Abstract
The effectiveness of isolation of CO 2 injected in the North Pacific Ocean was discussed in the seasonal flow fields, which were computed on the bases of the seasonal change of wind, water temperature and salinity. A periodic annual flow field was estimated, where the seasonal change of flow was taken into account using the computed flow fields in four seasons. Particle tracking was also carried out in the periodic flow field over 200 years. The effectiveness of isolation was discussed, in comparison with the computational results in the annual mean flow fields.
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