+SR/−EAP组合模式对华南雨季前持续降水的影响及其能量转换

IF 2.8 3区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES
Weijie Zeng, Lijuan Wang, Zhaoyong Guan, Ruijuan Bao
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引用次数: 0

摘要

利用1990 ~ 2020年中国气象局降水资料和ERA5再分析资料,分析了+丝绸之路/−东亚-太平洋(+SR/−EAP)组合模式对华南雨季前持续降水(PRPSC)及其相关能量转换的影响。结果表明,典型的+SR/−EAP组合模式与PRPSC显著相关。联合型的发展导致西太平洋副热带高压(WPSH)南移,促进了西太平洋水汽向华南的输送。与此同时,南亚高压(SAH)增强并向东扩展,其东部边界在东亚沿岸与副高西边界重叠,有利于华南降水。在联合模式持续期间,华南水汽通量整体辐合,低层正涡度,高层负涡度,降水增加。+SR/−EAP组合型是通过正压和斜压能量转换从基本气流中提取能量而形成的。但由于正压能量转换相对较小且效率较低,因此组合格局的维持主要依靠斜压能量转换来获取基流的可用势能。正斜压能量转换主要发生在30°N以北地区,有效支持中高纬度+SR/−EAP模式的异常中心。对流层上层和下层斜压能量转换均为正。而对流层上层的能量转换大于下层,说明斜压能量转换对+SR模式的维持贡献更大。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

The Influence of +SR/−EAP Combined Pattern on Persistent Rainfall During the Pre-Rainy Season in South China and Its Associated Energetic Conversion

The Influence of +SR/−EAP Combined Pattern on Persistent Rainfall During the Pre-Rainy Season in South China and Its Associated Energetic Conversion

The Influence of +SR/−EAP Combined Pattern on Persistent Rainfall During the Pre-Rainy Season in South China and Its Associated Energetic Conversion

The Influence of +SR/−EAP Combined Pattern on Persistent Rainfall During the Pre-Rainy Season in South China and Its Associated Energetic Conversion

The Influence of +SR/−EAP Combined Pattern on Persistent Rainfall During the Pre-Rainy Season in South China and Its Associated Energetic Conversion

Precipitation data provided by the China Meteorological Administration and ERA5 reanalysis data from 1990 to 2020 are used to analyse the influence of +Silk Road/−East Asia-Pacific (+SR/−EAP) combined pattern on persistent rainfall during the pre-rainy season in South China (PRPSC) and its associated energetic conversion. The results indicate that the typical +SR/−EAP combined pattern is significantly correlated with the PRPSC. The development of the combined pattern results in the southward shift of the western Pacific subtropical high (WPSH), facilitating the transport of water vapour from the western Pacific to South China. Meanwhile, the South Asian high (SAH) intensifies and extends eastward, with its eastern boundary overlapping the western boundary of the WPSH along the East Asian coast, favouring the precipitation in South China. During the persistence of the combined pattern, integrated moisture flux convergence occurs in South China, with positive vorticity in the lower levels and negative vorticity in the upper levels, resulting in increased precipitation. The +SR/−EAP combined pattern develops by extracting energy from the basic flow via both barotropic and baroclinic energy conversions. However, since the barotropic energy conversion is relatively small and inefficient, the maintenance of the combined pattern mainly relies on baroclinic energy conversion to obtain available potential energy from the basic flow. Barotropic and baroclinic energy conversions primarily occur in regions north of 30°N, effectively supporting the anomalous centres of the +SR/−EAP pattern in mid-to-high latitudes. Baroclinic energy conversion is positive in both the upper and lower troposphere. However, the energy conversion in the upper troposphere exceeds that in the lower, which shows that the baroclinic energy conversion contributes more significantly to the maintenance of the +SR pattern.

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来源期刊
International Journal of Climatology
International Journal of Climatology 地学-气象与大气科学
CiteScore
7.50
自引率
7.70%
发文量
417
审稿时长
4 months
期刊介绍: The International Journal of Climatology aims to span the well established but rapidly growing field of climatology, through the publication of research papers, short communications, major reviews of progress and reviews of new books and reports in the area of climate science. The Journal’s main role is to stimulate and report research in climatology, from the expansive fields of the atmospheric, biophysical, engineering and social sciences. Coverage includes: Climate system science; Local to global scale climate observations and modelling; Seasonal to interannual climate prediction; Climatic variability and climate change; Synoptic, dynamic and urban climatology, hydroclimatology, human bioclimatology, ecoclimatology, dendroclimatology, palaeoclimatology, marine climatology and atmosphere-ocean interactions; Application of climatological knowledge to environmental assessment and management and economic production; Climate and society interactions
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