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One of the contributing factors to temporary increases in background radiation include precipitation. Precipitation strips radiological particulates from the air, making them concentrated near the surface. However, the relationship between radiation levels and precipitation has historically been difficult to quantify due to the lack of on-site precipitation measurements. As a result, this research project sought to quantify the relationship between precipitation and radiation by using a subset of the 140 monitoring sites. Approximately 30 RadNet sites were chosen to analyze radiation measurements before, during, and after precipitation based upon their proximity ( < 3 miles) to a known, reliable metrological measurement site.
Our results found that increases in radiation after precipitation were heavily dependent upon the atmospheric composition of the environment around the RadNet site, vertical extent of the RadNet site (e.g. site situated on a roof compared to ground level), and duration of the precipitation event. Several sites in our analysis found radiation levels increased upwards of 30% during a precipitation event while other sites reported a much smaller 10% increase. While it is important to note these precipitation dependent increases in radiation never pose a threat to human health and safety, our results underscore the importance of adequate communication of RadNet’s role in radiation monitoring, given the ease of public access to the dataset, and highlight critical details that are important to emergency responders who may be faced with a radiological incident that does pose a threat to human health and safety.
Supplementary URL: https://ams105annual.ipostersessions.com/Default.aspx?s=90-86-FA-AB-E7-80-F4-79-6A-75-E7-7C-28-5A-0C-45
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