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Ninth International Conference on Permafrost ... - IARC Research

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Ni n t h In t e r n at i o n a l Co n f e r e n c e o n Pe r m a f r o s tResultsAn example illustrating the c<strong>on</strong>cept, from the North Slopeof Alaska, using TM, ETM and ALI data, in c<strong>on</strong>juncti<strong>on</strong>with topographic data to develop our object-based modelhas been undertaken. This analysis was c<strong>on</strong>ducted by firstprocessing the data within ENVI (by ITT visual informati<strong>on</strong>soluti<strong>on</strong>s) to retrieve surface reflectance values and toregister the datasets into a comm<strong>on</strong> reference system. Theresults were then imported into Definiens Pro (by DefiniensAG) for segmentati<strong>on</strong> and classificati<strong>on</strong> based <strong>on</strong> knownsurface units such as moist acidic tundra or moist n<strong>on</strong>acidictundra (~18 classes total). The results of this segmentati<strong>on</strong>appear to produce objects that corresp<strong>on</strong>d well to what haspreviously been established; however, further work is neededin characterizing class definiti<strong>on</strong>s.By using self-organized manifold learning (SOMs, anunsupervised Artificial Neural Network paradigm), wealso clustered a 9-band multispectral image from the ALIinstrument. Details of this technique, capabilities, andformer analyses are summarized in Merényi et al. (2007)and references therein. We separated 30 different vegetative,soil, and landscape units al<strong>on</strong>g the Dalt<strong>on</strong> Highway in theToolik Lake area. These include various water bodies withdifferent sediment loads, glacial ice, snow, a variety of soilsand vegetati<strong>on</strong>. Detailed interpretati<strong>on</strong> is <strong>on</strong>going. Thisunsupervised segmentati<strong>on</strong> serves to support a detailedsupervised classificati<strong>on</strong>.Point-source soils (ped<strong>on</strong>) data and field spectrometry datahave also been acquired at different units to provide groundtruth for the satellite image interpretati<strong>on</strong>.C<strong>on</strong>clusi<strong>on</strong>s and Future WorkPrevious studies c<strong>on</strong>ducted have utilized datasets thatwere largely moderate spatial and low spectra resoluti<strong>on</strong>.This study is employing datasets that are also moderatespatial resoluti<strong>on</strong>, but will be reinforced with high spectralresoluti<strong>on</strong> data, resulting in a more accurate assessment ofthe surface materials and increased c<strong>on</strong>fidence in the model.Additi<strong>on</strong>ally, by implementing a segmentati<strong>on</strong> of the datasets,it is possible to utilize textual and c<strong>on</strong>textual informati<strong>on</strong>that can be lost in pixel-based classificati<strong>on</strong>s (Blaschke &Strobl 2001). This type of processing also allows for a moreautomated processing scheme that can facilitate an efficienttemporal study and produce datasets that have underg<strong>on</strong>e thesame processing steps with little room for human error. Thisdecreases the amount of time it takes to run an analysis andincreases c<strong>on</strong>fidence in the model. Preliminary results haveshown that image segmentati<strong>on</strong> through a texture-based,object-oriented approach yields landscape unit geometriesthat appear to correlate well with previously c<strong>on</strong>ductedaerial photograph analysis undertaken in the regi<strong>on</strong> (Walker1996).Field spectral measurements, collected over major landcovertypes, indicate that the spectral differences betweendifferent landscape units are often minor. Based <strong>on</strong> highdimensi<strong>on</strong>alintricate signatures, hyperspectral data couldprovide material discriminati<strong>on</strong>, even in cases of many classeswith potentially subtle spectral distincti<strong>on</strong>s. Exploitati<strong>on</strong> ofthese types of data is a great challenge in itself, both fordiscovery (unsupervised clustering) and for mapping knownspecies (supervised classificati<strong>on</strong>). Fused with other data,this challenge increases. Analysis of hyperspectral imageryresides in our l<strong>on</strong>g-term goals, and we hope to report <strong>on</strong>those at a later date.AcknowledgmentsEM is partially supported by the AISRP (grantNNG05GA94G) of NASA’s SMD. BB is supported byNASA GSRP graduate fellowship NNX0AR79H. BC andJR are supported by NASA’s ICESat program.ReferencesBlaschke, T. & Strobl, J. 2001. What’s wr<strong>on</strong>g with pixels?Some recent developments interfacing remote sensingand GIS. GIS Zeitschrift fur Geoinformati<strong>on</strong>ssystme6(11): 12-17.Burnett, C. & Blaschke, T. 1994. A multi-scale segmentati<strong>on</strong>/object relati<strong>on</strong>ship modeling methodology forlandscape analysis. Ecological Modeling 31: 737-747.Darwish, A. et al. 2003. Image Segmentati<strong>on</strong> for the PurposeOf Object-Based Classificati<strong>on</strong>. Geoscience andRemote Sensing Symposium, 2003. IGARSS ’03.Proceedings. 2003 IEEE <str<strong>on</strong>g>Internati<strong>on</strong>al</str<strong>on</strong>g> 3: 2039-2041.Merényi, E., Farrand, W.H., Brown, R.H., Villmann, Th. &Fyfe, C. 2007. Informati<strong>on</strong> extracti<strong>on</strong> and knowledgediscovery from high-dimensi<strong>on</strong>al and high-volumecomplex data sets through precisi<strong>on</strong> manifoldlearning, Proc. NASA Science Technology <str<strong>on</strong>g>C<strong>on</strong>ference</str<strong>on</strong>g>(NSTC2007), College Park, Maryland, June 19–21,2007: 11pp. ISBN 0-9785223-2-X.Walker, D.A. 1996. GIS data from the Alaska North Slope.Nati<strong>on</strong>al Snow and Ice Data Center (Digital Media).Accessed 3-15-07.254

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