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Evaluating the variability of ANPP in central Iranian arid and semi-arid rangelands using CASA model and its relationship with climatic factors

机译:使用CASA模型评估伊朗干旱和半干旱牧场ANPP的变异及其与气候因子的关系

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Aboveground Net Primary Production (ANPP) plays an important role in regulating ecological processes and carbon cycle in arid and semi-arid rangelands. Hence, this study aimed to investigate the spatio-temporal variability of rangeland ANPP in seven bioclimatic zones in Isfahan Province using the Carnegie-Ames-Stanford Approach (CASA) ecosystem model fitted with MODIS-NDVI and climatic data during 2000-2016. The model evaluation indicated a good agreement between the estimated and observed ANPP (R-2 = 0.917). In concomitant with the precipitation gradient, the mean annual ANPP increased from east towards west and southwest of the region from zero to 160 g C m(-2) yr(-1). The maximum and minimum ANPP values occurred in humid and cold as well as hyper-arid and warm zone, respectively. The annual temporal variability of ANPP was analyzed in response to climatic factors (precipitation and temperature), Temperature Vegetation Dryness Index (TVDI) and Standard Precipitation Index (SPI) drought indices. The drought was found as the most important factor affecting ANPP. The minimum and maximum ANPP values were observed in 2000 (23.23 g C m(-2) yr(-1)) and 2014 (41.73 g C m(-2) yr(-1)). The maximum ANPP occurred in May and June during which temperature, as an important factor in plant growth, reached its optimum and precipitation affected with a time lag. The annual rangeland ANPP was positively associated with precipitation and negatively with temperature.
机译:在地上净初级生产(ANPP)在干旱和半干旱牧场调节生态过程和碳循环方面发挥着重要作用。因此,本研究旨在调查伊斯法罕 - 斯坦福(Casa)生态系统模型在2000-2016期间使用MODIS-NDVI和气候数据的七种生物魅力区居住在伊斯法罕的七种生物魅力区的时空变异性。模型评估表明估计和观察到的ANPP之间的良好一致性(R-2 = 0.917)。伴随着沉淀梯度,平均年度ANPP从东部向西和西南部的区域增加到从0到160g C m(-2)Yr(-1)。分别在潮湿和寒冷以及超干旱和温暖区发生的最大和最小ANPP值。响应气候因子(沉淀和温度),温度植被干燥指数(TVDI)和标准降水指数(SPI)干旱指数,分析了ANPP的年度时间变异性。干旱被发现是影响ANPP的最重要因素。在2000年观察到最小和最大ANPP值(23.23g C m(-2)Yr(-1))和2014(41.73g C m(-2)Yr(-1))。在5月和6月发生的最大ANPP在此温度下,作为植物生长的重要因素,达到了与时间滞后影响的最佳和沉淀。年岭南ANPP与温度呈阳性和负面的阳性相关。

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