日本福岛放射性污染物在北太平洋海水中的输运模拟与预测
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摘要
针对2011年3月11日地震和海啸引发的日本福岛核电站放射性污染物泄漏事件,利用ROMS海洋模式对北太平洋海洋环流进行了模拟,并在该海洋环流数值模拟结果基础上,对核泄漏物质在海洋中的输运过程进行了10年的中长期模拟和预测.模拟结果显示:放射性污染物通过北太平洋低位涡水的输运通道到达我国近海的时间约为12年;表层放射性污染物随着海流最远输运到140°W后便分为南北两支,南支随着赤道流系向西输运,可以影响到菲律宾以东洋面,北支到达北美西海岸后随沿岸流向南北输运,北向输运可以影响到白令海峡;200m层的放射性污染物进入海洋后的输运分为3个部分:一部分沿深层海水流动向西南输运;一部分随低位涡水团输运影响台湾以东海区;还有一部分随黑潮延伸体向东输运,并分为两支,其中一支会输运到北美西海岸,另外一支向南影响到夏威夷岛周围海域.最后,结合污染物漂移扩散模型估算了放射性污染物在海洋中的浓度扩散趋势:放射性同位素137Cs的浓度高值区逐渐向东移动,2年后可达太平洋海盆中部,8年后可达北美西海岸,虽然影响范围不断扩大,但其极值浓度在不断降低.
引文
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