Forward change detection 2000 - 2004: urban sprawl and imperviousness in Lexington, KY

D. Zourarakis, M. Palmer, A. Brenner, S. C. Lambert
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Abstract

Over time, changes in land cover are likely to alter the distribution of imperviousness in landscapes, bringing the possibility of negative effects on watersheds due to degradation of water quantity and quality parameters (Schueler, 1994). Imperviousness is generally correlated with and utilized as a strong indicator of urban and suburban growth, serving as a proxy for the “developed” Anderson Level II classes (low, medium, high, open). This classification scheme serves as the working paradigm upon which the National Landcover Dataset 2001 (NLCD01) and the Kentucky Landcover Dataset 2001 (KLCD01) were built (http://kls.ky.gov; http://landcover.usgs.gov/index.asp). The current phase of the Kentucky Landscape Snapshot project necessitates the development of a change detection component. At this stage, work is revolving around utilizing medium resolution imagery, from contemporary (2004; 20 m SPOT®) - and past (late 90’s - early 00’s; 30 m Landsat 7) – epochs for that purpose (Figures 1 and 2). The latter imagery is the basis of the NLCD01 imperviousness and canopy closure datasets (http://kls.ky.gov) (Yang et al., 2002). The goal of this paper is to present preliminary results of on-going, forward-change detection efforts, quantifying temporal change patterns in imperviousness in the vicinity of Lexington, KY. A subset of imagery where change in imperviousness was assessed to be minimal between ca. 2000 and 2004 was used as training for the classification and regression tree procedure (CART tools for ERDAS® Imagine® 8.7 and RuleQuest®’s Cubist®) applied to the 20 m, 4 band SPOT® imagery, resampled to 30 m. The result was a 2004, 30 m imperviousness dataset, which was then subtracted from and made relative to the earlier data (Figure 3). This change “mask” is used next to locate areas of potentially sizable imperviousness change. References.
正向变化检测2000 - 2004:肯塔基州列克星敦的城市扩张和不渗透
随着时间的推移,土地覆盖的变化可能会改变景观中不透水性的分布,由于水量和水质参数的退化,可能会对流域产生负面影响(schueller, 1994)。不透水性通常与城市和郊区增长相关,并被用作一个强有力的指标,作为“发达”安德森II级(低、中、高、开放)的代理。该分类方案是构建2001年国家土地覆盖数据集(NLCD01)和2001年肯塔基州土地覆盖数据集(KLCD01)的工作范式(http://kls.ky.gov;http://landcover.usgs.gov/index.asp)。肯塔基州景观快照项目的当前阶段需要开发一个变化检测组件。在这个阶段,工作围绕着利用中等分辨率的图像,从当代(2004;20米SPOT®)-和过去(90年代末- 00年代初;后者的图像是NLCD01不透水性和冠层封闭数据集的基础(http://kls.ky.gov) (Yang et al., 2002)。本文的目的是展示正在进行的,前瞻性变化检测工作的初步结果,量化肯塔基州列克星敦附近不透水性的时间变化模式。在大约2000年至2004年期间,不渗透变化被评估为最小的图像子集被用作分类和回归树程序的训练(用于ERDAS®Imagine®8.7和RuleQuest®的Cubist®的CART工具),应用于20米,4波段SPOT®图像,重新采样到30米。结果是2004年的30米不透水数据集,然后将其从早期数据中减去并相对于早期数据(图3)。接下来使用这种变化“掩码”来定位可能出现较大不透水变化的区域。参考文献
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