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Environmental resilience of rangeland ecosystems: assessment drought indices and vegetation trends on arid and semi-arid zones of Central Asia

机译:牧场生态系统的环境弹性:评估中亚干旱和半干旱地区的干旱指数和植被趋势

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The Central Asian (CA) rangelands is a part of the arid and semi-arid ecological zones and spatial extent of drylands in CA (Tajikistan, Kazakhstan, Uzbekistan, Kyrgyzstan, and Turkmenistan) is vast. Projections averaged across a suite of climate models, as measured between 1950-2012 by Standardised Precipitation-Evapotranspiration Index (SPEI) estimated a progressively increasing drought risks across rangelands (Turkmenistan, Tajikistan and Uzbekistan) especially during late summer and autumn periods, another index: Potential Evapotranspiration (PET) indicated drought anomalies for Turkmenistan and partly in Uzbekistan (between 1950-2000). On this study, we have combined a several datasets of drought indices (SPIE, PET, temperature_T℃ and precipitation_P) for better estimation of resilienceon-resilience of the ecosystems after warming the temperature in the following five countries, meanwhile, warming of climate causing of increasing rating of degradations and extension of desertification in the lowland and foothill zones of the landscape and consequently surrounding experienced of a raising balance of evapotranspiration (ET_0). The study concluded, increasing drought anomalies which is closely related with raising (ET_0) in the lowland and foothill zones of CA indicated on decreasing of NDVI indices with occurred sandy and loamy soils it will resulting a loss of vegetation diversity (endangered species) and raising of wind speeds in lowlands of CA, but on regional level especially towards agricultural intensification (without rotation) it indicated no changes of greenness index. It was investigated to better interpret how vegetation feedback modifies the sensitivity of drought indices associated with raising tendency of air temperature and changes of cold and hot year seasons length in the territory of CA.
机译:中亚(CA)牧场是干旱和半干旱生态区的一部分,CA(塔吉克斯坦,哈萨克斯坦,乌兹别克斯坦,吉尔吉斯斯坦和土库曼斯坦)的旱地空间范围广。根据标准化降水-蒸散指数(SPEI)在1950-2012年间测算的一系列气候模型的平均估计值估计整个牧场(土库曼斯坦,塔吉克斯坦和乌兹别克斯坦)的干旱风险在逐步增加,特别是在夏末和秋季期间,另一个指数:潜在的蒸散量(PET)表明土库曼斯坦和部分乌兹别克斯坦(1950-2000年)的干旱异常。在这项研究中,我们结合了几个干旱指数数据集(SPIE,PET,温度_T℃和降水量_P),以更好地估算以下五个国家温度升高后生态系统的复原力/非复原力,同时,气候变暖导致景观低地和山麓带的退化程度和荒漠化程度不断提高,因此周围地区的蒸散量(ET_0)升高。研究得出结论,干旱异常增加与CA低地和山麓地区的升高(ET_0)密切相关,这表明发生沙质和壤土的NDVI指数降低,这将导致植被多样性的丧失(濒危物种)和升高在CA低地风速,但在区域一级,特别是对农业集约化(无轮作),表明绿色指数没有变化。为了更好地解释植被反馈如何改变干旱指数的敏感性,干旱指数与加利福尼亚州境内气温的升高趋势以及冷,热年季节长度的变化有关。

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