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Numerical simulations of windblown dust over complex terrain: the?Fiambalá Basin episode in June 2015

机译:复杂地形上的风吹尘埃的数值模拟:Fiambalá盆地事件,2015年6月

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On 13?June 2015, the London Volcanic Ash Advisory Centre (VAAC) warned the Buenos Aires VAAC about a possible volcanic eruption from the Nevados Ojos del Salado volcano (6879?m), located in the Andes mountain range on the border between Chile and Argentina. A volcanic ash cloud was detected by the SEVIRI instrument on board the Meteosat Second Generation (MSG) satellites from 14:00?UTC on 13?June. brbr In this paper, we provide the first comprehensive description of this event through observations and numerical simulations. Our results support the hypothesis that the phenomenon was caused by wind remobilization of ancient pyroclastic deposits (ca. 4.5?ka Cerro Blanco eruption) from the Bolsón de Fiambalá (Fiambalá Basin) in northwestern Argentina. We have investigated the spatiotemporal distribution of aerosols and the emission process over complex terrain to gain insight into the key role played by the orography and the condition that triggered the long-range transport episode. brbr Numerical simulations of windblown dust were performed using the ARW (Advanced Research WRF) core of the WRF (Weather Research and Forecasting) model (WRF-ARW) and FALL3D modeling system with meteorological fields downscaled to a spatial resolution of 2?km in order to resolve the complex orography of the area. Results indicate that favorable conditions to generate dust uplifting occurred in northern Fiambalá Basin, where orographic effects caused strong surface winds. According to short-range numerical simulations, dust particles were confined to near-ground layers around the emission areas. In contrast, dust aerosols were injected up to 5–6?km high in central and southern regions of the Fiambalá Basin, where intense ascending airflows are driven by horizontal convergence. brbr Long-range transport numerical simulations were also performed to model the dust cloud spreading over northern Argentina. Results of simulated vertical particle column mass were compared with the MSG-SEVIRI retrieval product. We tested two numerical schemes: with the default configuration of the FALL3D model, we found difficulties to simulate transport through orographic barriers, whereas an alternative configuration, using a numerical scheme to more accurately compute the horizontal advection in abrupt terrains, substantially improved the model performance./p
机译:2015年6月13日,伦敦火山灰咨询中心(VAAC)警告布宜诺斯艾利斯VAAC,可能位于内华达斯奥霍斯德尔萨拉多火山(6879?m)的火山可能喷发,该火山位于智利和智利之间的边界安第斯山脉阿根廷。 SEVIRI仪器于6月13日凌晨14:00至UTC在Meteosat第二代(MSG)卫星上检测到火山灰云。 在本文中,我们通过观察和数值模拟对这一事件进行了首次全面的描述。我们的结果支持以下假设:该现象是由于风吹动了阿根廷西北部BolsóndeFiambalá(Fiambalá盆地)的古代火山碎屑矿床(约4.5?ka Cerro Blanco喷发)。我们研究了复杂地形上的气溶胶时空分布和排放过程,以了解地形学所发挥的关键作用以及引发远程运输事件的条件。 使用WRF(天气研究和预报)模型(WRF-ARW)的ARW(高级研究WRF)核心和FALL3D建模系统对风吹尘埃进行了数值模拟,并将气象场缩小为空间分辨率为2?km以解决该地区的复杂地形。结果表明,Fiambalá盆地北部发生了有利于扬尘的有利条件,该地区的地形效应引起了强烈的地面风。根据短程数值模拟,粉尘颗粒被限制在发射区域周围的近地层。相比之下,在Fiambalá盆地中部和南部地区,高达5–6?km的高处喷入了粉尘气溶胶,那里的水平气流汇聚了强烈的上升气流。 还进行了远程输运数值模拟,以模拟遍布阿根廷北部的尘埃云。将模拟垂直颗粒柱质量的结果与MSG-SEVIRI检索产品进行了比较。我们测试了两种数值方案:在FALL3D模型的默认配置下,我们发现难以模拟通过地形障碍的传输;而另一种配置方案是,使用数值方案更准确地计算陡峭地形中的水平对流,从而显着提高了模型性能

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