以环青海湖地区为研究区,基于MODIS NPP数据、气象数据和Thornthwaite模型,估算了草地实际净初级生产力(actual net primary productivity,简称NPP_A)和潜在净初级生产力(potential net primary productivity,简称NPP_P),并将NPP_P和NP...以环青海湖地区为研究区,基于MODIS NPP数据、气象数据和Thornthwaite模型,估算了草地实际净初级生产力(actual net primary productivity,简称NPP_A)和潜在净初级生产力(potential net primary productivity,简称NPP_P),并将NPP_P和NPP_A的差作为人类活动对净初级生产力的影响(net primary productivity influenced by human,简称NPP_H),在此基础上,分析了草地NPP_A的时空变化以及气候变化和人类活动对草地的影响。结果表明:2000—2015年,环青海湖地区的年均草地NPP_A为176.93 g C·m^(-2)·a^(-1);16年来环青海湖地区草地NPP_A呈波动增加趋势,在空间分布上,草地NPP_A从西到东呈逐渐增加的态势;16年来环青海湖地区87.42%的区域草地发生恢复,12.58%的区域发生退化,总体上草地以恢复为主;在气候变化和人类活动对草地恢复的影响中,由气候变化主导草地恢复的比例为10.98%,由人类活动主导草地恢复的比例为5.27%,而人类活动和气候变化共同主导草地恢复的比例为83.75%,气候变化和人类活动的共同作用是草地恢复的主导力量;在气候变化和人类活动对草地退化的影响中,仅由气候变化主导草地退化的比例为6.28%,由人类活动主导草地退化的比例为50.75%,两者共同主导的草地退化的比例为42.97%。可见,草地的局部退化主要是由于不合理的人类活动导致的,如过度放牧、草地开垦和土地覆盖变化等。展开更多
Desertification is one of the most serious eco-environmental problems around Qinghai Lake.Based on GIS and RS,GIS analysis was used to obtain the information of spatial-temporal change and different pattern of deserti...Desertification is one of the most serious eco-environmental problems around Qinghai Lake.Based on GIS and RS,GIS analysis was used to obtain the information of spatial-temporal change and different pattern of desertification in each county around Qinghai Lake in four phases of1976,1987,1995 and 2006.Using the function of intersect and overlay supported by ARCGIS,with analyzing attributes of vector RS images,we obtained transition data and established transfer matrix of land-use types in recent 30 years,besides,protracted land-use transition maps of all desertification classes.In further,we analyzed transition quantity and direction of desertification in each county,moreover,reconstructed the process of spatial-temporal evolution of desertification.The results are showed below:(1)it's the transition between desertified land and others but not in the desertified that played the main role in Gangcha and Gonghe County,while the transfer between desertified lands were greater than that with other land-use types in Haiyan County.(2)Extremely severe desertified land mainly distributes in Ketu and Sand Islands that belongs to Haiyan County,and moderate desertified land in riversides of Gangcha County,also,the light desertification expanded too rapidly to become the most desertified land-use type in the surrounding of Qinghai Lake since 1976.(3)By using relative change rate of desertified land,the regional variability rank from top to toe was Gangcha,Haiyan and Gonghe.展开更多
文摘以环青海湖地区为研究区,基于MODIS NPP数据、气象数据和Thornthwaite模型,估算了草地实际净初级生产力(actual net primary productivity,简称NPP_A)和潜在净初级生产力(potential net primary productivity,简称NPP_P),并将NPP_P和NPP_A的差作为人类活动对净初级生产力的影响(net primary productivity influenced by human,简称NPP_H),在此基础上,分析了草地NPP_A的时空变化以及气候变化和人类活动对草地的影响。结果表明:2000—2015年,环青海湖地区的年均草地NPP_A为176.93 g C·m^(-2)·a^(-1);16年来环青海湖地区草地NPP_A呈波动增加趋势,在空间分布上,草地NPP_A从西到东呈逐渐增加的态势;16年来环青海湖地区87.42%的区域草地发生恢复,12.58%的区域发生退化,总体上草地以恢复为主;在气候变化和人类活动对草地恢复的影响中,由气候变化主导草地恢复的比例为10.98%,由人类活动主导草地恢复的比例为5.27%,而人类活动和气候变化共同主导草地恢复的比例为83.75%,气候变化和人类活动的共同作用是草地恢复的主导力量;在气候变化和人类活动对草地退化的影响中,仅由气候变化主导草地退化的比例为6.28%,由人类活动主导草地退化的比例为50.75%,两者共同主导的草地退化的比例为42.97%。可见,草地的局部退化主要是由于不合理的人类活动导致的,如过度放牧、草地开垦和土地覆盖变化等。
基金National Key Technology R&D Program of China(2007BAC30B03)"The Fundamental Research Funds for the Central Universities"and"Forestry Industry Research Special Funds for Public Welfare"(201004025)
文摘Desertification is one of the most serious eco-environmental problems around Qinghai Lake.Based on GIS and RS,GIS analysis was used to obtain the information of spatial-temporal change and different pattern of desertification in each county around Qinghai Lake in four phases of1976,1987,1995 and 2006.Using the function of intersect and overlay supported by ARCGIS,with analyzing attributes of vector RS images,we obtained transition data and established transfer matrix of land-use types in recent 30 years,besides,protracted land-use transition maps of all desertification classes.In further,we analyzed transition quantity and direction of desertification in each county,moreover,reconstructed the process of spatial-temporal evolution of desertification.The results are showed below:(1)it's the transition between desertified land and others but not in the desertified that played the main role in Gangcha and Gonghe County,while the transfer between desertified lands were greater than that with other land-use types in Haiyan County.(2)Extremely severe desertified land mainly distributes in Ketu and Sand Islands that belongs to Haiyan County,and moderate desertified land in riversides of Gangcha County,also,the light desertification expanded too rapidly to become the most desertified land-use type in the surrounding of Qinghai Lake since 1976.(3)By using relative change rate of desertified land,the regional variability rank from top to toe was Gangcha,Haiyan and Gonghe.
