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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >A climatological study of the strongest local winds of Japan 'Inami-kaze'
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A climatological study of the strongest local winds of Japan 'Inami-kaze'

机译:日本最强大的当地风的气候研究“Inami-Kaze”

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This study examines the meteorological and climatological features of the Inami-kaze in the Tonami Plain, the strongest local winds in Japan. The plain faces the Sea of Japan on the north side, while the remaining three sides are surrounded by high mountain ranges. An interview survey to local residents and the distribution of windbreak trees both indicate that the Inami-kaze is localized to a surprisingly small region near the Inami town (about 6 km parallel to the mountain ridge and 3 km perpendicular to it), at the base of a very small saddle-like topography in the mountain ridge. Wind statistics with a dense observation network during 2006-2014 (28 Inami-kaze events) supports the above finding. Indeed, the wind speed is mostly (95%) below 11 m/s at the Tonami town, just 5 km away from the Inami town, while the Inami-kaze (>= 15 m/s) blows at the Inami town. Such a spatial pattern should be formed as a result of downslope windstorm with hydraulic jumps, which is indicated from the internal Froude number change across the mountain (0.9 at the upstream, 1.4 at the mountain top, and 0.3 at downstream). The required synoptic atmospheric condition for the Inami-kaze is the pressure pattern "extratropical cyclone in the Sea of Japan." The sufficient condition is the SSW-SSE wind (>= 25 m/s) or south wind (around 20 m/s) at the 800-pressure level over the mountain chain, indicating the allowed directional window is very narrow. On the other hand, the Inami-kaze has an aspect of foehn. While the Inami-kaze occur, the potential temperature at the Inami town tends to be higher by 4.7 K on average than in the windward plain on the Pacific Ocean side.
机译:本研究探讨了日本最强大的当地风中Inami-Kaze的气象和气候特征。平原面对日本的海边,而剩下的三面被高山范围包围。对当地居民的面试调查以及防风树树的分配表明,Inami-Kaze将在Inami镇附近的一个令人惊讶的小区域(与山脊平行6公里,垂直于垂直于它),在基地上在山脊上的一个非常小的马鞍地形。 2006 - 2014年期间,具有密集观察网络的风统计(28 Inami-Kaze事件)支持上述发现。实际上,风速大多(95%)在古马镇距离Inami镇仅有5公里,距离Inami Town仅有5公里,而Inami-Kaze(> = 15米/秒)在Inami镇吹来。这种空间图案应该是由液压跳转的下坡风暴形成的,这从山上的内部Froude数变化表示(在山顶上的上游,1.4处0.9,下游0.3)。 inami-kaze所需的天气大气条件是“日本海域的乌贼旋风”的压力模式。足够的条件是SSW-SSE风(> = 25米/秒)或南风在山链上的800压力水平上的南风(约20米/秒),表示允许的方向窗口非常窄。另一方面,Inami-Kaze具有泡沫的一个方面。虽然发生Inami-Kaze,但Inami Town的潜在温度平均趋于4.7 k,而不是太平洋侧面的迎风平原。

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