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Response of Grassland Degradation to Drought at Different Time-Scales in Qinghai Province: Spatio-Temporal Characteristics, Correlation, and Implications

机译:青海省不同时间尺度草地退化对干旱的响应:时空特征,相关性及其意义

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Grassland, as the primary vegetation on the Qinghai-Tibet Plateau, has been increasingly influenced by water availability due to climate change in last decades. Therefore, identifying the evolution of drought becomes crucial to the efficient management of grassland. However, it is not yet well understood as to the quantitative relationship between vegetation variations and drought at different time scales. Taking Qinghai Province as a case, the effects of meteorological drought on vegetation were investigated. Multi-scale Standardized Precipitation Evapotranspiration Index (SPEI) considering evapotranspiration variables was used to indicate drought, and time series Normal Difference Vegetation Index (NDVI) to indicate the vegetation response. The results showed that SPEI values at different time scales reflected a complex dry and wet variation in this region. On a seasonal scale, more droughts occurred in summer and autumn. In general, the NDVI presented a rising trend in the east and southwest part and a decreasing trend in the northwest part of Qinghai Province from 1998 to 2012. Hurst indexes of NDVI revealed that 69.2% of the total vegetation was positively persistent (64.1% of persistent improvement and 5.1% of persistent degradation). Significant correlations were found for most of the SPEI values and the one year lagged NDVI, indicating vegetation made a time-lag response to drought. In addition, one month lagged NDVI made an obvious response to SPEI values at annual and biennial scales. Further analysis showed that all multiscale SPEI values have positive relationships with the NDVI trend and corresponding grassland degradation. The study highlighted the response of vegetation to meteorological drought at different time scales, which is available to predict vegetation change and further help to improve the utilization efficiency of water resources in the study region.
机译:草原是青藏高原的主要植被,近几十年来由于气候变化,其水资源供应日益受到影响。因此,查明干旱的演变对有效管理草地至关重要。但是,关于不同时间尺度上植被变化与干旱之间的定量关系,人们还没有很好的理解。以青海省为例,研究了干旱对植被的影响。考虑蒸散量的多尺度标准降水蒸散指数(SPEI)用于指示干旱,而时间序列正态植被指数(NDVI)用于指示植被响应。结果表明,不同时间尺度的SPEI值反映了该区域复杂的干湿变化。在季节性范围内,夏季和秋季发生更多的干旱。总体而言,从1998年到2012年,NDVI在青海省的东部和西南部呈上升趋势,而在西北部呈下降趋势。NDVI的Hurst指数表明,总植被中有69.2%为正持续性(占64.1%)。持续改善和持续退化的5.1%)。发现大多数SPEI值与一年的NDVI滞后具有显着的相关性,表明植被对干旱做出了时滞响应。另外,一个月滞后的NDVI在年度和两年期尺度上对SPEI值做出了明显的响应。进一步的分析表明,所有多尺度SPEI值均与NDVI趋势和相应的草地退化呈正相关。该研究强调了不同时间尺度上植被对气象干旱的响应,可用于预测植被变化并进一步帮助提高研究区域水资源的利用效率。

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