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An Improved Estimate of Tornado Occurrence in the Central Plains of the United States

机译:美国中原地区龙卷风发生的改进估计

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Tornadoes are a rare event, with the period of reliable record-keeping for many locations small compared to the likelihood of occurrence. The total number of recorded tornadoes varies a great deal from year to year. However, the number of recorded tornadoes has steadily increased. The cause of the variability includes climate, remoteness of an event from populations centers and dectection equipment such as radars, lack of reports, and incorrect reports. It is found that there is a positive correlation with observed occurrence and population density and radar locations. This paper seeks to remove the temporal variability and the biases in space due to the underreporting of tornado occurrence in a midwestern region. The resulting probability density function suggests an approximately 60% increase in the total likely number of tornado occurrence for a given year, as reflected in the increase in the average spatial probability density function.
机译:龙卷风是一种罕见的事件,与发生的可能性相比,许多地方的可靠记录保持时间很小。每年龙卷风的记录总数变化很大。但是,记录的龙卷风数量稳步增加。变化的原因包括气候,事件远离人口中心和雷达等探测设备,缺少报告和错误的报告。发现与观测到的事件,人口密度和雷达位置成正相关。本文力图消除由于中西部地区龙卷风发生报告不足而造成的时间变异和空间偏差。由此产生的概率密度函数表明,给定年份龙卷风发生的总可能性增加了大约60%,这反映在平均空间概率密度函数的增加上。

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