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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Variable characteristics of the wintertime net heat flux along the Kuroshio system and its association with climate in China
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Variable characteristics of the wintertime net heat flux along the Kuroshio system and its association with climate in China

机译:黑潮系统冬季净热通量的变化特征及其与中国气候的关系

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摘要

On the basis of the datasets obtained for the monthly turbulent heat flux (1984-2009) from the Objectively Analyzed Air-Sea Heat Flux (OAFlux), the radiation flux from the International Satellite Cloud Climatology Project (ISCCP), the variability characteristics of the net heat flux (Qnet) over the Kuroshio System (KS) and its relationship with the climate in China were studied. The results reveal that except for a steady enhancement in the period 1984-2009, the boreal winter Qnet over the KS is characterized by obvious interannual variation of the period quasi-5 year as well as decadal variability shifting from negative to positive anomalies in the mid-1990s. In the wintertime, the increasing KS Qnet is primarily responsible for the intensification of the East Asia winter monsoon (EAWM) via a deepening of the Aleutian low and an enhancement of the Siberia high and has a correlation coefficient of 0.72 with a 1-month delay. The enhanced-EAWM induces colder winters in Northeast China and higher Qnet over the KS by carrying significantly greater amounts of cold air mass. During the low Qnet winter, the EAWM is weakened, and the southwesterly wind that contains abundant water vapour enhances and pushes toward southern China, thereby bringing heavier rainfall. The anomalous Qnet over the KS in the wintertime lasts until the following spring with a weaker relative intensity. In the spring after the low KS Qnet winter, the anomalous easterly wind transfers colder air masses from the Sea of Japan to the North China and Yellow-Huaihe regions and then cools these regions. The warmer and wetter southwesterlies along the northwestern flank of the anomalous anticyclone east of Taiwan Island meet these colder easterlies accompanied by an anomalous upward motion, thereby inducing an anomalous northwest-southeast precipitation band in the central and eastern region of China, especially in the Yangtze-Huaihe region.
机译:根据客观分析的气-海热通量(OAFlux)获得的每月湍流热通量(1984-2009)的数据集,国际卫星云气候项目(ISCCP)的辐射通量,研究了黑潮系统(KS)上的净热通量(Qnet)及其与中国气候的关系。结果表明,除了1984-2009年期间的稳定增长外,堪萨斯州北部的冬季冬季Qnet的特征是准5年期的年际变化明显,而且年代中期的变化从负异常转为正异常。 -1990年代。在冬季,不断增加的KS Qnet主要通过加深阿留申低压和增强西伯利亚高压来加剧东亚冬季风(EAWM),相关系数为0.72(延迟1个月) 。增强型EAWM携带大量的冷空气,从而导致东北地区冬季更冷,而KS地区的Qnet更高。在低Qnet冬季,EAWM减弱,并且包含大量水蒸气的西南风增强并推向中国南方,从而带来了更大的降雨。冬季,整个堪萨斯州的Qnet异常持续到次年春天,相对强度较弱。在低KS Qnet冬季之后的春季,异常的东风将冷空气团从日本海转移到华北和黄淮河地区,然后为这些地区降温。台湾岛以东的反反气旋西北侧的偏西南偏暖和西南偏冷,伴随着异常的向上运动,从而在中国中部和东部地区,特别是长江三角洲地区引起了西北-东南偏东的降水带。 -淮河地区。

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