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A satellite-derived climatology of unreported tornadoes in forested regions of northeast Europe

机译:在东北欧洲森林地区未报告龙卷风的卫星衍生的气候学

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AbstractThis study presents a novel method of tornado track identification in forested regions in Europe based on remote sensing data. The method enables an objective estimate (i.e. independent of population density and observational networks) of tornado climatology in forested regions. The method is based on the identification of narrow and elongated areas as forest disturbances obtained using Landsat satellite images and Landsat-based Global Forest Change (GFC) data. These areas were subsequently verified with high-resolution satellite images for verification of a tornadic cause of forest damage. Landsat and MODIS satellite images, weather station observations and reanalysis data were additionally involved in order to determine tornado dates. A minimum F-scale tornado intensity was estimated by a Weibull distribution model using information on tornado path lengths and widths. The method is applied to the forested regions of northeast Europe, where 110 tornado tracks were identified between the 2000 and 2014years, 105 of which were previously unreported and discovered for the first time. For some regions, tornado density estimates using the new method is 2–3 times higher than other previously published estimates. The largest number of tornadoes occurred in 2009, and June is the most favourable month for tornado formation (including strong tornadoes and tornado outbreaks). Most identified tornadoes have path length <10km with maximum and mean widths of approximately 200–300m and 100–200m, respectively. A few tornadoes with long and wide paths were found; four of them likely had F3 minimal intensity.展开▼
机译:<![cdata [ 抽象 本研究提出了一种基于遥感数据欧洲森林地区龙卷风轨道识别的新方法。该方法使得在森林地区龙卷风气候学的客观估计(即独立于人口密度和观察网络)。该方法基于使用Landsat卫星图像和基于Landsat的全球森林变化(GFC)数据获得的森林障碍的窄和细长区域的识别。随后通过高分辨率卫星图像验证了这些区域,以验证森林损伤的霸王原因。还涉及Landsat和Modis卫星图像,气象站观测和再分析数据,以确定Tornado日期。使用龙卷风路径长度和宽度的信息估算了Moibull分布模型的最小F级龙卷风强度。该方法适用于东北欧洲的森林地区,在2000和2014年之间确定了110个龙卷风轨道,其中105个以前首次未报告和发现。对于一些地区,使用新方法的龙卷风密度估计比以前发布的估计高2-3倍。 2009年发生的最多龙卷风,六月是龙卷风形成最有利的月份(包括强烈的龙卷风和龙卷风爆发)。大多数已识别的龙卷风的路径长度<10km,分别为约200-300m和100-200m的最大和平均宽度。发现了一些长而宽阔的路径的龙卷风;其中四个可能具有F3最小强度。

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