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首页> 外文期刊>農業気象 >Climatological characteristics of basin fog at the Ohzu Basin, Ehime prefecture
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Climatological characteristics of basin fog at the Ohzu Basin, Ehime prefecture

机译:爱媛县大津盆地盆雾的气候特征

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The Ohzu Basin is located in the north western part of Shikoku Island as is shown in Fig. I. As in other basins in Japan, basin fog appears frequently from autumn to winter. In order to make clear the climatological characteristics of basin fog at the Ohzu Basin, Ehime prefecture, and understand its role as an element of agro-climatological resources, observations were carried out from Sep. 8, 1995 to Feb. 5, 1996. The sites were located at bottom of the basin and on mountainside faced to the center of the basin. The latter site was situated above the upper surface of the fog layer which appears typically in the Ohzu Basin. Spatial distribution of the fog were also analyzed using the LANDSAT images provided on Dec. 5, 1985 and Dec. 13, 1988. The results obtained in this study were summarized as follows: (1) The total number of fog day reached 46 days during the present observation period mentioned above. In the most frequent period, fog occurred at the ratio of one day to two day in October and November. (2) Dispersion time of the fog changed seasonally accordance with a shift of time of sunrise, and the fog has lasted 4 hours or more after the sunrise under dominant foggy conditions. (3) The meteorological characteristics of foggy day were shown as follow, attenuated of solar radiation in the morning, decreased of radiative cooling in nighttime, and low temperature until fog dissipate. (4) Several percent of monthly total solar radiation was shaded by fog layer at the basin bottom site. Total time of saturation condition indicated by R.H.= 100 percent on foggy days became 21 hours at the site of mountain slope. At the basin bottom site, it reached 493 hours during the period of the observation. (5) Upper surface of the fog layer was limited to a height about 300 m above the sea level, and distributed horizontally along lower part of the Hiji River. The maximum height was affected by the surrounding topography. (6) In the Ohzu Basin, hamlets on the mountain slope distributed zonally above the fog layer. This indicates that the fog has a remarkable influence on human life of mountainous region. On the other hand, the chinese cabbage-producing district was formed in the foggy area. Utilizing this foggy climate of the basin, high quality chinese cabbage with soft leave are produced in the basin bottom.
机译:如图1所示,大津盆地位于四国岛的西北部。与日本其他盆地一样,从秋天到冬天,盆地雾频繁出现。为了弄清爱媛县大津盆地盆雾的气候特征,并了解其作为农业气候资源的作用,于1995年9月8日至1996年2月5日进行了观测。遗址位于盆地底部,面向盆地中心的山腰。后者位于雾层上表面的上方,雾层通常出现在Ohzu盆地中。还使用1985年12月5日和1988年12月13日提供的LANDSAT图像分析了雾的空间分布。本研究获得的结果归纳如下:(1)雾日总数达到46天。目前上述观察期。在最频繁的时期,10月和11月的雾发生率为一天到两天。 (2)雾的扩散时间随日出时间的变化而季节性变化,在主要的有雾条件下,雾在日出后持续了4小时以上。 (3)大雾天的气象特征如下:早晨太阳辐射减弱,夜间辐射降温减少,直至雾消散的温度较低。 (4)流域底部的雾层遮挡了每月总太阳辐射的百分之几。在雾天,R.H。= 100%表示的饱和状态总时间在山坡处变为21小时。在盆地底部,观测期间达到了493小时。 (5)雾层的上表面被限制在海平面以上300 m的高度,并沿比治河的下部水平分布。最大高度受周围地形影响。 (6)在大津盆地,山坡上的小村庄分布在雾层上方。这表明雾对山区人的生活有重大影响。另一方面,在大雾地区形成了大白菜产区。利用盆地的多雾气候,在盆地底部产生了带有软叶的优质大白菜。

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