主办单位：中国气象局沈阳大气环境研究所
国际刊号：ISSN 1673-503X
国内刊号：CN 21-1531/P
气象与环境学报

气象与环境学报 ›› 2013, Vol. 29 ›› Issue (5): 74-80.doi:

• 论　文 • 上一篇    下一篇

基于昼夜温差序列非均一性的高空温度订正

吴慧1,2  翟盘茂2  林建兴3   

  1. 1. 海南省气候中心，海南 海口 570203；2.中国气象科学研究院灾害天气国家重点实验室，北京 100081；  3.海南省气象台，海南 海口 570203
  • 出版日期:2013-10-31 发布日期:2013-10-31

Adjustment of upper air temperature based on inhomogeneity of day-night temperature difference series

WU Hui 1,2   ZHAI Pan-mao 2   LIN Jian-xing 3   

  1. 1.Hainan Climate Center, Haikou 570203, China; 2. State Key Laboratory of Severe Weather, Chinese Academy of Meteorological Sciences, Chinese Meteorological Administration, Beijing 100081, China; 3. Hainan Meteorological Observatory, Haikou 570203, China
  • Online:2013-10-31 Published:2013-10-31

PDF (PC)

450

被引次数

2

摘要： 利用中国东部地区75个高空探测站1958－2005年逐日08：00和20：00资料和元数据信息，采用昼夜温度对比和二相线性回归方法，对不同等压面的温度序列进行均一性检测和订正。在此基础上，以最大缺测率30 %作为序列取舍标准，对49个探空站订正前后的年平均温度变化趋势进行了对比分析。结果表明：探空仪器变化和辐射订正方法改变是造成中国东部地区高空温度序列非均一性的主要原因，1966年前后和2000年前后是两个较为可靠的间断点，且1966年前后的非均一性更突出。非均一性最明显的等压面主要在100 hPa。1958－2005年，500 hPa以下等压面温度的上升趋势较订正前减弱，但200 hPa到50 hPa等压面温度的下降趋势也被削弱，削弱幅度为0.04－0.08 ℃/10 a。与1958－2005年相比，1979年以来东部地区对流层各层温度增温趋势明显，而平流层底层降温趋势也更加显著，该时段内订正前后温度变化趋势差异较小。

关键词: 高空温度, 均一化订正, 昼夜温差, 二相线性回归

Abstract: Based on the daily temperature data from 75 radiosonde stations in the eastern China at 08:00 and 20:00 during 1958 to 2005 and the corresponding metadata, homogeneity of temperature at different levels was tested and adjusted using  methods of a temperature difference between daytime and nighttime and a two-phase linear regression. The annual trends of the observed and revised temperature at 49 stations were analyzed by selecting data using 30 % maximum missing rate as a standard. The results indicate that inhomogeneity of temperature is caused by changes of radiosonde instrument and radiation correction method in upper level over the eastern China. The credible breakpoints for inhomogeneity occur in 1966 and 2000, especially in 1996. The most obvious inhomogeneity appears at 100 hPa. Compared with the original temperature series, warming trend of temperature below 500 hPa weakens from 1958 to 2005, so is its decreasing trend from 200 hPa to 50 hPa and the ratio is 0.04-0.08 ℃ every decade. Troposphere temperature increases and lower stratosphere temperature decreases significantly since 1979. Therefore, temperature discrepancy of adjusted and original time series during 1958 to 2005 is small compared with that during 1958 to 2005.

Key words: Upper air temperature, Inhomogeneous adjustment, Day-night temperature difference, Two-phase linear regression