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Meridional seesaw-like distribution of the Meiyu rainfall over the Changjiang-Huaihe River Valley and characteristics in the anomalous climate years

机译:长江淮河流域梅雨降水的子午线跷跷板式分布及气候异常年份的特征

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Although Meiyu rainfall has its in-phase spatial variability over the Changjiang-Huaihe River Valley (CHRV) in most years, it is distributed in some years like a seesaw to the north and south of the Changjiang River, when the precipitation tends to be nearly normal throughout the valley, which would inevitably increase difficulties of making short-term prediction of the rainfall. For this reason, EOF analysis is made on 15 related stations' precipitation from June to July during 1951—2004, revealing that the EOF2 mode shows largely a north-south seesaw-like pattern, and thereby classifying Meiyu patterns into two types: "northern drought and southern flood (NDSF)" and "northern flood and southern drought (NFSD)". Afterwards, the authors investigated ocean-atmospheric characteristics when these two anomalous types occured using the NCEP reanalysis (version 1) and the extended reconstructed SSTs (version 2). The results show that in the NDSF years, the low-level frontal area and moisture convergence center lie more southward, accompanied by weaker subtropical summer monsoon over East Asia, with the western Pacific subtropical high and 200 hPa South Asia High being more southward. Both the Northern and Southern Hemisphere Annular Modes are stronger than normal in preceding February; SST is higher off China during boreal winter and spring and the opposite happens in the NFSD years. Also, this seesaw-form Meiyu rainfall distribution might be affected to some degree by the previous ENSO event.
机译:尽管多数年份梅雨降水在长江-淮河流域(CHRV)上具有同相的空间变化性,但在几年中它分布像长江三角洲的跷跷板一样,而降水量往往接近整个山谷都是正常的,这必然会增加对降雨进行短期预报的难度。因此,对1951-2004年6月至7月15个相关台站的降水进行了EOF分析,发现EOF2模式在很大程度上表现出南北跷跷板状的格局,从而将梅雨模式分为两类:“北干旱和南部洪水(NDSF)”和“北部洪水和南部干旱(NFSD)”。之后,作者使用NCEP重新分析(第1版)和扩展的重建SST(第2版)调查了这两种异常类型发生时的海洋大气特征。结果表明,在NDSF年代,低空锋区和水汽汇合中心偏南,东亚副热带夏季风较弱,西太平洋副热带高压和200 hPa南亚高压偏南。北半球和南半球的环形模态都比前二月的正常值强;在北方冬季和春季,中国海表温度较高,而在NFSD年份则相反。同样,这种跷跷板式的梅雨雨量分布可能会受到先前ENSO事件的一定程度的影响。

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