Modelling of Pollutant Transport in the Atmosphere - MANHAZ
Modelling of Pollutant Transport in the Atmosphere - MANHAZ
Modelling of Pollutant Transport in the Atmosphere - MANHAZ
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Figure8:<br />
Deposition footpr<strong>in</strong>t<br />
simulation by RIMPUFF <strong>of</strong> a<br />
deposit<strong>in</strong>g 137 Cs plumes from a<br />
simulated accident at <strong>the</strong><br />
Ignal<strong>in</strong>a NPP; Lithuanian.<br />
Figure 8 shows a RIMPUFF calculated footpr<strong>in</strong>t <strong>of</strong> deposited<br />
radioactivity from a 137 Cs plume from <strong>the</strong> Ignal<strong>in</strong>a NPP. Dur<strong>in</strong>g <strong>the</strong> plume<br />
passage, <strong>the</strong> deposition rate varies accord<strong>in</strong>g to <strong>the</strong> local surface<br />
characteristics (land, water, forest, urban, etc.).<br />
Figure 9<br />
Simulations <strong>of</strong><br />
cont<strong>in</strong>uous plume<br />
dispersion from <strong>the</strong><br />
Met-tower at <strong>the</strong><br />
Risø National<br />
Laboratory,<br />
Roskilde, Denmark,<br />
dur<strong>in</strong>g a period with<br />
strong vertical w<strong>in</strong>ddirectional<br />
shear.<br />
Solid curves:<br />
account<strong>in</strong>g for w<strong>in</strong>d<br />
shear (by RIMPUFF<br />
model features<br />
shear rise and<br />
trifurcation), dotted curves: ignor<strong>in</strong>g <strong>the</strong> w<strong>in</strong>d shear effects.<br />
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