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Seasonal/Regional Variation of Variability Characteristic of Daily Maximum/Minimum Temperatures in Japan Observed and Reproduced by RegCM Nested in NCAR-CSM

机译:NCAR-CSM中嵌套的RegCM观测和复制的日本每日最高/最低温度的变化特征的季节性/区域变化

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摘要

Observation data and output of a regional climate model, RegCM2.5, nested in a global climate model, NCAR-CSM, were analyzed to determine the standard deviation and frequency of extreme values, which were used as indices to characterize the variability of the daily minimum (Tmin) and maximum (Tmax) temperatures in Japan. The frequency of extreme values, which are defined in this paper as deviations greater than twofold the standard deviation, was estimated from data using a new method. The significant results of this analysis of observation data are as follows. With regards to both Tmin andTmax, the significant seasonal variations of standard deviation are the annual and semiannual ones, with the minimum value in August and a weak minimum in January. The region where the standard deviation is large drifts northward from February to May, with a maximum standard deviation in Apri1. The central latitude almost agrees with that where the zonal wind is maximum at 500 hPa. As compared with the normal distribution, the extremely high temperature in summer, and the extremely low temperature in winter, are observed less frequently. The indices calculated from the model's output after simulating the current climatic condition were compared with the observation data for evaluation. From this comparison, it is shown that the variability characteristic of Tmax was not reproduced well; however, that of Tmin was reproduced well by the model. Therefore, it is concluded that Tmin. reproduced by RegCM/CSM can be used to predict the change in the frequency of extreme values by correcting the systematic temperature bias, which is within ±1 K.
机译:对嵌套在全球气候模型NCAR-CSM中的区域气候模型RegCM2.5的观测数据和输出进行分析,以确定标准偏差和极值出现的频率,将其用作表征每日变化的指标日本的最低(Tmin)和最高(Tmax)温度。使用新方法从数据中估计出极端值的频率,在本文中将其定义为偏差大于标准偏差的两倍。观察数据分析的重要结果如下。关于Tmin和Tmax,标准偏差的显着季节性变化是年度和半年度变化,其最小值在8月,而在1月则较小。标准偏差较大的区域从2月到5月向北漂移,最大标准偏差为Apri1。中心纬度几乎与纬向风在500 hPa处最大的情况一致。与正态分布相比,夏季出现的极端高温和冬季出现的极端低温的频率降低。将模拟当前气候条件后从模型输出中计算出的指标与观测数据进行比较,以进行评估。从该比较可知,不能很好地再现Tmax的变异性。但是,该模型很好地再现了Tmin的值。因此,可以得出Tmin。 RegCM / CSM复制的数据可用于通过校正系统温度偏差(在±1 K以内)来预测极值频率的变化。

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