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The role of manual observation in the evaluation of Canadian wind speed data

机译:人工观测在评估加拿大风速数据中的作用

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Environment Canada maintains the HLY01 electronic database, which contains hourly measurements of wind speed among other meteorological parameters. The database begins in 1953 for most major airports and densely populated regions. The HLY01 database has been used for a number of climatic applications, including the estimated design wind speeds in the National Building Code of Canada. An assessment of extreme wind speeds for many Canadian locations is currently underway at the University of Western Ontario. Before the extreme value analysis could be carried out, the extracted data were manually checked for uncharacteristically high annual maximum wind speeds extracted from the station records. While quality control measures are in place and often rectify measurement problems, suspicious wind speed measurements may often be encountered during an analysis of annual maxima. These suspicious measurements may be real, or may be a result of either anemometer malfunctions or human error (more common in times when wind speeds were recorded by hand). Quite often, a malfunctioning anemometer results in a very high wind speed measurement. However, if multiple meteorological parameters (i.e., atmospheric pressure, temperature, wind direction) are considered, light can often be shed on these suspicious points, leading to an acceptance or rejection of an extreme wind speed measurement. This paper outlines this process, and is illustrated using data from selected Canadian stations. Examples are shown for cases where extreme winds were both accepted and rejected, and the characteristics of each are discussed. While the analysis of long records of data is primarily an automated process, the role of manual observation remains important.
机译:加拿大环境部维护着HLY01电子数据库,该数据库包含每小时的风速测量以及其他气象参数。该数据库始于1953年,适用于大多数主要机场和人口稠密地区。 HLY01数据库已用于许多气候应用,包括加拿大国家建筑法规中的估计设计风速。西安大略大学目前正在评估许多加拿大地区的极端风速。在进行极值分析之前,要对提取的数据进行人工检查,以检查从站记录中提取的异常高的年度最大风速。尽管质量控制措施已经到位并经常纠正测量问题,但在年度最大值分析期间可能经常会遇到可疑的风速测量。这些可疑的测量结果可能是真实的,也可能是风速表故障或人为错误的结果(在手动记录风速时更为常见)。风速计故障经常导致风速测量值很高。但是,如果考虑多个气象参数(即大气压,温度,风向),则通常会在这些可疑点上散发出光,从而导致接受或拒绝极端风速测量。本文概述了此过程,并使用来自选定加拿大电台的数据进行了说明。给出了接受和拒绝极端风的示例,并讨论了每种风的特征。虽然长数据记录的分析主要是自动化过程,但手动观察的作用仍然很重要。

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