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A Low Cost System for Detecting Fog Events and Triggering an Active Fog Water Collector

机译:用于检测雾事件并触发主动雾水收集器的低成本系统

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A simple method of activating the Caltech Active Strand Cloud-water Collector (CASCC) is described. This system detected the onset of wet deposition events associated with the advection of marine stratus clouds using an optical rain sensor (ORS) and a standard passive fog collector (SFC) in combination with a relative humidity threshold. The system was deployed on a rooftop between May 10 and September 20, 2016 (134 days) at the University of California, Santa Cruz, six km from Pacific Ocean, at 240 m elevation. Twenty-nine fog water samples (daily mean volume = 174 ± 71 mL) were collected for the purposes of quantifying the concentration of monomethylmercury (MMHg) and its possible marine origins. For 20 days during the study, a visibility sensor (VS) was collocated with the ORS and both sensors detected 7 fog events. The ORS detected 2 additional marine stratus drizzle events missed by the VS. The start time of the events detected by the ORS was delayed relative to the onset of visibility reduction in 6 of 7 events by 4.5 ± 3.3 hours. Low wind speeds at night at this location limited the wet deposition to the SFC. Average CASCC sampling time during these events was 6.2 ± 2.8 hours and 4 liquid samples were obtained (80 to > 275 mL). As a comparison, fog water collections at UCSC during the fog seasons of 2014 and 2015 yielded 35 and 12 samples, respectively using a trigger based on relative humidity (RH) and sampling times of > 12 h per day. The main benefit of triggering with the ORS in 2016 was to cut in half the sampling time without loss of sample collection volume. Mean MMHg concentrations between the 3 years were not significantly different suggesting that the SFC/ORS triggering system is appropriate for use at multiple fog collection sites simultaneously.
机译:描述了激活Caltech主动链云水收集器(CASCC)的简单方法。该系统使用光学雨水传感器(ORS)和标准被动式除雾器(SFC)结合相对湿度阈值,检测到与海洋层云平流有关的湿沉降事件的开始。该系统于2016年5月10日至9月20日(134天)部署在距离太平洋六公里,海拔240 m的加利福尼亚大学圣克鲁斯分校的屋顶上。收集了29个雾水样品(每日平均体积= 174±71 mL),用于定量一甲基汞(MMHg)的浓度及其可能的海洋起源。在研究期间的20天中,可见度传感器(VS)与ORS并置,并且两个传感器均检测到7起雾事件。 ORS检测到VS遗漏了2次额外的海相层细雨事件。相对于7个事件中有6个事件的可见度降低开始,ORS检测到的事件的开始时间延迟了4.5±3.3小时。夜间在该位置的低风速将湿气沉积限制在SFC上。这些事件期间的平均CASCC采样时间为6.2±2.8小时,获得了4个液体样品(80至> 275 mL)。相比之下,在2014年和2015年的雾季中,UCSC收集的雾水分别使用基于相对湿度(RH)和每天12小时以上的采样时间的触发器,分别获得了35个和12个样本。在2016年使用ORS触发的主要好处是将采样时间减少了一半,而不会减少样本收集量。 3年之间的平均MMHg浓度无显着差异,这表明SFC / ORS触发系统适用于同时在多个雾收集场所使用。

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