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Phenological data series of cherry tree flowering in Kyoto, Japan, and its application to reconstruction of springtime temperatures since the 9th century

机译:日本京都樱花开花的物候数据系列及其在重建9世纪以来的春季温度中的应用

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Changes in springtime temperature in Kyoto, Japan, since the 9th century were reconstructed, using the phenological data series for cherry tree (Prunus jamasakura), deduced from old diaries and chronicles. Phenological data for 732 years was made available by combining data from previous studies. The full-flowering date of cherry trees fluctuates in accordance with temperature conditions during February and March. Full-flowering dates were closely related to the March mean temperature by means of a temperature accumulation index, in which plant growth is considered to be an exponential function of temperature. Calibration enabled accurate estimation of temperatures in the instrumental period, after 1880; the root mean square error (RMSE) of temperature estimates was determined to be within 0.1 degrees C, after smoothing by local linear regression over time spans of 31 years. The results suggested the existence of four cold periods, 1330-1350, 1520-1550, 1670-1700, and 1825-1830, during which periods the estimated March mean temperature was 4-5 degrees C, about 3-4 degrees C lower than the present normal temperature. These cold periods coincided with the less extreme periods, known as the Wolf, Spoerer, Maunder, and Dalton minima, in the long-term solar variation cycle, which has a periodicity of 150-250 years. The sunspot cycle length, a short-term solar variation cycle, was also compared with the temperature estimates, with the result that a time lag of about 15 years was detected in the climatic temperature response to short-term solar variation. Copyright (C) 2007 Royal Meteorological Society.
机译:利用从旧日记和纪事中推导出的樱桃树(Prunus jamasakura)物候数据系列,重建了自9世纪以来日本京都的春季温度变化。通过合并先前研究的数据,可以获得732年的物候数据。樱桃树的盛花期根据2月和3月的温度条件而波动。通过温度累积指数,盛开的日期与三月平均温度密切相关,在该指数中,植物的生长被认为是温度的指数函数。通过校准,可以精确估算1880年后仪器使用期间的温度;在31年的时间跨度内通过局部线性回归平滑后,温度估算的均方根误差(RMSE)被确定在0.1摄氏度以内。结果表明存在四个寒冷时期,即1330-1350、1520-1550、1670-1700和1825-1830,在此期间,估计的三月平均温度为4-5摄氏度,比3月低3-4摄氏度。当前的正常温度。这些寒冷时期与长期的太阳变化周期(周期为150-250年)中的极端极端时期(称为Wolf,Spoerer,Maunder和Dalton极小时期)相吻合。太阳黑子的周期长度,即短期的太阳变化周期,也与温度估计值进行了比较,结果是在对短期太阳变化的气候温度响应中检测到约15年的时间滞后。皇家气象学会(C)2007。

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