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Landscape Dynamics and Sustainability Assessment of Isolated Island Habitats (Zijin Mountain) on the Loess Plateau from 1975 to 2018

机译:黄土高原离岛生境(紫金山)1975年至2018年的景观动态和可持续性评估

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Based on Landsat Multispectral Scanner (MSS)/Thematic Mapper (TM)/Enhanced Thematic Mapper Plus (ETM+)/Operational Land Imager (OLI) sensors data (1975-2018), MODIS NDVI data (2000-2018), some average annual precipitation and temperature data of surrounding meteorological stations (1980-2015) and ASTER GDEM digital elevation model data, we carried on the fragmentation degree, spatial-temporal differentiation and correlation analyses on the climate change factors (average annual precipitation and temperature), human activity factors (urban and rural residential land, regional lighting index, land use change) and remote sensing index (normalized differential vegetation index, NDVI) in Zijin Mountain region. The results show that some ecological, cultural and geographical indicators have changed in the Zijin Mountain region for the past 44 years. The study area of urban and rural construction land has increased by 4.29 times. Over the 32 years, the average vegetation index of the whole basin has increased by 35.12%, the area of shrubs has increased to 52.60% of the basin's available area, and the area of forest has increased by about 1.3%. The average annual precipitation change rate of 36a (1980~2015) was +18.7 mm/10a, and the annual average temperature change rate was +0.42 °C/10a. Above all, the study area has had a warm-humid tendency to develop. In the past 44 years, the habitat fragmentation index of the ecological environment has increased by 6.04 times. The Zijin Mountain region has been transformed from an original mountain grassland ecosystem to a mountainous dry-farming agricultural ecosystem. Human activities have changed the original ecological structure, accelerated the habitat fragmentation, and become the leading factor in the degradation of ecological structure.
机译:基于Landsat多光谱扫描仪(MSS)/ Thematic Mapper(TM)/ Enhanced Thematic Mapper Plus(ETM +)/ Operational Land Imager(OLI)传感器数据(1975-2018),MODIS NDVI数据(2000-2018),一些年平均降水量气象站的温度和温度数据(1980-2015年)和ASTER GDEM数字高程模型数据,我们对气候变化因子(年平均降水量和温度),人类活动因子进行了破碎程度,时空分异和相关性分析(紫金山地区的城市和农村居民用地,区域照明指数,土地使用变化)和遥感指数(归一化植被指数,NDVI)。结果表明,过去44年来紫金山地区的一些生态,文化和地理指标发生了变化。城乡建设用地研究面积增加了4.29倍。 32年来,整个流域的平均植被指数增加了35.12%,灌木面积增加到流域可利用面积的52.60%,森林面积增加了约1.3%。 36a(1980〜2015)的年平均降水变化率为+18.7 mm / 10a,年平均温度变化率为+0.42°C / 10a。最重要的是,研究区域具有温暖湿润的发展趋势。在过去的44年中,生态环境的生境破碎化指数增加了6.04倍。紫金山地区已从原始的高山草地生态系统转变为山区干旱的农业农业生态系统。人类活动改变了原始的生态结构,加速了生境的破碎化,并成为导致生态结构退化的主要因素。

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