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作 者:司鹏[1] 郝立生[1] 罗传军[1] 曹晓岑 梁冬坡[1] Si Peng;Hao Lisheng;Luo Chuanjun;Cao Xiaocen;Liang Dongpo(Tianjin Meteorological Bureau, Tianjin 300074, China)
机构地区:[1]天津市气象局,天津300074
出 处:《气候变化研究进展》2017年第1期41-51,共11页Climate Change Research
基 金:公益性行业(气象)科研专项(重大专项)(GYHY201506001-1)
摘 要:基于多源的气温月值资料,在数据整合和初步质量控制基础上,同时采用标准化序列法和多元线性回归法对河北保定气象站1913—2014年月平均气温、最高气温和最低气温资料进行了插补。通过交叉检验法分析发现,标准化序列法插补得到的气温序列效果较好,并且气候统计特征与同区域周边站的研究结果更具一致性。利用惩罚最大F检验(PMF)对插补后序列的均一性进行了检验,结果表明:通过插补得到的保定站百年气温月值序列的均一性相对较好,仅月平均最低气温序列存在2个显著间断点,分别由同类型仪器的更换和台站迁移导致,研究中采用分位数匹配(QM)对其进行了订正,建立了保定站百年气温月值序列。通过与邻近单站及我国中东部区域均一化百年气温序列的综合对比显示,本文建立的保定站百年气温月值序列与邻近单站的相关性基本达到0.8以上;从增暖趋势来看,保定站与中东部区域平均序列分别达0.121℃/10a、0.204℃/10a,基本在同一量级内:这一定程度上说明建立的保定站百年气温序列相对合理。Using multi-source of monthly temperature data on the basis of preliminary integration and quality control, monthly mean temperature, maximum temperature, and minimum temperature time series covering 1913-2014 at Baoding station in Hebei province were interpolated by both two approaches of standardized method and multivariate linear regression. The interpolation results were analyzed by cross validation. The standardized method is more suitable for temperature data at Baoding, and the climate statistics characteristics from that are more consistent with those from surrounding stations in the same area. So the interpolated time series were homogenized by the penalized maximal F test (PMF), and results indicate that those monthly hundredyear temperature data are relatively continuous, only two breakpoints have been detected in mean minimum temperature series, which are caused by instrument replacement and station relocation, respectively, and then adjusted by Quantile-Matching (QM). Accordingly, the monthly hundred-year temperature time series at Baoding station were constructed. Moreover, the time series here were compared with the others at Beijing and Tianjin, and regional series in eastern and central China from some aspects of trend change and correlation analysis. The results show that the correlation coefficients of monthly mean temperature between Baoding and adjacent single station almost reached more than 0.8, and the warming amplitude of trends for annual mean hundred-year temperatureat Baoding and regional series in eastern and central China were nearly in the same order of magnitude, with 0.121 ℃ /10a and 0.204 ℃ /10a, respectively. Therefore, the data we have developed in this paper are relatively logical and errorless, to a certain extent.
分 类 号:P416[天文地球—大气科学及气象学]
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