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Interannual variability of the normalized difference vegetation index on the Tibetan Plateau and its relationship with climate change

机译:青藏高原归一化植被指数年际变化及其与气候变化的关系

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The Qinghai-Xizang Plateau, or Tibetan Plateau, is a sensitive region for climate change, where the manifestation of global warming is particularly noticeable. The wide climate variability in this region significantly affects the local land ecosystem and could consequently lead to notable vegetation changes. In this paper, the interannual variations of the plateau vegetation are investigated using a 21-year normalized difference vegetation index (NDVI) dataset to quantify the consequences of climate warming for the regional ecosystem and its interactions. The results show that vegetation coverage is best in the eastern and southern plateau regions and deteriorates toward the west and north. On the whole, vegetation activity demonstrates a gradual enhancement in an oscillatory manner during 1982–2002. The temporal variation also exhibits striking regional differences: an increasing trend is most apparent in the west, south, north and southeast, whereas a decreasing trend is present along the southern plateau boundary and in the central-east region. Covariance analysis between the NDVI and surface temperature/precipitation suggests that vegetation change is closely related to climate change. However, the controlling physical processes vary geographically. In the west and east, vegetation variability is found to be driven predominantly by temperature, with the impact of precipitation being of secondary importance. In the central plateau, however, temperature and precipitation factors are equally important in modulating the interannual vegetation variability.
机译:青藏高原或青藏高原是气候变化敏感地区,全球变暖的表现尤为明显。该地区广泛的气候变化极大地影响了当地的土地生态系统,因此可能导致明显的植被变化。本文利用21年归一化植被指数(NDVI)数据集研究了高原植被的年际变化,以量化气候变暖对区域生态系统及其相互作用的影响。结果表明,植被覆盖度在东部和南部高原地区最好,而向西部和北部则恶化。总体而言,植被活动在1982-2002年期间呈振荡方式逐渐增强。时间变化也表现出惊人的区域差异:在西部,南部,北部和东南部,上升趋势最为明显,而在南部高原边界和中东部地区则呈下降趋势。 NDVI与地表温度/降水之间的协方差分析表明,植被变化与气候变化密切相关。但是,控制物理过程在地理位置上有所不同。在西部和东部,发现植被变化主要受温度驱动,而降水影响次要。然而,在中部高原,温度和降水因子在调节年际植被变化方面同样重要。

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