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Attribution of temperature and precipitation changes to greenhouse gases in northwest Iran

机译:温度和降水变化对伊朗西北部温室气体的影响

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摘要

Increase of the greenhouse gases has a considerable effect on climatic variables changes such as temperature and precipitation. Three-dimensional models of coupled ocean-atmosphere general circulation, AOGCMs, under all emissions scenarios, are able to simulate past and future climate periods. The present study investigates the possible attribution of climate change to the increase of the greenhouse gases in northwest Iran. Interannual variability range for the long-term (1000 years) of temperature and precipitation, resulting from control run (greenhouse gas constant) CGCM3 model used for the study area in northwest Iran. Then, the range of natural climate variables was determined from two-dimensional graphs of temperature and precipitation based on two-variant normal distribution. Ultimately, the detected trends of climate variables can be compared with the natural climate variability range of the region. The results showed that in different parts of the study area, the range of natural climate variables for temperature and precipitation changes (95% probability) in the west of the study area are less than 1.8 C~° and 40%, respectively. These values are less than 4 C~° and 40% respectively, in the east of the study area. However, the climate variables in the most regions of the west are almost outside the range of natural climate variables in the recent years (1998-2008). The result indicates the effect of climate changes on the climatic variables for the case study in recent years.
机译:温室气体的增加对气候变量的变化(例如温度和降水)有相当大的影响。在所有排放情景下,耦合的海洋-大气总环流,AOGCM的三维模型都可以模拟过去和未来的气候周期。本研究调查了气候变化对伊朗西北部温室气体增加的可能影响。长期(1000年)温度和降水的年际变化范围,是由用于伊朗西北部研究区域的控制运行(温室气体常数)CGCM3模型得出的。然后,基于二元正态分布,根据温度和降水的二维图确定自然气候变量的范围。最终,可以将检测到的气候变量趋势与该地区的自然气候变化范围进行比较。结果表明,在研究区的不同区域,研究区西部的温度和降水变化的自然气候变量范围(概率为95%)分别小于1.8 C°和40%。在研究区域的东部,这些值分别小于4 C°和40%。然而,最近几年(1998-2008年),西部大部分地区的气候变量几乎超出了自然气候变量的范围。结果表明,近年来气候变化对气候变量的影响。

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  • 来源
    《Quaternary International》 |2014年第29期|130-137|共8页
  • 作者单位

    Department of Irrigation, College of Agriculture, Khouzestan Science and Research Branch, Islamic Azad University, Ahvaz, Iran;

    Department of Irrigation and Drainage Engineering, Collage of Abouraihan, University of Tehran, Pakdasht, Iran;

    Department of Watershed Management, Collage of Natural Resources, University of Yazd, Narmak, Tehran, Iran;

    Department of Water Engineering, Isfahan University of Technology, Iran;

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