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Drought Monitoring and Evaluating for Qinghai-Tibet Plateau Grassland

机译:青藏高原草原干旱监测和评价

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The grassland is the main part of the Qinghai-Tibet Plateau which consists of 30% of grassland in China. The method of grassland drought monitoring and evaluating was studied on base of Penman-Monteith equation (Allen et al. 1998) and AVIM-GPvASS model (Qian et al. 2012 ) using daily meteorological data in Qinghai-Tibet Plateau from 1961 to 2007. Temperature, precipitation, sunshine hours, evapotranspiration, water surplus and deficit of a year and four seasons, in the growing season from April to September were systemically calculated and analysed. The grassland drought index was developed according to climate suitability of grassland vegetation, water surplus and deficit, net primary productivity (NPP). The grassland drought index and indicators of drought monitoring and evaluating were validated using data in 2006 and 2007, applied in 2012 for Qinghai-Tibet Plateau grassland. Results showed the index and indicators reflected the water surplus and deficit, drought conditions and its influence ongrassland productivity.
机译:草原是青藏高原的主要部分,由中国30%的草原组成。在Penman-Monteith方程(Allen等,1998)和Avim-GPVass Model(Qian等人)的基础上研究了草地干旱监测和评估的方法4月至9月至9月在生长季节的温度,降水量,阳光小时,蒸散,水盈余和赤字,并分析了4月至9月的生长季节。草地干旱指数是根据草原植被,水盈和赤字,初级生产力(NPP)的气候适用性开发的。 2012年2006年2006年和2007年的数据验证了草原干旱指数和干旱监测和评估指标,适用于青藏高原草原。结果表明,指数和指标反映了水盈和赤字,干旱条件及其影响截止地生产力。

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