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The Effect of Climate Change on Future Reference Evapotranspiration in Different Climatic Zones of Iran

机译:气候变化对伊朗不同气候区未来参考蒸散的影响

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Evapotranspiration can be considered as an indicator in evaluating the effects of climate change. It is the sole factor with the capability of concurrently balancing the ecosystem energy and water fluxes. Reference evapotranspiration (ETo) is the amount of water evaporated from reference crop that is affected by climatic parameters. The aim of this study was to assess ETo during the period of 2020-2049 in various climatic zones of Iran (including Tabriz, Bushehr, Isfahan, Sanandaj and Urmia). Climatic parameters including relative humidity, wind speed, Sunshine hours, atmospheric pressure, maximum and minimum temperatures were utilized for calculating ETo using FAO Penman-Monteith equation. The NCEP data and HADCM3 model data (under scenario A2 and B2) were used for prediction of future climatic parameters during 2020-2049. Statistical down scaling model was used as a hybrid regression model as well as a stochastic weather data generator. The course period was between 1986 and 2015 that was regarded for calibration and evaluation of the model. Subsequently, evapotranspiration was estimated using the model outputs in the FAO Penman-Monteith equation. Results indicated that the simulated data by the model has the same accuracy and validity under both scenarios A2 and B2. Results showed that in the studied areas, ETo tend to have an increasing trend in upcoming years. In scenario A2, ETo will increase about 16.81, 0.137, 17.52, 9.46 and 2.57 mm year(-1) in Tabriz, Bushehr, Isfahan, Sanandaj and Urmia stations, respectively. Also our results represented that ETo will increase about 7.67, 6.52, 10.33, 7.73 and 1.99 mm year(-1) in Tabriz, Bushehr, Isfahan, Sanandaj and Urmia stations, respectively based on the B2 scenario. Although no significant trend was observed in most of the climatic variables under A2 and B2 scenarios over the time period of 2020-2049, the ETo significantly increased during this period. Hence it could be concluded that ETo is a better indicator for
机译:蒸散可以被视为评估气候变化影响的指标。它是具有同时平衡生态系统能量和水通量的能力的唯一因素。参考蒸发(EtO)是由气候参数影响的参考作物蒸发的水量。本研究的目的是在伊朗的各种气候区(包括Tabriz,Bushehr,Isfahan,Sanandaj和Urmia)的2020-2049期间评估ETO。包括相对湿度,风速,阳光小时,大气压,最大和最小温度的气候参数用于使用FAO Penman-Monteith方程计算ETO。 NCEP数据和HADCM3模型数据(在场景A2和B2下)用于预测2020-2049期间将来的气候参数。统计下缩放模型用作混合回归模型以及随机天气数据发生器。课程期间是1986年至2015年间认为校准和评估该模型。随后,使用FAO Penman-Monteith方程中的模型输出估计蒸发蒸腾。结果表明,模型的模拟数据在两个场景A2和B2下具有相同的准确性和有效性。结果表明,在学习的地区,ETO往往在即将到来的年度趋势越来越大。在情景A2中,ETO将分别增加约16.81,0.137,17.52,9.46和2.57 mm(-1)在Tabriz,Bushehr,Isfahan,Sanandaj和Urmia站中。此外,我们的结果表明,塔托将根据B2场景分别基于B2场景增加约7.67,6.52,1.33,7.73和1.9.52,10.33,7.73和1.99 mm年(-1),Sanandaj和Urmia站。虽然在A2和B2场景下的大多数气候变量中没有观察到显着趋势,但在2020-2049的时间段内,ETO在此期间显着增加。因此,可以得出结论,Eto是一个更好的指标

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