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Meteorological observations collected during the Storms and Precipitation Across the continental Divide Experiment (SPADE), April–June 2019

机译:在2019年4月 - 2019年4月的风暴和沉淀过程中收集的气象观察

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The continental divide along the spine of the Canadian Rockies in southwestern Canada is a critical headwater region for hydrological drainages to the Pacific, Arctic, and Atlantic oceans. Major flooding events are typically attributed to heavy precipitation on its eastern side due to upslope (easterly) flows. Precipitation can also occur on the western side of the divide when moisture originating from the Pacific Ocean encounters the west-facing slopes of the Canadian Rockies. Often, storms propagating across the divide result in significant precipitation on both sides. Meteorological data over this critical region are sparse, with few stations located at high elevations. Given the importance of all these types of events, the Storms and Precipitation Across the continental Divide Experiment (SPADE) was initiated to enhance our knowledge of the atmospheric processes leading to storms and precipitation on either side of the continental divide. This was accomplished by installing specialized meteorological instrumentation on both sides of the continental divide and carrying out manual observations during an intensive field campaign from 24?April–26?June 2019. On the eastern side, there were two field sites: (i)?at Fortress Mountain Powerline (2076?m?a.s.l.) and (ii)?at Fortress Junction Service, located in a high-elevation valley (1580?m?a.s.l.). On the western side, Nipika Mountain Resort, also located in a valley (1087?m?a.s.l.), was chosen as a field site. Various meteorological instruments were deployed including two Doppler light detection and ranging instruments (lidars), three vertically pointing micro rain radars, and three optical disdrometers. The three main sites were nearly identically instrumented, and observers were on site at Fortress Mountain Powerline and Nipika Mountain Resort during precipitation events to take manual observations of precipitation type and microphotographs of solid particles. The objective of the field campaign was to gather high-temporal-frequency meteorological data and to compare the different conditions on either side of the divide to study the precipitation processes that can lead to catastrophic flooding in the region. Details on field sites, instrumentation used, and collection methods are discussed. Data from the study are publicly accessible from the Federated Research Data Repository at https://doi.org/10.20383/101.0221 (Thériault et al., 2020). This dataset will be used to study atmospheric conditions associated with precipitation events documented simultaneously on either side of a continental divide. This paper also provides a sample of the data gathered during a precipitation event.
机译:沿着加拿大西南部的加拿大罗基斯脊柱的大陆划分是太平洋,北极和大西洋水文排水的关键地图。由于上坡(东方)流动,主要洪水事件通常归因于其东部的大量降水。当源自太平洋的水分遇到加拿大罗基斯的西方斜坡时,沉淀也可能发生沉淀。通常,在分裂中传播的风暴导致两侧的显着降水。这个关键区域上的气象数据稀疏,几个电台位于高海拔。鉴于所有这些类型的事件的重要性,启动了整个大陆鸿沟实验(SPade)的风暴和降水,以提高我们对大陆鸿沟两侧的大气流程的知识。这是通过在大陆鸿沟的两侧安装专门的气象仪表来实现,并在24岁以下的野外活动期间进行手动观察?2019年6月。在东侧,有两个现场网站:(i)?在堡垒山力电力线(2076?M?asl)和(ii)?在堡垒交界处,位于高海拔山谷(1580?m?Asl)。在西侧,Nipika Mountain Resort,也位于山谷(1087?M?A.S.L。),被选为现场。部署了各种气象仪器,包括两个多普勒光检测和测距仪器(LIDARS),三个垂直指向微雨雷达和三种光学分数仪。这三个主要网站几乎相同仪表,观察员在堡垒山上电力线和Nipika Mountain Resort的现场,在降水事件中,采用手动观察沉淀型和固体颗粒的显微镜摄影。现场运动的目的是收集高时频率的气象数据,并比较分裂两侧的不同条件,以研究可能导致该地区灾难性洪水的降水过程。讨论了关于现场网站,所使用的仪器和收集方法的详细信息。来自该研究的数据可从HTTPS://Doi.org/10.20383/101.0221(Thériault等,2020)的联邦研究数据存储库公开访问。该数据集将用于研究与大陆鸿沟两侧同时记录的降水事件相关的大气条件。本文还提供了在降水事件期间收集的数据样本。

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