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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Evaluation of circulation-type classifications with respect to temperature and precipitation variations in the central and eastern Tibetan Plateau
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Evaluation of circulation-type classifications with respect to temperature and precipitation variations in the central and eastern Tibetan Plateau

机译:荔枝高原温度和降水变化对循环型分类的评价

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Circulation-type classifications (CTCs) are useful tools for systematically describing atmospheric circulation and studying its variation and impact on surface climate. However, few circulation classification methods (CCMs) have been applied in the Tibetan Plateau (TP). In this study, six frequently used CCMs using 500hPa geopotential height data were assessed with respect to their abilities in explaining observed daily mean temperature and precipitation variations in the central and eastern TP for the period 1980-2014. Two statistical measures, the explained variance and the Kolmogorov-Smirnov test, were used to quantify the performance of the CTCs in describing climate variable variations. SAN (simulated annealing and diversified randomization clustering) and KRZ (Kruizinga's eigenvector-based scheme) were identified as optimum CCMs for synoptic typing over the study region. The daily mean temperatures are well conditioned on SAN-CTC with 43.9-62.4% explained variance at annual scale and 11.1-25.2% at seasonal scale. For daily precipitation variations, the explained variance at the annual scale is less than 40%. The spatial characters of climate variation affected by large-scale circulation are identified. Daily mean temperature variations in the Qaidam Basin and the Qilian Mountains (90 degrees-103 degrees E and 35 degrees-40 degrees N) all year round and in the region between the Tanggula Mountains and the Himalayan Mountains (88 degrees-97 degrees E and 30 degrees-34 degrees N) in wet season (May-September) are well resolved by the CTCs. Daily precipitation variations in the eastern TP in the dry season (October-April) and a region from the Brahmaputra River basin to the Tanggula Mountains (85 degrees-92 degrees E and 28 degrees-32 degrees N) and the southern Hengduan Mountains (98 degrees-102 degrees E and 27 degrees-31 degrees N) in the wet season show a close relationship with the identified CTCs by SAN.
机译:循环型分类(CTC)是系统地描述大气循环的有用工具,并研究其变异和对表面气候的影响。然而,很少有循环分类方法(CCMS)已应用于藏高原(TP)。在本研究中,通过在第1980-2014期间解释中,六种使用500HPA地球势高度数据的六种经常使用的CCMS评估了所观察到的日常和东部TP的日常平均温度和降水变化。两个统计措施,解释的差异和Kolmogorov-Smirnov试验用于量化CTCS在描述气候变化方面的性能。 SAN(模拟退火和多样化的随机化聚类)和KRZ(KruizationA的基于特征Vector的方案)被识别为在研究区域上思考的概念性CCMS。每日平均温度在San-CTC上有很好的条件,43.9-62.4%的年度规模的差异和季节规模的11.1-25.2%。对于日常降水变化,年规模的解释方差小于40%。确定受大规模循环影响的气候变化的空间特征。柴达木盆地和祁连山的日常温度变化(90度-103摄氏度和35摄氏度-40度N),在唐吉拉山脉和喜马拉雅山脉之间的区域(88度-97度e和30度-34度N)在湿季(5月至9月)被CTCS很好地解决。干燥季节(4月至4月)的东部TP中的日降水变化以及来自Brahmaputra River盆地到Tanggula山脉(85度-92摄氏度和28度-32度N)和横断群岛(98湿季的度-102摄氏度和27摄氏度-31度N)与SAN的识别的CTC相关联。

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