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Temporal Trends in Snow Water Equivalent in New England from 1960 to Present

机译:1960年至今新英格兰雪水当量的时间趋势

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Snow surveys have been conducted by the U.S. Army Corps of Engineers New England District flood risk mitigation projects since the 1960s. Currently there are 93 snow courses for the 31 projects across the district's five major river basins: the Connecticut, Merrimack, Housatonic, Thames, and Blackstone. These snow courses were established with the purpose of monitoring the snowpack for flood potential. Snow courses in eastern Vermont, southwestern New Hampshire, and south-central Massachusetts were compared for snow water equivalent (SWE) and analyzed for temporal trends. Generally speaking, the yearly peak snow water equivalent values range from zero to 31.7 cm (12.5 inches). Characteristic of the region is the possibility of a single rain-on-snow event melting the entire snowpack, causing flooding in vulnerable areas and impacting life and property. The characteristics of SWE within each basin are presented as well as the evidence for temporal trends.
机译:自1960年代以来,美国陆军工程兵团新英格兰地区进行了降雪调查。目前,该地区五个主要流域(康涅狄格州,梅里马克,休萨托尼奇,泰晤士河和黑石镇)的31个项目共有93个雪道。建立这些降雪路线的目的是监视积雪的洪灾潜力。比较佛蒙特州东部,新罕布什尔州西南部和马萨诸塞州中南部的雪道的雪水当量(SWE),并分析其时间趋势。一般来说,每年的最高雪水当量值范围从零到31.7厘米(12.5英寸)。该地区的特点是,一次雪上暴雨可能会使整个雪堆融化,从而在脆弱地区造成洪水泛滥,并危及生命和财产。介绍了每个流域内SWE的特征以及时间趋势的证据。

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