Analyzing the Fluctuations of Atmospheric Precipitable Water in Iran During Various Periods Based on the Retrieving Technique of NCEP/NCAR

I. Rousta, Mehdi Doostkamian, H. Ólafsson, Hao Zhang, Sayed Hossein Vahedinejad, Omar Sarif, E. Vargas
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引用次数: 3

Abstract

The current study has compared the fluctuations of atmospheric precipitable water over Iran during three periods of 1948 – 1957, 1958 – 1978, and 1979 – 2012 using upper-air reanalyzed data from NCEP/NCAR. The results indicated that, in all the three periods, average distribution and coefficient of spatial variation decreased with altitude. In contrast, there was a positive relationship between coefficient of spatial variation and altitude. The results of trend analysis showed that atmospheric precipitable water of Iran calculated using the upper-air reanalyzed data by NCEP/NCAR experienced various fluctuations during the three periods of 1948 – 1957, 1958 – 1978, and 1979 – 2012. The increase of the precipitable water during the first period was not significant at the level of 95%. The increase of the precipitable water during the second period was significant at the level of 95% just in 25% of the regions. In contrast to the second period, 70% of the country’s area followed a declining trend. However, this decreasing trend was not significant at the level of 95%, either. The results of Alexandersson statistical method showed that the biggest shift in the average of precipitable water happened during the third period. Overall, variations in the precipitable water over Iran in the past ~60 years are not within the uncertainty of the reanalysis data and are therefore clearly discernible.
基于NCEP/NCAR反演技术的伊朗不同时期大气可降水量波动分析
目前的研究利用NCEP/NCAR的高空再分析数据,比较了1948 - 1957年、1958 - 1978年和1979 - 2012年三个时期伊朗大气可降水量的波动。结果表明,3个时期的平均分布和空间变异系数均随海拔高度的增加而减小。空间变异系数与海拔高度呈正相关。趋势分析结果表明,利用NCEP/NCAR高空再分析资料计算的伊朗大气可降水量在1948—1957年、1958—1978年和1979—2012年三个时期经历了不同程度的波动。第一期可降水量的增加在95%的水平上不显著。第二期可降水量增加显著,仅在25%的地区达到95%的水平。与第二阶段相比,该国70%的地区呈下降趋势。但在95%水平上,这种下降趋势也不显著。Alexandersson统计结果表明,第3期降水量变化最大。总体而言,伊朗过去~60年的可降水量变化不在再分析数据的不确定性范围内,因此可以清楚地识别。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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