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首页> 外文期刊>Weather and forecasting >Synoptic and mesoscale analysis of a high-latitude Derecho-severe thunderstorm outbreak in Finland on 5 July 2002
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Synoptic and mesoscale analysis of a high-latitude Derecho-severe thunderstorm outbreak in Finland on 5 July 2002

机译:2002年7月5日芬兰高纬度Derecho-严重雷暴暴发的天气和中尺度分析

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On 5 July 2002, a rapidly propagating bow echo formed over eastern Finland causing severe wind damage in an exceptionally large area. The Ministry of the Interior's Emergency Response Centers received nearly 400 thunderstorm-related wind damage reports. The 5 July 2002 case is the highest-latitude derecho that has ever been documented. The bow echo developed ahead of a northeastward-moving 500-hPa trough inside of the warm sector of a secondary low and moved north-northwestward on the eastern (warm) side of the quasi-stationary front. The leading edge of the bow echo was oriented perpendicular to the low-level southerly wind shear and the convective system propagated along the 850-hPa equivalent potential temperature ridge with a speed that was close to the maximum wind throughout the troposphere. It is particularly noteworthy that the synoptic pattern was oriented about 90 counterclockwise when compared with the typical synoptic pattern associated with warm season derechos in the United States. This kind of synoptic situation associated along with the derecho mesoscale convective system's (MCS's) motion toward the north-northwest has not been mentioned in literature before. The MCS started as a cluster of thunderstorms and became a bow echo a few hours later. The leading edge of the bow echo had a strong reflectivity gradient and the region of stratiform precipitation was behind the strongest echoes. At the most intense stage, a rear-inflow notch was visible both in radar and satellite pictures. It was in good accordance with the location of an area of the most severe damage. Moreover, the storm-relative winds derived from the proximity sounding in the wake of the system showed the existence of rear-to-front flow above 850 hPa. The downdraft air appeared to originate from 4 km ASL, where the relative humidity was less than 50%. This probably led to enhanced evaporative cooling and the intense cold pool, which propagated faster than the mean wind. In the mesoscale, the 5 July 2002 derecho had many similarities to other derecho MCSs that have been described in the literature.
机译:2002年7月5日,在芬兰东部形成了迅速传播的弓形回波,在很大的面积上造成了严重的风害。内政部的应急中心收到了近400起与雷暴有关的风灾报告。 2002年7月5日的案件是有史以来记录的最高纬度回波。弓形回波在次低带暖区内向东北移动的500hPa槽的前方发展,并在准静止锋的东部(暖)侧向西北偏北移动。船首回波的前缘垂直于低水平的南风切变,对流系统沿850hPa等效势温脊传播,其速度接近整个对流层的最大风速。特别值得注意的是,与美国暖季退潮相关的典型天气模式相比,天气模式逆时针方向约90度。以前没有文献提到这种天气情况,与地雷中尺度对流系统(MCS)向西北偏北运动有关。 MCS开始时是雷阵雨,数小时后变成弓形回声。弓形回波的前缘具有很强的反射率梯度,并且层状降水区域位于最强回波的后面。在最激烈的阶段,雷达和卫星图片中都可以看到一个后入缺口。它与损坏最严重的区域的位置完全吻合。此外,从系统唤醒后的近距离测深得出的相对风暴风表明,在850 hPa以上存在从前到后的流量。向下的空气似乎来自4 km ASL,那里的相对湿度小于50%。这可能导致蒸发冷却的增强和强烈的冷池,其传播速度快于平均风。在中尺度上,2002年7月5日的derecho与文献中描述的其他derecho MCS有很多相似之处。

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