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Alpine sparsely vegetated areas in the eastern Qilian Mountains shrank with climate warming in the past 30 years

机译:阿尔卑斯山在东部祁连山的植被区稀疏,在过去的30年里,气候变暖萎缩

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Alpine sparsely vegetated areas (ASVAs) in mountains are sensitive to climate change and rarely studied. In this study, we focused on the response of ASVA distribution to climate change in the eastern Qilian Mountains (EQLM) from the 1990s to the 2010s. The ASVA distribution ranges in the EQLM during the past three decades were obtained from the Thematic Mapper remote sensing digital images by using the threshold of normalized difference vegetation index (NDVI) and artificial visual interpretation. Results indicated that the ASVA shrank gradually in the EQLM and lost its area by approximately 11.4% from the 1990s to the 2010s. The shrunken ASVA with markedly more area than the expanded one was mainly located at altitudes from 3700 m to 4300 m, which were comparatively lower than the average altitude of the ASVA distribution ranges. This condition led to the low ASVA boundaries in the EQLM moving upwards at a significant velocity of 22 m/decade at the regional scale. This vertical zonal process was modulated by topography-induced differences in local hydrothermal conditions. Thus, the ASVA shrank mainly in its lower parts with mild and sunny slopes. Annual maximum NDVI in the transition zone increased significantly and showed a stronger positive correlation with significantly increasing temperature than insignificant precipitation variations during 1990–2015. The ASVA shrinkage and up-shifting of its boundary were attributed to climate warming, which facilitated the upper part of alpine meadow in the EQLM by releasing the low temperature limitation on vegetation growth.
机译:山脉中的高山稀疏地区(Asvas)对气候变化敏感,很少研究。在这项研究中,我们专注于Asva分配在20世纪90年代到2010年代东祁连山(EQLM)的气候变化对气候变化的响应。通过使用归一化差异植被指数(NDVI)和人工视觉解释的阈值,从专题映射器遥感数字图像中获得EQLM中的ASVA分发范围。结果表明,ASVA逐渐在EQLM中逐渐萎缩,并将其面积从20世纪90年代损失约11.4%。缩小的ASVA具有比扩展的更大的区域主要位于3700米至4300米的海拔高度,比ASVA分配范围的平均海拔相对低。这种情况导致EQLM中的低ASVA边界在区域尺度上以22米/十年的显着速度向上移动。这种垂直的区间过程通过地形诱导的局部水热条件的差异来调节。因此,ASVA主要在其下部萎缩,具有温和和阳光倾斜的斜坡。过渡区中的年度最大NDVI显着增加,并显示出比1990 - 2015年期间微不足道的降水变化显着增加的阳性相关性更强。其边界的ASVA收缩和升压归因于气候变暖,这通过释放对植被生长的低温限制,促进了AQLM中的高寒草甸的上部。

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