Combined analysis of early pressure observation data and historical daily weather documents for winter climate reconstruction in Japan

J. Hirano, Tekahiko Mikami, M. Zaiki
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Abstract

Abstract. The East Asian winter monsoon is characterized by a strong east–west surface pressure gradient and the outbreak of cold air around Japan. It causes heavy snowfall in the Sea of Japan side of the Japanese Islands. Meanwhile, fine weather prevails over the Pacific Ocean side owing to topographical effects. Documents pertaining to daily weather in Japan often provide useful weather information regarding the appearance of typical “winter-monsoon-type weather patterns” in the historical period. In addition to historical daily weather documents, we recovered several early pressure observation series in Japan and China from the 19th century. A combined analysis of historical daily weather documents and early surface pressure observation may result in an effective detection of outbreaks arising from the East Asian winter monsoon in the historical period. Knowledge regarding atmospheric circulation fields associated with “winter-monsoon-type weather patterns” is essential for this combined analysis. We first investigate temporal evolutions of circulation fields associated with “winter-monsoon-type weather patterns” for the present day (1968–1980). The result indicates that the southward expansion of the Siberian High and eastward movement of extratropical cyclones around Japan result in a significant east–west surface pressure gradient in East Asia. This pressure gradient causes “winter-monsoon-type weather patterns” in Japan. Subsequently, we attempted to reconstruct the outbreak of the winter monsoon around Japan for the winter of 1851/52 using both historical weather documents and newly recovered early instrumental pressure data of Japan and China. The reconstructed results show that the outbreak of the East Asian winter monsoon can be reasonably detected by focusing on the sequence of reconstructed daily weather patterns and the east–west pressure gradient calculated using early instrumental pressure data.
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日本冬季气候重建早期气压观测资料与历史日气象资料的结合分析
摘要东亚冬季风以强烈的东西向地面气压梯度和日本周围冷空气的爆发为特征。它在日本群岛的日本海一侧造成了大雪。同时,受地形影响,太平洋一侧天气晴朗。有关日本日常天气的文件通常提供有关历史时期典型的“冬季-季风型天气模式”出现的有用天气信息。除了历史的每日天气资料外,我们还恢复了19世纪以来日本和中国的几个早期气压观测序列。将历史日气象资料与早期地面气压观测相结合,可以有效地发现东亚冬季风在历史时期的爆发。关于与“冬季-季风型天气模式”相关的大气环流场的知识对于这一综合分析至关重要。我们首先研究了当今(1968-1980)与“冬季-季风型天气模式”相关的环流场的时间演变。结果表明,西伯利亚高压南下扩张和日本周边温带气旋东移导致东亚地区出现明显的东西向地面气压梯度。这种气压梯度导致了日本的“冬季季风型天气模式”。随后,我们利用历史气象资料和新恢复的日本和中国的早期仪器压力资料,试图重建1851/52年冬季日本周围冬季季风的爆发。重建结果表明,通过逐日天气模式的重建序列和利用早期仪器气压资料计算的东西压力梯度,可以合理地探测东亚冬季风的爆发。
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