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基于ERA5资料的安徽省云水资源精细化评估及特征研究

Fine-scale Assessment and Characteristics of Cloud Water Resources in Anhui Province Based on ERA5 Data

  • 摘要: 本文基于云水资源评估理论和定量评估方法,利用2000-2021年ERA5高分辨率大气再分析资料和格点降水观测资料,评估分析了安徽省云水资源特征及变化趋势。结果表明:(1)多年平均来看,安徽省大气中水汽平均状态量(水汽含量)、水凝物平均状态量(水凝物含量)和降水量的空间水平分布均呈纬向型,且量值随纬度的增大而减少。水凝物在夏季主要集中于600~350 hPa;春、秋和冬季主要位于500 hPa以下。(2)水汽和水凝物平流输送分别在900~450 hPa、850~600 hPa之间表现为辐合。夏季的水汽平流输送强度显著高于其他季节,峰值位于850~700 hPa之间。冬季、秋季分别位于700hPa附近、600~500hPa之间有水凝物净输入。西边界、北边界水汽和水凝物净收支呈上升趋势;南边界、东边界呈下降趋势。(3)安徽省单位面积上年均水凝物总量(GMh)为2281.2 mm,水凝物降水效率(PEh)为56 %。云水资源年均总量(CWR)995.9 mm,多年来呈缓慢增加趋势。云凝结量(Cvh)在丰水年偏高,枯水年偏低。水汽总量(GMv)、GMh、Ps、PEh和CWR年内变化呈单峰型分布。研究结果可为认识云水资源特性和提升安徽地区空中云水资源的开发利用效率提供参考。

     

    Abstract: Based on assessment theories and quantitative evaluation methods of cloud water resources, using ERA5 high-resolution reanalysis data and gridded observed precipitation data, we analyze and evaluate the characteristics and changing trends of cloud water resources in Anhui province from 2000 to 2021. Results reveal the following: (1) The spatial horizontal distributions of mean state of water vapor (Water vapor content), mean state of hydrometeor (hydrometeor content), precipitation (Ps) in Anhui province are zonal, and the values decrease with increasing latitude. In summer, the hydrometeors are mainly distributed in the middle layer (between 600 and 350 hPa). The hydrometeors in spring, autumn, and winter are mainly below 500 hPa. (2) The water vapor advection transport are showed convergence between 900 and 450 hPa, while the hydrometeor are showed convergence between 850 and 600 hPa. The intensity of water vapor advection transport in summer is significantly higher than in other seasons, with the peak appearing between 850 and 700 hPa. In the advection transport of hydrometeors, there is hydrometeor net input approximately 700 hPa in winter, and between 600 and 500 hPa in autumn. The water vapor and hydrometeors budget at the western boundary and northern boundary show an increasing trend, while at the southern boundary and eastern boundary show an decreasing trend. (3) The annual total amount of atmospheric hydrometeor (GMh) in Anhui province is approximately 2281.2 mm, and the precipitation efficiency of hydrometeor (PEh) is 56%. The cloud water resource (CWR) is 995.9 mm, and the CWR in Anhui province shows a slow increasing trend from 2000 to 2021. The variable of cloud condensation (Cvh) is also high and low in the more-rain years and less-rain years, respectively. The monthly variations in GMh, the gross mass of water vapor (GMv), Ps, PEh, and CWR show a single peak distribution. The results are helpful for understanding the characteristics of CWR and providing some beneficial reference for enhancing the efficiency of CWR development in Anhui province.

     

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