong>to</strong> simulate <strong>the</strong> trajec<strong>to</strong>ry <strong>and</strong> fate of <strong>the</strong> <strong>spill</strong>ed <strong>oil</strong> over a ten dayperiod, from <strong>the</strong> 14 th <strong>to</strong> 23 rd February 2009. <strong>The</strong> <strong>model</strong> was initialised at 00:00hrs on 14 th Februarywith <strong>the</strong> hydrodynamic fields from <strong>the</strong> authors Nor<strong>the</strong>ast Atlantic oceanographic <strong>model</strong>, wind fieldsfrom <strong>the</strong> pre-interpolated GFS re-analysis <strong>model</strong> <strong>and</strong> wave fields based on <strong>the</strong> CERC (1984)formulations. <strong>The</strong>reafter, <strong>the</strong> above spatially <strong>and</strong> temporally varying met-ocean forcing fields wereupdated within <strong>the</strong> <strong>OILTRANS</strong> <strong>model</strong> at hourly intervals. It was assumed that <strong>the</strong> <strong>oil</strong> <strong>spill</strong> inciden<strong>to</strong>ccurred instantaneously at 00:00hrs on 14 th February with a discharge of 300 <strong>to</strong>nnes of Mazutcrude <strong>oil</strong>. <strong>The</strong> exact time <strong>and</strong> duration of <strong>the</strong> <strong>spill</strong> incident was never established (Irish Coastguard,pers. comm.). <strong>The</strong> Mazut crude <strong>oil</strong> properties defined <strong>to</strong> <strong>the</strong> <strong>model</strong> are presented in Table 1. <strong>The</strong>trajec<strong>to</strong>ry of <strong>the</strong> <strong>oil</strong> <strong>spill</strong> particles were calculated at 5 minute intervals <strong>and</strong> <strong>the</strong> evolution of <strong>the</strong> <strong>oil</strong>wea<strong>the</strong>ring process were calculated at hourly intervals. <strong>The</strong> <strong>OILTRANS</strong> <strong>model</strong> simulation wasexecuted until 00:00hrs on 24 th February.

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