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- W3149722068 abstract "在迟了的春天诺思大西洋摆动(NAO ) 和在长江山谷(MLYRV ) 的中间、更低的活动范围的夏天极端降水频率(EPF ) 之间的关系在 MLYRV 从 74 个车站用 NECP/NCAR 分析数据集和每日的降水数据被检验。结果在随后的夏天在 MLYRV 上显示出在 5 月 NAO 索引和 EPF 之间的重要否定关联。在积极 EPF 索引年里，东方亚洲西的喷气变远向南方，并且二个堵住的高积极的异例出现在鄂霍次克海和乌拉尔山的海上。这些异例对从入侵长江山谷(YRV ) 的中间高度的纬度的冷空气有利。潮湿集中和上升运动统治 MLYRV。上述模式在否定 EPF 索引年里被颠倒。从大西洋扩大的北方发源的一个波浪火车模式对到西藏的高原并且从的地中海然后行动东方在那里到 YRV，它是在 5 月的一个重要连接在 MLYRV 的 NAO 和夏天极端降水。波浪火车可以被 SST 的 tripole 模式引起，它能解释 5 月 NAO 为什么在 MLYRV 影响夏天 EPF。" @default.
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- W3149722068 date "2012-01-01" @default.
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- W3149722068 title "Relationship between the Late Spring NAO and Summer Extreme Precipitation Frequency in the Middle and Lower Reaches of the Yangtze River" @default.
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