Relationship between large amounts of Cryptomeria japonica D. Don pollen dispersion and cold front passage

Yuichi Takahashi, S. Kawashima, Yusuke Suzuki, S. Kakehata
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Abstract

Recently, with the proliferation of automatic Cryptomeria japonica pollen monitors, it has become possible to obtain data measured simultaneously from multiple locations. The KH-3000 monitor used by the Pollen Observation System of the Japanese Ministry of the Environment, “Hanako-san”, and the “Pollen Robo” monitor created by Weathernews Inc. were installed in various places in the Tohoku region for collection of simultaneous pollen count data, and the results indicated that the period of the day when large amounts of C. japonica pollen were dispersed may be related to the passage of a cold front extending from a low pressure system. When the types of pollen dispersed on that day were examined under a microscope, most of them were C. japonica pollen. Therefore, we investigated the relationship between the periods of these two events, with transit time of the cold front determined from the point when the wind direction changed from eastward to westward. The area with a high concentration of C. japonica pollen moved from the Sea of Japan side to the Pacific Ocean side in conjunction with the movement of the front. In 40% of the cases, the highest dispersion of C. japonica pollen occurred at the same time as the front passed, and 90% of the cases were within two hours before or after the passage. The number of dispersions was high in the northern part of the Tohoku region close to the low pressure system at the end of the front and low in the southernmost part of the Tohoku region away from this system.
柳杉花粉大量弥散与冷锋通道的关系
近年来,随着日本柳杉(Cryptomeria japonica)花粉自动监测仪的普及,从多个地点同时获得测量数据已成为可能。日本环境省花粉观测系统“Hanako-san”使用的KH-3000监测仪和Weathernews公司研制的“花粉机器人”监测仪在东北地区多处安装,同时采集花粉数量数据,结果表明,一天中大量粳稻花粉分散的时段可能与低压系统延伸的冷锋通过有关。在显微镜下观察当天散布的花粉种类,大部分为粳稻花粉。因此,我们研究了这两个事件的周期关系,冷锋的过境时间从风向由东向西转变的点开始确定。随着锋面的移动,花粉密集区从日本海一侧向太平洋一侧移动。40%的病例花粉散布高峰发生在锋线通过的同时,90%的病例发生在锋线通过前后2小时内。在锋面末端靠近低压系统的东北地区北部弥散数量较多,而在远离低压系统的东北地区最南端弥散数量较少。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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