Error processes in the integration of digital cartographic data in geographic information systems.

Errors within a Geographic Information System (GIS) arise from several factors. In the first instance receiving data from a variety of different sources results in a degree of incompatibility between such information. Secondly, the very processes used to acquire the information into the GIS may in fact degrade the quality of the data. If geometric overlay (the very raison d'etre of many GISs) is to be performed, such inconsistencies need to be carefully examined and dealt with. A variety of techniques exist for the user to eliminate such problems, but all of these tend to rely on the geometry of the information, rather than on its meaning or nature. This thesis explores the introduction of error into GISs and the consequences this has for any subsequent data analysis. Techniques for error removal at the overlay stage are also examined and improved solutions are offered. Furthermore, the thesis also looks at the role of the data model and the potential detrimental effects this can have, in forcing the data to be organised into a pre-defined structure

Fault specific GIS based seismic hazard maps for the Attica Region, Greece

Traditional seismic hazard assessment methods are based on the historical seismic records for the calculation of an annual probability of exceedance for a particular ground motion level. A new fault specific seismic hazard assessment method is presented, in order to address problems related to the incompleteness and the inhomogeneity of the historical records and to obtain higher spatial resolution of hazard. This method is applied to the region of Attica, which is the most densely populated area in Greece, as nearly half of the country’s population lives in Athens and its surrounding suburbs, in Greater Athens Area. The methodology is based on a database of 22 active faults that could cause damage to Attica in case of seismic rupture. This database provides information about the faults slip rates, lengths and expected magnitudes. The final output of this method are four fault specific seismic hazard maps, showing the recurrence of expected intensities that each locality in the map has been shaken at. These maps offer a high spatial resolution, as they consider the surface geology. Despite the fact that almost half of the Attica region lies on the lowest seismic risk zone according to the official seismic hazard zonation of Greece, different localities have repeatedly experienced strong ground motions during the last 15 kyrs. Moreover, the maximum recurrence for each intensity occurs in different localities across Attica. Highest recurrence for intensity VII (151-156 times over 15 kyrs, or up to 96 year return period) is observed in the central part of the Athens basin. The maximum intensity VIII recurrence (114 times over 15 kyrs, or up to 131 year return period) is observed in the western part of Attica, while the maximum intensity IX (73-77/15kyrs, or 195 year return period) and X (25-29/15kyrs, or 517 year return period) recurrences are observed near the South Alkyonides fault system, which dominates the strong ground motions hazard in the western part of the Attica mainland

Developing Guidelines for Two-Dimensional Model Review and Acceptance

Two independent modelers ran two hydraulic models, SRH-2D and HEC-RAS 2D. The models were applied to the Lakina River (MP 44 McCarthy Road) and to Quartz Creek (MP 0.7 Quartz Creek Road), which approximately represent straight and bend flow conditions, respectively. We compared the results, including water depth, depth averaged velocity, and bed shear stress, from the two models for both modelers. We found that the extent and density of survey data were insufficient for Quartz Creek. Neither model was calibrated due to the lack of basic field data (i.e., discharge, water surface elevation, and sediment characteristics). Consequently, we were unable to draw any conclusion about the accuracy of the models. Concerning the time step and the equations used (simplified or full) to solve the momentum equation in the HEC-RAS 2D model, we found that the minimum time step allowed by the model must be used if the diffusion wave equation is used in the simulations. A greater time step can be used if the full momentum equation is used in the simulations. We developed a set of guidelines for reviewing model results, and developed and provided a two-day training workshop on the two models for ADOT&PF hydraulic engineers

Comparing Nonlinear and Nonparametric Modeling Techniques for Mapping and Stratification in Forest Inventories of the Interior Western USA

Recent emphasis has been placed on merging regional forest inventory data with satellite-based information both to improve the efficiency of estimates of population totals, and to produce regional maps of forest variables. There are numerous ways in which forest class and structure variables may be modeled as functions of remotely sensed variables, yet surprisingly little work has been directed at surveying modem statistical techniques to determine which tools are best suited to the tasks given multiple objectives and logistical constraints. Here, a series of analyses to compare nonlinear and nonparametric modeling techniques for mapping a variety of forest variables, and for stratification of field plots, was conducted using data in the Interior Western United States. The analyses compared four statistical modeling techniques for predicting two discrete and four continuous forest inventory variables. The modeling techniques include generalized additive models (GAMs), classification and regression trees (CARTs), multivariate adaptive regression splines (MARS), and artificial neural networks (ANNs). Alternative stratification schemes were also compared for estimating population totals. The analyses were conducted within six ecologically different regions using a variety of satellite-based predictor variables. The work resulted in the development of an objective modeling box that automatically models spatial response variables as functions of any assortment of predictor variables through the four nonlinear or nonparametric modeling techniques. In comparing the different modeling techniques, all proved themselves workable in an automated environment, though ANNs were more problematic. When their potential mapping ability was explored through a simple simulation, tremendous advantages were seen in use of MARS and ANN for prediction over GAMs, CART, and a simple linear model. However, much smaller differences were seen when using real data. In some instances, a simple linear approach worked virtually as well as the more complex models, while small gains were seen using more complex models in other instances. In real data runs, MARS performed (marginally) best most often for binary variables, while GAMs performed (marginally) best most often for continuous variables. After considering a subjective ease of use measure, computing time and other predictive performance measures, it was determined that MARS had many advantages over other modeling techniques. In addition, stratification tests illustrated cost-effective means to improve precision of estimates of forest population totals. Finally, the general effect of map accuracy on the relative precision of estimates of population totals obtained under simple random sampling compared to that obtained under stratified random sampling was established and graphically illustrated as a tool for management decisions

Microscopic tunneling experiments on atomic impurities in graphene and on magnetic thin films

This thesis presents investigations on hydrogenated graphene by scanning tunneling microscopy and spectroscopy (STM/STS) as well as the implementation of spin-polarized STM. Preparation processes for a magnetic standard sample and spin-sensitive chromium tips are developed. The measurements on graphene reveal specific hydrogen adsorption sites in low coverage and the formation of a pattern at higher coverage. Both is found to be in agreement with previous predictions and calculations. Upon hydrogenation, an impurity midgap state emerges in the density of states which is measured directly for the first time. Complementing angle resolved photoemission experiments confirm that this state is dispersionless over the whole Brillouin zone. A routine is developed to prepare the standard sample system of ultra-thin iron films on tungsten (Fe/W(110)). Investigations on this system confirm the magnetic properties known from literature, including the presence of a spin spiral, and prove that it is well suited for the characterization of spin-polarized tips. Different approaches for the preparation of tips from the antiferromagnetic material chromium are tested. Among these, a promising new method is presented: The coating of crystalline chromium tips with fresh chromium material suggests reproducibility of the tip characteristics. The performance of the produced tips in STM measurements is excellent in regard to a fixed spin-polarization, high resolution and stability. Especially, a recovery of the tip magnetization direction proposed in this thesis makes this new preparation method superior to all processes yielding antiferromagnetic tips reported so far.:1 Introduction 2 Basics 2.1 Scanning tunneling microscopy 2.2 Spin-polarized STM – access to magnetic information 2.3 Measurement setup 3 Probing local hydrogen impurities in quasi-free-standing graphene 3.1 Functionalization of graphene 3.2 In-situ fabrication of quasi-free-standing graphene and its functionalization 3.3 Interpretation of the results 3.4 Short summary 4 Chromium tips for spin-polarized tunneling experiments 4.1 Magnetism at the nanoscale 4.2 Growth and properties of Fe/W(110) 4.3 Preparation of tips with outstanding properties 4.4 Short summary 5 Summary and outlookInhalt der vorliegenden Arbeit sind Untersuchungen von hydogeniertem Graphen mittels Rastertunnelmikroskopie und -spektroskopie (RTM/RTS) sowie die Einführung spin-polarisierter RTM. Im Rahmen dessen wurden Präparationsprozesse für magnetische Standardproben und spin-sensitive Chrom-Spitzen entwickelt. Die Messungen an Graphen zeigen spezifische Wasserstoff-Adsorptionsstellen bei geringer Bedeckung und die Ausbildung eines Musters bei höherer Bedeckung, jeweils in Übereinstimmung mit Vorhersagen und Berechnungen. Der durch Hydrogenierung entstehende Störstellenzustand in der Bandlücke der Zustandsdichte wurde zum ersten Mal direkt gemessen. Ergänzende winkelaufgelöste Photoelektronenspektroskopieexperimente bestätigen, dass dieser Zustand in der gesamten Brillouinzone dispersionsfrei ist. Ein Verfahren zur Herstellung magnetischer Standardproben aus ultradünnen Eisenfilmen auf Wolfram (Fe/W(110)) wurde entwickelt. RTM-Untersuchungen an diesem System bestätigen die bereits aus der Literatur bekannten magnetischen Eigenschaften, insbesondere das Vorhandensein einer Spinspirale. Damit ist Fe/W(110) hervorragend geeignet für die Charakterisierung spin-polarisierter Spitzen. Verschiedene Ansätze, die zur Herstellung von Spitzen aus dem antiferromagnetischen Material Chrom verfolgt wurden, werden präsentiert, darunter auch eine vielversprechende neue Methode: Das Aufwachsen eines frischen Chromfilms auf kristalline Spitzen desselben Materials verspricht eine Reproduzierbarkeit von Spitzeneigenschaften. Der Einsatz von so hergestellten Spitzen in RTMMessungen ist geprägt von einer festgelegten Spin-Polarisation, hohem Auflösungsvermögen und Stabilität. Insbesondere die mögliche Reproduzierbarkeit der Magnetisierungsrichtung, die in dieser Arbeit diskutiert wird, macht diese Methode allen bisher berichteten Herstellungprozessen antiferromagnetischer Spitzen überlegen.:1 Introduction 2 Basics 2.1 Scanning tunneling microscopy 2.2 Spin-polarized STM – access to magnetic information 2.3 Measurement setup 3 Probing local hydrogen impurities in quasi-free-standing graphene 3.1 Functionalization of graphene 3.2 In-situ fabrication of quasi-free-standing graphene and its functionalization 3.3 Interpretation of the results 3.4 Short summary 4 Chromium tips for spin-polarized tunneling experiments 4.1 Magnetism at the nanoscale 4.2 Growth and properties of Fe/W(110) 4.3 Preparation of tips with outstanding properties 4.4 Short summary 5 Summary and outloo