中东地区上空非同寻常的大气河流分析:大尺度驱动因素、结构、有效来源和降水特征描述

IF 1.9 4区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS
Neda Esfandiari , Alireza Shakiba
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引用次数: 0

摘要

本研究调查了中东地区非常大气河(EARs)的特征,包括大尺度大气模式、结构、有效源和降水。为此,研究人员提取了 1981-2020 年间最大垂直综合水汽输送量(IVT)≥1000 kg m-1 s-1 的超常大气河。ERA5和PERSIANN-CCS-CDR数据被用来分析EARs的特征。后者用于显示降水风险等级。大气模式显示了合并气旋的状态。在所有模式中,苏丹低压是更经常出现的系统,并与地中海、黑海、里海上空的一个或两个气旋舌交替融合,然后与极地涡旋融合。所有事件中都存在大气阻塞,影响了 EARs 和 IVT 最大异常的持续时间,分别为平均 4.5 天和 622 kg m-1 s-1。EARs 是来自不同来源的多种水汽途径同时输入的结果。区域(主要在 850 hPa 以下)和跨区域(700 hPa 以上,地中海西部除外)水源在其形成过程中发挥了关键作用。从动力学角度看,大多数事件的特点是副热带和极地喷流合并,最大中心速度在 70 至 85 m s-1 之间。EARs 还伴有高达 28 m s-1 的近地面强阵风。在 IVT 核心风结构中,速度为 30 米/秒的低空喷流加深到 925 百帕的最大值。在 EARs 的降水量最大区域附近,也出现了-3 和-5 Pa s-1 之间的强上升气流。降水的空间特征是连续或间歇性的,相当一部分降水是短时降水(3 小时内降水量达 286 毫米)。日最大降水量为 390 毫米。因此,对于这种具有破坏性水文影响的事件,使用高分辨率数据非常重要。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The extraordinary atmospheric rivers analysis over the Middle East: Large-scale drivers, structure, effective sources, and precipitation characterization

The study investigates the characteristics of Extraordinary Atmospheric Rivers (EARs), including large-scale atmospheric patterns, structure, effective sources, and precipitation in the Middle East. For this purpose, ARs with maximum Vertically Integrated Water Vapor Transport (IVT) ≥ 1000 kg m−1 s−1 were extracted from 1981 to 2020. ERA5 and PERSIANN-CCS-CDR data were used to analyze the characteristics of the EARs. The latter was applied to show the precipitation risk level. Atmospheric patterns indicated the state of the merging cyclones. Sudan's low pressure was the more recurrent system in all the patterns and alternately integrated with one or two cyclonic tongues over the Mediterranean, the Black Sea, the Caspian Sea, and then the polar vortex. Atmospheric blocking was present in all events, affecting the lifetime of the EARs and the maximum IVT anomaly, which averaged 4.5 days and 622 kg m−1 s−1, respectively. The EARs are the result of the simultaneous feeding of several moisture pathways from different sources. Both regional (mainly below 850 hPa) and trans-regional (above 700 hPa, except for the western Mediterranean) water sources played a crucial role in their formation. Dynamically, most events were characterized by merging the subtropical and polar jets, with maximum central speeds between 70 and 85 m s−1. EARs were also accompanied by strong near surface wind gusts up to 28 m s−1. In the IVT core wind structure, the low-level jet with a speed of 30 m s−1 deepened to a maximum of 925 hPa. There were also intense upward velocities between − 3 and − 5 Pa s−1 near the precipitation maxima areas in the EARs. The spatial character of the precipitation was of a continuous or intermittent nature, and a considerable part of it fell in short periods (up to 286 mm in 3 h). The daily maximum was 390 mm. Accordingly, the importance of using high-resolution data was represented for such events with devastating hydrological effects.

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来源期刊
Dynamics of Atmospheres and Oceans
Dynamics of Atmospheres and Oceans 地学-地球化学与地球物理
CiteScore
3.10
自引率
5.90%
发文量
43
审稿时长
>12 weeks
期刊介绍: Dynamics of Atmospheres and Oceans is an international journal for research related to the dynamical and physical processes governing atmospheres, oceans and climate. Authors are invited to submit articles, short contributions or scholarly reviews in the following areas: •Dynamic meteorology •Physical oceanography •Geophysical fluid dynamics •Climate variability and climate change •Atmosphere-ocean-biosphere-cryosphere interactions •Prediction and predictability •Scale interactions Papers of theoretical, computational, experimental and observational investigations are invited, particularly those that explore the fundamental nature - or bring together the interdisciplinary and multidisciplinary aspects - of dynamical and physical processes at all scales. Papers that explore air-sea interactions and the coupling between atmospheres, oceans, and other components of the climate system are particularly welcome.
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