基于网格单元的西北干旱区城市土地覆被/土地利用时空变化研究——以新疆喀什市为例          下载免费PDF全文

鄂子骥  阿里木江·卡斯木  买买提江·买提尼亚孜  安尼瓦尔·阿布都热依木 《干旱区地理》2018,41(3):625-633

利用1995、2005和2015年3期Landsat遥感数据,提取新疆喀什地区喀什市土地覆被/土地利用信息,并将各时期用地分类数据分别转入50 m×50 m的矢量网格单元,建立基于矢量网格单元的土地覆被/土地利用网格图,探讨喀什市1995-2015年土地覆被/土地利用时空变化特征及驱动因素;通过叠加分析,研究时期内各用地类型之间相互转换和替代关系。结果显示：（1）1995-2015年间喀什市土地覆被/土地利用变化剧烈,以建设用地面积变化最为显著,20 a间面积增加近3倍,未利用地和绿地面积均有所减少,水体的面积变化显现波动态势。（2）1995-2015年喀什市建设用地扩张主要以"摊大饼"式的外延扩张为主,但也伴随少量内部填充的集约式增长模式,通过回归分析,建设用地面积的增加与城市人口的增加和社会经济的发展具有紧密的正相关关系。（3）建设用地在扩张过程中主要侵占和替代了未利用地和绿地,并且绿地的增加与减少和未利用地的侵占与被侵占有着直接关联。  相似文献   

WISE EXPLOITATION OF NEWLY GROWING LAND RESOURCES——An Assessment on Land-use Change of Chongming Island Using GIS   总被引：2，自引：0，他引：2  

ZHAO Bin    LI Bo  MA Zhi-jun  CHEN Jia-kuan  NAKAGOSHI Nobukazu 《中国地理科学(英文版)》2003,(2)

1INTRODUCTIONThreewell-documentedmajorglobalchangesaffectinghumanbeingsareincreasingconcentrationofcarbondioxideintheatmosphere,alterationinthebiochemistryoftheglobalnitrogencycle,andon-goinglanduse/coverchange(LUCC)(VITOUSEK,1994).Forcen-turies,humanbeingshavebeenalteringtheearth'ssurfacetoproducetheirfoodandsheltersthroughagri-culturalactivities(REIDetal.,2000).Likeothercountries,Chinaisalsosubjecttolandtransformation,forinstance,abouthalfamillionhectaresofwetlandshavebeenreclaime…  相似文献   

Snow water content estimation from measured snow temperature     

李志军  赵海清  冯恩民  程斌  卢鹏 《极地研究(英文版)》2007,18(1):1-7

The vertical temperature profiles of snow and sea ice have been measured in the Arctic during the 2nd Chinese National Arctic Research Expedition in 2003(CHINARE2003).The high-resolution temperature profile in snow is solved by one-dimensional heat transfer equation.The effective heat diffusivity,internal heat sources are identified.The internal heat source refers to the penetrated solar radiation which usually warms the lower part of the snow layer in summer.By temperature gradient analysis,the zero level can be clarified quantitatively as the boundary of the dry and wet snow.According to the in situ time series of vertical temperature profile,the time series of water content in snow is obtained based on an evaluation method of snow water content associated with the snow and ice physical parameters.The relationship of snow water content and snow temperature and temporal-spatial distribution of snow water content are presented  相似文献   

Evaluation of snow models in terrestrial biosphere models using ground observation and satellite data: impact on terrestrial ecosystem processes     

Kazuhito Ichii  Michael A. White  Petr Votava  Andrew Michaelis  Ramakrishna R. Nemani 《水文研究》2008,22(3):347-355

Snow is important for water management, and an important component of the terrestrial biosphere and climate system. In this study, the snow models included in the Biome‐BGC and Terrestrial Observation and Prediction System (TOPS) terrestrial biosphere models are compared against ground and satellite observations over the Columbia River Basin in the US and Canada and the impacts of differences in snow models on simulated terrestrial ecosystem processes are analysed. First, a point‐based comparison of ground observations against model and satellite estimates of snow dynamics are conducted. Next, model and satellite snow estimates for the entire Columbia River Basin are compared. Then, using two different TOPS simulations, the default TOPS model (TOPS with TOPS snow model) and the TOPS model with the Biome‐BGC snow model, the impacts of snow model selection on runoff and gross primary production (GPP) are investigated. TOPS snow model predictions were consistent with ground and satellite estimates of seasonal and interannual variations in snow cover, snow water equivalent, and snow season length; however, in the Biome‐BGC snow model, the snow pack melted too early, leading to extensive underpredictions of snow season length and snow covered area. These biases led to earlier simulated peak runoff and reductions in summer GPP, underscoring the need for accurate snow models within terrestrial ecosystem models. Copyright © 2007 John Wiley & Sons, Ltd.  相似文献   

Incorporating topographic variability into a simple regional snowmelt model     

W. T. Sloan  C. G. Kilsby  R. Lunn 《水文研究》2004,18(17):3371-3390

General circulation models (GCMs), or stand‐alone models that are forced by the output from GCMs, are increasingly being used to simulate the interactions between snow cover, snowmelt, climate and water resources. The variation in snowpack extent, and hence albedo, through time in a cell is likely to be substantial, especially in mid‐latitude mountainous regions. As a consequence, the energy budget simulation by a GCM relies on a realistic representation of snowpack extent. Similarly, from a water resource perspective, the spatial extent of the pack is key in predicting meltwater discharges into rivers. In this paper a simple computationally efficient regional snow model has been developed, which is based on a degree‐day approach and simulates the fraction of the model domain covered by snow, the spatially averaged melt rate and the mean snowpack depth. Computational efficiency is achieved through a novel spatial averaging procedure, which relies on the assumptions that precipitation and temperature scale linearly with elevation and that the distribution of elevations in the domain can be modelled by a continuous function. The resulting spatially averaged model is compared with both observations of the duration of snow cover throughout Austria and with results from a distributed model based on the same underlying assumptions but applied at a fine spatial resolution. The new spatially averaged model successfully simulated the seasonal snow duration observations and reproduced the daily dynamics of snow cover extent, the spatially averaged melt rate and mean pack depth simulated by the distributed model. It, therefore, offers a computationally efficient and easily applied alternative to the current crop of regional snow models. Copyright © 2004 John Wiley & Sons, Ltd.  相似文献   

Channel braiding and stability of the Brahmaputra River, Bangladesh, since 1967: GIS and remote sensing analyses   总被引：1，自引：1，他引：1  

T. Takagi  T. Oguchi  J. Matsumoto  M.J. Grossman  M.H. Sarker  M.A. Matin 《Geomorphology》2007,85(3-4):294

Spatial and temporal changes in channel distribution in the large, sandy, braided system of the Brahmaputra River, Bangladesh, were analyzed using satellite images and GIS. Supervised classification of the images within the braided belt, i.e., channels and bars between the bank-lines, provided raster land cover data for 14 different years between 1967 and 2002. The width of the braided-belt, the number and width of channels, the distribution of land cover attributes and land stability change were examined from the data. The results indicate that the recent history of the dynamics of the Brahmaputra can be divided into four phases: 1) the late 1960s to early 1970s, 2) the mid-1970s to early 1980s, 3) the mid-1980s to early 1990s, and 4) the mid-1990s to early 2000s. Spatial distributions of the land cover and channels in Phase 4 were the least complex suggesting a state of dynamic equilibrium. Land cover and channel distributions during Phase 2 were partly less complex indicating quasi-dynamic equilibrium. Phases 1 and 3 can be regarded as transitional phases with more complex conditions. Frequent large floods may have triggered significant changes in the river system during Phases 1 and 3.  相似文献   

风蚀影响因子的敏感性试验   总被引：3，自引：0，他引：3  

李万源  沈志宝  吕世华  李耀辉 《中国沙漠》2007,27(6):984-993

 对风蚀模式的各重要影响因子进行了敏感性试验，结果表明：①随风力的增大，跃动沙粒的粒径范围迅速增大，从而会使更多、更大的尘粒因受到更强烈的撞击作用而释放于空中。但随土壤水分和植被覆盖度的增加，跃动沙粒粒径范围会变窄，较大的粒子很难被激发到空中。②各种土壤沙流通量及尘粒释放率随粒径的变化趋势Q(d)和F(d)与相应的地表土壤有效粒度分布Ps(d)具有相似的特征，说明前人用近地层沙尘粒度分布来代表地表土壤的有效粒度分布是合理的。③若以总沙流通量Q>0.5 g·m^-1·s^-1为风蚀过程开始发生的标准，在干燥、裸露的情况下，沙土、沙壤土、壤土、黏土和粉黏土表面发生风蚀的临界摩擦速度都约为0.3 m·s^-1。相同风力条件下（u*=0.6 m·s^-1），若地表干燥（w=0）并忽略小于0.1 g·m^-1·s^-1的总沙流通量，则抑制5种土壤发生风蚀的最小植被覆盖度分别约为：沙土0.35、沙壤土0.45、壤土0.45、黏土0.55、粉黏土0.55；若地表裸露，抑制风蚀发生的最小水分含量分别为：沙土0.15、沙壤土0.18、壤土0.3、黏土0.36和粉黏土0.33。④通常情况下沙土最不易起尘，它在各个粒径的尘粒释放率比其他土壤均约小3~5个量级。粉黏土最易起尘，且粒径较小，较容易传输到下游很远处。⑤总尘粒释放率F和总沙流通量Q随风力、地表条件的变化一般是同相的，即Q增大，F也会增大。⑥一般情况下F随摩擦速度u*的增大或植被覆盖度cf和土壤水分w的减小而增大；土壤拖曳系数sx和弹性压力垂直分量pye的增加会大大降低尘粒释放率。⑦通常风蚀情况下，5种土壤中粉黏土和沙壤土因聚合粒子破碎产生的尘粒释放率Fc最大，Fc随风力、地表条件变化的敏感度也最强；沙土的Fc最小，其对风力、地表条件的敏感度也最弱。  相似文献   

基于MODIS NDVI的新疆土地覆盖类型划分与潜在荒漠化区域探测   总被引：9，自引：0，他引：9  

王莉雯  牛铮  卫亚星 《干旱区地理》2007,30(4):73-578

采用2002年MODIS 1km的全年NDVI时序数据对新疆及周边地区进行了土地覆盖分类,在分类的过程中重点强调了稀疏植被覆盖区域,这些区域具有潜在荒漠化的趋势。介绍了一种针对不同土地覆盖类型并能重点突出稀疏植被的分类方法,这种方法较好地综合了季节性影响因素和多变的自然条件影响因素。从16天合成的优化过的时序NDVI图像上,通过分析物候变化,可以获得较好的分类结果。将具有潜在荒漠化趋势的区域模型化研究以后,研究结果表明新疆及周边地区40万km2的土地有潜在荒漠化的趋势。由于MODIS NDVI数据覆盖范围较大,并且对植被的生长变化有较高的敏感度,所以它可以被有效地应用于监测大尺度环境变化和荒漠化进程。  相似文献   

Comparative assessment of CORINE2000 and GLC2000: Spatial analysis of land cover data for Europe   总被引：3，自引：0，他引：3  

K. Neumann  M. Herold  A. Hartley  C. Schmullius   《International Journal of Applied Earth Observation and Geoinformation》2007,9(4):425-437

Given the current lack of interoperability between global and regional land cover products, efforts are underway to link the new European global land cover map (GLOBCOVER) with the existing global land cover 2000 map (GLC2000) and European CORINE mapping initiative. Since both datasets apply different mapping standards, key for a successful implementation is a thorough understanding of the heterogeneities among both datasets. Thus, this paper provides an assessment of compatibilities and differences between the CORINE2000 and GLC2000 datasets. The comparative assessment considers inconsistencies between the thematic legends (using the UN land cover classification system-LCCS), class specific accuracies, and the spatial resolution and heterogeneity of the datasets. The results are summarized with implications for the development of the new GLOBCOVER datasets.  相似文献   

光谱与纹理信息复合的土地利用/覆盖变化动态监测研究   总被引：8，自引：0，他引：8  

张锦水  潘耀忠  韩立建  苏伟  何春阳 《遥感学报》2007,11(4):500-510

及时、准确地动态监测地球表面特性对于掌握人类和自然现象之间的关系和相互作用是非常重要的,并为决策的制定奠定基础。传统卫星遥感的土地利用/覆盖变化动态监测方法基本上可分为光谱直接比较法和分类比较法两大类,但两类方法多以光谱信息为基础来提取土地利用变化信息,而忽略纹理等空间信息。本研究中,基于变化向量分析方法,将光谱与纹理两种信息复合计算变化强度,并采用支持向量机法提取变化/非变化信息,通过监督分类确定变化区域内的土地利用/覆盖类型的转移方向,完成土地利用/覆盖动态监测。最后,利用两期TM数据,对海淀区1997—2004年进行土地利用/覆盖变化动态监测,以验证该方法。该方法较分类后比较法在一定程度上减少误差积累,降低了错误类型转化,提取的变化信息总精度达到93.1%,Kappa为0.862,比利用光谱信息双窗口变步长的变化向量分析方法提取出土地利用/覆盖变化信息的精度有一定的提高(总体精度为90.2%,Kappa为0.804)。纹理信息与光谱信息复合,能够更大拉开变化/非变化信息之间的距离,有利于动态变化信息的提取,是该方法能够有效提取变化信息的关键所在。  相似文献