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161.
Spatiotemporal changes in vegetation coverage and its driving factors in the Three-River Headwaters Region during 2000-2011 总被引:1,自引:0,他引:1
LIU Xianfeng ZHANG Jinshui ZHU Xiufang PAN Yaozhong LIU Yanxu ZHANG Donghai LIN Zhihui 《地理学报》2014,24(2):288-302
The Three-River Headwaters Region (TRHR),which is the source area of the Yangtze River,Yellow River,and Lancang River,is of key importance to the ecological security of China. Because of climate changes and human activities,ecological degradation occurred in this region. Therefore,"The nature reserve of Three-River Source Regions" was established,and "The project of ecological protection and construction for the Three-River Headwaters Nature Reserve" was implemented by the Chinese government. This study,based on MODIS-NDVI and climate data,aims to analyze the spatiotemporal changes in vegetation coverage and its driving factors in the TRHR between 2000 and 2011,from three dimensions. Linear regression,Hurst index analysis,and partial correlation analysis were employed. The results showed the following:(1) In the past 12 years (2000-2011),the NDVI of the study area increased,with a linear tendency being 1.2%/10a,of which the Yangtze and Yellow River source regions presented an increasing trend,while the Lancang River source region showed a decreasing trend. (2) Vegetation coverage presented an obvious spatial difference in the TRHR,and the NDVI frequency was featured by a bimodal structure. (3) The area with improved vegetation coverage was larger than the degraded area,being 64.06% and 35.94%,respectively during the study period,and presented an increasing trend in the north and a decreasing trend in the south. (4) The reverse characteristics of vegetation coverage change are significant. In the future,degradation trends will be mainly found in the Yangtze River Basin and to the north of the Yellow River,while areas with improving trends are mainly distributed in the Lancang River Basin. (5) The response of vegetation coverage to precipitation and potential evapotranspiration has a time lag,while there is no such lag in the case of temperature. (6) The increased vegetation coverage is mainly attributed to the warm-wet climate change and the implementation of the ecological protection project. 相似文献
162.
LIU Xianfeng ZHANG Jinshui ZHU Xiufang PAN Yaozhong LIU Yanxu ZHANG Donghai LIN Zhihui 《地理学报(英文版)》2014,24(2):288-302
The Three-River Headwaters Region (TRHR), which is the source area of the Yangtze River, Yellow River, and Lancang River, is of key importance to the ecological secu- rity of China. Because of climate changes and human activities, ecological degradation oc- curred in this region. Therefore, "The nature reserve of Three-River Sou,'ce Regions" was established, and "The project of ecological protection and construction for the Three-River Headwaters Nature Reserve" was implemented by the Chinese government. This study, based on MODIS-NDVI and climate data, aims to analyze the spatiotemporal changes in vegetation coverage and its driving factors in the TRHR between 2000 and 2011, from three dimensions. Linear regression, Hurst index analysis, and partial correlation analysis were employed. The results showed the following: (1) In the past 12 years (2000-2011), the NDVI of the study area increased, with a linear tendency being 1.2%/10a, of which the Yangtze and Yellow River source regions presented an increasing trend, while the Lancang River source region showed a decreasing trend. (2) Vegetation coverage presented an obvious spatial difference in the TRHR, and the NDVI frequency was featured by a bimodal structure. (3) The area with improved vegetation coverage was larger than the degraded area, being 64.06% and 35.94%, respectively during the study period, and presented an increasing trend in the north and a decreasing trend in the south. (4) The reverse characteristics of vegetation cov- erage change are significant. In the future, degradation trends will be mainly found in the Yangtze River Basin and to the north of the Yellow River, while areas with improving trends are mainly distributed in the Lancang River Basin. (5) The response of vegetation coverage to precipitation and potential evapotranspiration has a time lag, while there is no such lag in the case of temperature. (6) The increased vegetation coverage is mainly attributed to the warm-wet climate change and the implementation of the ecological protection project. 相似文献
163.
基于倾斜摄影测量的三维建模已成为城市级实景三维建设的发展趋势。在城市三维模型中,由于植被表面不平整,需要用大量的三角面来刻画,但这并不是实景三维数据记录和表达的重点,并且大量的数据会给模型展示和应用带来很大的困难。因此,本文提出了一种顾及地物类别的倾斜摄影三维模型简化方法。首先,计算三维模型的纹理信息和几何信息,结合马尔可夫随机场(MRF)顾及空间一致性的优点提取植被;然后,采用二次误差测度(QEM)算法简化特定的植被区域;最后,对简化后的白膜模型进行纹理重映射。试验结果表明,本文方法能够准确提取并有效简化植被区域,纹理重映射的结果在外观上也与原始模型相差无几,取得了预期的良好效果。 相似文献
164.
Heather M. Stoll Ana Moreno Ana Mendez-Vicente Saul Gonzalez-Lemos Montserrat Jimenez-Sanchez Maria Jose Dominguez-Cuesta R. Lawrence Edwards Hai Cheng Xianfeng Wang 《Quaternary Research》2013
Speleothem growth requires humid climates sufficiently warm to stimulate soil CO2 production by plants. We compile 283 U/Th dates on 21 stalagmites from six cave systems in the NW coast of Spain to evaluate if there are patterns in stalagmite growth that are evidence of climatic forcing. In the oldest stalagmites, from marine oxygen isotope stage (MIS) 7–5, growth persists through the glacial period. Hiatuses and major reductions in growth rate occur during extreme minima in summer insolation. Stalagmites active during the last interglaciation cease growth at the MIS 5–4 boundary (74 ka), when regional sea-surface temperature cooled significantly. During MIS 3, only two stalagmites grew; rates were highest between 50 and 60 ka during the maximum in summer insolation. One stalagmite grew briefly at 41 ka, 36.5 and 28.6 ka, all during warm phases of the Dansgaard–Oeschger cycles. A pronounced Holocene optimum in stalagmite growth occurs from 9 to 6 ka. The cessation of most growth by 4.1 ka, coincident with broad increases in aridity over the Mediterranean and areas influenced by the North African Monsoon, suggest that regions such as NW Spain, with dominant Atlantic moisture sources, also experienced increased aridity at this time. 相似文献
165.
本文论述了大学生身体素质达标计算和评价信息系统问题,作者对建立系统的目的、设计开发方法以及所需设备等作了扼要的介绍,以推动计算机在体育教育事业中的应用。 相似文献
166.
167.
YUEPeng WANGYandong GONGJianya HUANGXianfeng 《地球空间信息科学学报》2004,7(3):174-179
This paper compares the differences between the mathematical model in graph theory and GIS network analysis model. Thus it claims that the GIS network analysis model needs to solve. Then this paper introduces the spatial data management methods in object-relation database for GIS and discusses its effects on the network analysis model. Finally it puts forward the GIS network analysis model based on the object-rela-tion database. The structure of the model is introduced in detail and research is done to the internal and external memory data structure of the model. The results show that it performs well in practice. 相似文献
168.
中国地震应急搜救中心于2004年10月28日在北京正式挂牌成立。这标志着中国地震应急救援体系进一步得到健全,并走向规范化。中国地震应急搜救中心将致力于整合中国地震现场工作资源,努力建设具有国际先进水平的国家级地震应急搜救基地和技术中心, 相似文献
169.
深层地热能是一种清洁环保的可再生能源,尾水回灌是深层地热可持续开发利用的重要保证,但目前国内地热尾水回灌还处在起步阶段,地热尾水回灌方案优化设计的理论模型尚不成熟。文章结合示踪试验,提出了基于等效渗流通道模型的热储参数反演与开采井热突破预测的完整理论框架。应用多孔介质溶质运移理论,修正了等效渗流通道中的溶质浓度解析解,并联合移动渐近线法提出了热储参数反演理论模型;推导了等效渗流通道中的对流传热解析模型,可对开采井中的水温变化进行预测。依托山东省德州市平原县魏庄社区地热对井示踪试验,应用该理论框架进行了示踪试验反演及开采井热突破预测,并对影响开采井热突破的主要因素进行了敏感性分析。 相似文献
170.
欧龙布鲁克地块西北缘青海冷湖北片麻状花岗闪长岩SiO_2、MgO含量较低,Al_2O_3、Na_2O、CaO含量较高,铝饱和指数(ASI)为0.79~0.92,属高钾钙碱性系列。球粒陨石标准化稀土元素配分曲线表现为轻稀土元素富集型,轻、重稀土元素分馏明显,Eu呈弱的负异常(δEu=0.82~0.90)。微量元素地球化学特征显示,岩石富集大离子亲石元素Rb、Th和U,弱亏损高场强元素Nb、Ta、Zr等,显示出与板块俯冲作用有关的造山带岩浆岩的特征。青海冷湖北片麻状花岗闪长岩为角闪岩相压力条件下变玄武质岩石部分熔融的产物。LA-ICP-MS锆石206Pb/238Pb年龄为470.2±1.2Ma(n=19,MSWD=0.68),代表片麻状花岗闪长岩的成岩年龄。结合区域地质演化特征认为,该岩体形成于火山弧构造环境,是早奥陶世北阿尔金洋壳向欧龙布鲁克地块俯冲作用的地质记录。 相似文献