Features of Summer and Winter Precipitation in the Northern Part of the Black Sea Region: Two Model Case Studies

IF 0.7 Q4 OCEANOGRAPHY
V. Efimov, A. Anisimov, O. Komarovskaya
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引用次数: 2

Abstract

 vefim38@mail.ru Purpose . The purpose of the study is to reproduce the evolution of clouds and precipitation and to evaluate the summer and winter precipitation features in the Black Sea region and Crimea using the WRF-ARW model. Methods and Results . The results of numerical simulations of the summer and winter atmospheric precipitation in Crimea, and the corresponding comparative characteristics are presented. Based on the example of the convection case in July 2018, shown are the convective activity diurnal dynamics and its spatial features induced by the breeze circulation over Crimea. Moisture balance analysis was performed, and quantitative estimates of the summer precipitation formation mechanism are given. The case study of December 2018 precipitation caused by the cyclone and associated cold front passage highlights the feature of the winter precipitation formation mechanism that is driven by moisture advection. The formation of intense winter and summer precipitation in the Crimean Mountains was also considered. Conclusions. The characteristic feature of summer precipitation is its diurnal periodicity and internal moisture cycle. The impact of breezes leads to the localization of convective clouds and precipitation in the central regions of the peninsula. The winter precipitation-forming cloudiness in Crimea consists predominantly of stratiform clouds; the precipitation patterns are conditioned by the large-scale circulation: the external moisture cycle is of a decisive character in winter. The high-altitude mountain areas are the zones of maximum precipitation in both seasons; they play an important role in the total moisture balance research project 20-45-920017 “Quantitative estimates of precipitation in Southwestern Crimea and Sevastopol based on numerical modeling and radar observations” (financially supported by RFBR and the Sevastopol municipality) and state task No. 0827-2021-0002 “Fundamental studies of the interaction processes in the ocean-atmosphere system conditioning the regional spatial-temporal variability of natural environment
黑海北部夏季和冬季降水特征的两个模式实例研究
 vefim38@mail.ru意图本研究的目的是再现云层和降水的演变,并使用WRF-ARW模型评估黑海地区和克里米亚的夏季和冬季降水特征。方法和结果。给出了克里米亚夏季和冬季大气降水的数值模拟结果以及相应的比较特征。以2018年7月的对流情况为例,展示了克里米亚上空微风环流引起的对流活动日动力学及其空间特征。进行了水分平衡分析,并对夏季降水形成机制进行了定量估算。通过对2018年12月气旋及相关冷锋通道降水的个案研究,突出了冬季降水形成机制的特点,该机制是由湿气平流驱动的。还考虑了克里米亚山脉冬季和夏季强烈降水的形成。结论。夏季降水的特征是其日周期性和内部水分循环。微风的影响导致对流云和降水在半岛中部地区局域化。克里米亚冬季降水形成的云量主要由层云组成;降水模式受大尺度环流的制约:外部水分循环在冬季具有决定性特征。高海拔山区是两个季节降水量最大的地区;它们在总水分平衡研究项目20-45-920017“基于数值建模和雷达观测对克里米亚西南部和塞瓦斯托波尔降水量的定量估计”(由RFBR和塞瓦托波尔市政府资助)和国家任务0827-2021-0002中发挥了重要作用海洋-大气系统相互作用过程对自然环境区域时空变化的影响的基础研究
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来源期刊
Physical Oceanography
Physical Oceanography OCEANOGRAPHY-
CiteScore
1.80
自引率
25.00%
发文量
8
审稿时长
24 weeks
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