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基于均一化观测序列的京津冀地区气候变化格局分析
引用本文:窦以文,丹利,严中伟,李珍,胡保昆,史君卿.基于均一化观测序列的京津冀地区气候变化格局分析[J].气候与环境研究,2018,23(5):524-532.
作者姓名:窦以文  丹利  严中伟  李珍  胡保昆  史君卿
作者单位:1.北京市气象信息中心, 北京 1000892.中国科学院大气物理研究所中国科学院东亚区域气候-环境重点实验室, 北京 1000293.北京农业职业学院, 北京 100093
基金项目:国家重点研发计划项目2016YFA0602501,国家自然科学基金项目41630532,北京市气象局科技项目BMBKJ201401004
摘    要:利用1960~2015年京津冀地区88个国家级气象站观测资料(包括日平均气温、日最高气温、日最低气温、日降水、日平均风速等),使用MASH(Multiple Analysis of Series for Homogenization)方法剔除台站迁址、仪器变更等因素所致偏差后,生成均一化的观测资料集。基于新资料集计算了各站气温、降水和凤速序列的线性趋势和Morlet小波等统计特征,分析了京津冀地区气候变化格局。结果表明:MASH方法能较准确地检测并校订观测序列中迁站、仪器变更等因素所导致的非均一性;1960~2015年期间京津冀年平均气温显著上升,上升幅度为0.261℃/10 a;降水减少,平均减少11.27 mm/10 a;风速显著减小,平均减小0.193 m s-1(10 a)-1。

关 键 词:均一化    气温    降水    风速
收稿时间:2017/3/29 0:00:00

Analysis of Climate Change in Beijing-Tianjin-Hebei Region Based on Homogenized Observations
DOU Yiwen,DAN Li,YAN Zhongwei,LI Zhen,HU Baokun and SHI Junqing.Analysis of Climate Change in Beijing-Tianjin-Hebei Region Based on Homogenized Observations[J].Climatic and Environmental Research,2018,23(5):524-532.
Authors:DOU Yiwen  DAN Li  YAN Zhongwei  LI Zhen  HU Baokun and SHI Junqing
Institution:1.Beijing Meteorological Information Centre, Beijing 1000892.Key Laboratory of Regional Climate-Environment Research for Temperate East Asia, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 1000293.Beijing Vocational College of Agriculture, Beijing 100093
Abstract:Based on MASH-generated homogenized observation series of daily mean, maximum, and minimum temperatures and daily precipitation and wind speed from 88 national meteorological stations in Beijing-Tianjin-Hebei region (BTH) during 1960-2015, we calculate the linear trends and Morlet wavelets of the time series at each station to analyze the climate change in BTH. The results suggest that the MASH method can detect and adjust discontinuities in association with changes in the locations of stations, observation instruments and surrounding environs. The annual mean temperature over the region on average has risen by 0.26℃/10 a, precipitation has decreased by 11.3 mm/10 a, and wind speed has decreased by 0.19 m s-1(10 a)-1.
Keywords:Homogenization  Surface air temperature  Precipitation  Wind speed
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