| 由最高最低气温求算的平均气温对我国年平均气温序列影响 |
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| 引用本文： | 唐国利,丁一汇.由最高最低气温求算的平均气温对我国年平均气温序列影响[J].应用气象学报,2007,18(2):187-192. |
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| 作者姓名： | 唐国利 丁一汇 |
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| 作者单位： | 1.国家气候中心 中国气象局气候研究开放实验室, 北京 100081 |
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| 基金项目： | 国家科技攻关计划;中国气象局科研项目 |
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| 摘 要： | 针对研究全国近百年平均气温长期变化的实际需要，利用603个测站1961—2002年气温观测资料，比较分析了最高最低平均气温距平序列和4次观测记录平均气温距平序列的差异，讨论了最高、最低气温变化趋势。结果表明:两种统计方法得到的平均气温距平序列及增温速率的差异均不明显，在一定条件下两者可以互相替换。此外，最高、最低气温变化普遍存在不对称现象，且可分为4种类型，这种不对称性对平均气温变化速率并没有明确一致的影响。
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| 关 键 词： | 气温序列 最高最低气温 平均气温求算方法 |
| 收稿时间： | 2005-11-11 |
| 修稿时间： | 2006-07-14 |
Impacts of the Average Air Temperature Derived from Maximum and Minimum Temperatures on Annual Mean Air Temperatures Series of China |
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| Tang Guoli,Ding Yihui.Impacts of the Average Air Temperature Derived from Maximum and Minimum Temperatures on Annual Mean Air Temperatures Series of China[J].Quarterly Journal of Applied Meteorology,2007,18(2):187-192. |
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| Authors: | Tang Guoli Ding Yihui |
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| Affiliation: | 1.Laboratory for Climate Studies, National Climate Center, CMA, Beijing 1000812.Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 1000293.Graduate University, Chinese Academy of Sciences, Beijing 100039 |
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| Abstract: | The global warming is one of the focuses to which greatly attention are paid by scholars, officials and the public in the world. And the global or regional surface air temperature changing trend is a key issue in the climate change detection and research. The mean temperature data which are derived from the 4 time observations per day are generally adopted in the research on climate change in China. But for the purpose of studying the long term mean air temperatures in the last 100 years in China, because the observation time is different and complicated, the observation time systems are not unified and the statistical methods for the mean temperature are inconsistent, severe inhomogeneity exists in the monthly mean temperature data before 1950. As a result, the inhomogeneity of the data brings down the reliability of the surface air temperature series, thus has influences on both the connection of air temperature series of different periods and the estimate of the long term temperature change trend. Especially it will severely affect the quality of China's last 100 year air temperature series. A feasible way to overcome this problem is to re calculate the mean temperature based on the average of maximum and minimum temperatures and form China's surface air temperature series and the estimation of warming extent from it. Its advantage is highly obvious. Using this method, the cause of the above mentioned inhomogeneity can be eliminated and the relevant error with it can also be avoided. Accordingly, the homogeneity and quality of China's surface air temperature series can be improved greatly. However, it will bring some questions as follows: Do the differences (or obvious differences) between the results (including the mean air temperature and its anomaly series of regional average) derived from the two different statistical methods exist? And the maximum and the minimum air temperature changes have obvious dissymmetry phenomena, which have been found in previous researches. Do the dissymmetrical changes affect new mean air temperature series and the accuracy of the estimate of the air temperature change rate over China? To answer these questions, and satisfy the practical need in researches on the long term surface air temperature change in the last 100 years in China, using air temperature data of 603 stations during 1961—2002, the differences between the two kinds of mean air temperature anomaly series, averaged from the maximum and the minimum temperatures and the 4 time observations respectively, are compared and examined, also, the maximum and the minimum temperature change trends are discussed for researching their impacts on the long term annual mean air temperature series over China. The results show that there are no remarkable differences between the two kinds of mean temperature anomaly series obtained separately by means of different approaches and between their temperature change rates. They can be replaced by each other under certain conditions. In addition, the dissymmetrical phenomena of the maximum and the minimum air temperature changes are ubiquitous in China. And they may be classified into four types according to the features of the temperature changes. However, the impacts of dissymmetry on the mean air temperature change rates are uncertain. |
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| Keywords: | air temperature series maximum and minimum temperatures calculations of mean air temperature |
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