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祁连山南坡主要河谷NDVI时空变化及影响因素分析 被引量:4
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作者 杨荣荣 曹广超 +3 位作者 曹生奎 兰垚 张卓 陈治荣 《广西植物》 CAS CSCD 北大核心 2021年第3期429-437,共9页
为进一步保护祁连山生态环境及合理开发利用河流沿线的植被资源,该文基于MODIS数据的NDVI产品及DEM数据集,对祁连山南坡主要河流谷地2000—2018年植被生长季的NDVI时空分布特征进行了研究,并提取研究区的主要地形因子,分析其对河流谷地... 为进一步保护祁连山生态环境及合理开发利用河流沿线的植被资源,该文基于MODIS数据的NDVI产品及DEM数据集,对祁连山南坡主要河流谷地2000—2018年植被生长季的NDVI时空分布特征进行了研究,并提取研究区的主要地形因子,分析其对河流谷地植被生长季NDVI的影响。结果表明:随着河流两侧缓冲区距离逐渐增大,各年份的NDVI值呈现先增加后平稳再减少的分布特点;2000—2018年研究区河谷NDVI的变化趋势基本一致,整体表现出2010年出现了近20年的峰值;祁连山南坡河流谷地NDVI值,从斜坡(16°~25°)至急坡(41°~45°)增加的速率最大,说明该区间为NDVI值突变区间。2000—2018年祁连山南坡主要河流谷地的NDVI时空分布,可能受地形、气温和降水等自然因素影响较大,其受人为干扰因素影响较小,其中降水并非影响研究区河谷植被NDVI分布的主导因素,而气温可能是影响研究区河谷植被NDVI分布的主导因素。在地形因子中,存在较适合植被生长的特定坡度区间,且太阳辐射能量的增加有利于植被的生长。 展开更多
关键词 河流谷地 NDVI 时空分布 影响因素
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Variations and trends of trans-boundary runoff in the longitudinal range-gorge region
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作者 YU Yan-ling PAN Feng +2 位作者 LIU Xin-you CHEN Wen-hua HE Da-ming 《Journal of Mountain Science》 SCIE CSCD 2017年第2期316-324,共9页
The mountainous hydrological process usually shows high variation to climate change and human action. In the Longitudinal Range-Gorge Region(LRGR), Southwestern China and Southeast Asian, the transboundary runoff va... The mountainous hydrological process usually shows high variation to climate change and human action. In the Longitudinal Range-Gorge Region(LRGR), Southwestern China and Southeast Asian, the transboundary runoff variations are much more sensitive and complex under the interaction of climate change, "corridor-barrier" functions in LRGR,and dams building. In this paper, based on the long hydrological records(1956-2013) from three mainstream hydrological stations in Nu River,Lancang River, and Red River, the region runoff variations were analyzed. The results show out: i) the regional runoff changes were strongly influenced by the "Corridor-Barrier" functions in LRGR from west to east, the variability extent of annual runoff increased, but tended to decrease after 2009 and the reduced extents also increased; ii) the annual runoff change in the three rivers had high concentration degrees; iii) there were periodicities of 33 years of runoff change in Nu River and Lancang River, and 30 years in Red River, and the lower flow period would continue for 8-9 years in Nu River and Lancang River but only for 4 years in Red River; iv) since 2010, as the two mega dams of Xiaowan and Nuozhadu built in Lancang River mainstream, their variations of annual runoff were quite different. The research results could offer a scientific base for sustainable utilization,conservation, and management of the regional water resources 展开更多
关键词 Runoff variations Climate change "Corridor-barrier" functions Longitudinal rangegorge region Transboundary rivers
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