Thesis--Rheinische Friedrich-Wilhelms-Universität Bonn, 1996. / Includes bibliographical references (p. 317-327).

Thesis (M.S.)--Brigham Young University. Dept. of Geological Sciences, 2008. / Includes bibliographical references.

The entire thesis text is included in the research.pdf file; the official abstract appears in the short.pdf file; a non-technical public abstract appears in the public.pdf file. Title from PDF of title page (University of Missouri--Columbia, viewed on October 16, 2009). Thesis advisor: Dr. Richard P. Guyette. Includes bibliographical references.

Thesis (M. A.)--Florida State University, 2005. / Advisor: Dr. Frederick R. Davis, Florida State University, College of Arts and Sciences, Dept. of History. Title and description from dissertation home page (viewed Sept. 15, 2005). Document formatted into pages; contains v, 81 pages. Includes bibliographical references.

Thesis (M.S.)--Southern Oregon University, 2006. / Includes bibliographical references (leaves 88-93). Also available via Internet as PDF file through Southern Oregon Digital Archives: http://soda.sou.edu. Search Bioregion Collection.

With an increasing number of large area data sets, many study areas exhibit spatial non-stationarity or spatial variation in mean and variance of observed phenomena. This poses issues for a number of spatial analysis methods which assume data are stationary. The Getis and Ord’s Gi* statistic is a popular measure that, like many others, is impacted by non stationarity. The Gi* is used for locating hot and cold spots in marked data through the detection of spatial autocorrelation in values that are extreme relative to the global mean value, or the mean entire study area. This thesis describes modifications of the Getis and Ord’s Gi* local measure of spatial association, in part to account for regional differences (spatial non-stationarity) in a dataset. Instead of using data from the entire study area to calculate the mean parameter, as is done for the standard Gi*, I capture points for calculation of the mean using a circular distance band centred on the pivot location, which I call the local region (similar to the Ord and Getis Oi statistic). This approach can be applied to a single instance of a local region or to multiple spatial scales of the local region. I explore both in this paper using simulated datasets and a case study on mountain pine beetle infestation data. I find that the local region, when of a similar size to a true region (homogeneous section of the study area where the mean is approximately the same across locations), obtains similar results to the standard Gi* calculated separately on distinct regions (simulated to be distinct), but has the advantage of not needing explicit delineation of regional boundaries or partitioning into separate subareas. The results of a probability score for a multi-scale approach include high and low scores that are more evenly distributed across the study area and that are thus able to pick out more subtle variations within different regions. Through the case study I demonstrate how the multi-scale approach may be applied to a real dataset.

Την 8η Ιουνίου 2008, στις 15:25 τοπική ώρα (12:25 GMT) ένας σεισμός μεγέθους Mw 6.4 εκδηλώθηκε στη ΒΔ Πελοπόννησο, στη Δυτική Ελλάδα. Το επίκεντρο προσδιορίστηκε κοντά στο χωριό Μιχόι, στη Δημοτική Ενότητα Μόβρης, περίπου 35 km ΝΔ της Πάτρας. Στην παρούσα εργασία, έγινε μία μελέτη ανισοτροπίας στην επικεντρική περιοχή του σεισμού της 8ης Ιουνίου. Συγκεκριμένα, έγινε μία μελέτη για την ανίχνευση του φαινομένου διαχωρισμού των εγκαρσίων κυμάτων και της εξέλιξής του σε σχέση με την εκδήλωση του σεισμού της 8ης Ιουνίου. Χρησιμοποιήθηκαν οι καταγραφές από τον σεισμολογικό σταθμό του Ριόλου (RLS), καθώς είναι ο μόνος κοντινός σταθμός στο επίκεντρο του σεισμού της 8ης Ιουνίου που βρισκόταν σε συνεχή λειτουργία κατά τα χρονικά διαστήματα πριν και μετά την εκδήλωση του σεισμού. Για τη μελέτη του φαινομένου του διαχωρισμού των εγκαρσίων κυμάτων χρησιμοποιήθηκε η μέθοδος cross-correlation (Ando et al., 1983; Fukao, 1984). Μετά την επεξεργασία των δεδομένων, προσδιορίστηκαν οι παράμετροι του φαινομένου, φ (διεύθυνση ταλάντωσης της ταχύτερης συνιστώσας των εγκαρσίων κυμάτων) και dt (χρόνος καθυστέρησης μεταξύ των δύο συνιστωσών) για κάθε ένα σεισμικό γεγονός. Ο διαχωρισμός των εγκαρσίων κυμάτων (shear-wave splitting) είναι ένα φαινόμενο κατά το οποίο, τα εγκάρσια κύματα διαχωρίζονται σε δύο συνιστώσες, με διαφορετικές διευθύνσεις πόλωσης και διαφορετικές ταχύτητες διάδοσης. Ο διαχωρισμός αυτός πραγματοποιείται κατά την διάδοση των εγκαρσίων κυμάτων μέσα από ένα ανισοτροπικό μέσο (Crampin and Chastin, 2003; Crampin and Peacock, 2005). Σύμφωνα με τη θεωρία, ο διαχωρισμός των εγκαρσίων κυμάτων στον φλοιό, προκαλείται εξαιτίας της ύπαρξης μικρο-ρωγμών, μικρο-διαρρήξεων κορεσμένων με ρευστά. Οι μικρο-διαρήξεις αυτές έχουν συνήθως διευθύνσεις παράλληλες ή υπό-παράλληλες με αυτή της μέγιστης οριζόντιας συμπιεστικής τάσης σε μία περιοχή (Crampin, 1993). Η ανάλυση των δεδομένων κατέδειξε την ύπαρξη του φαινομένου διαχωρισμού των εγκαρσίων κυμάτων στην υπό μελέτη περιοχή. Τόσο πριν, όσο και μετά την εκδήλωση του σεισμού της 8ης Ιουνίου, οι διευθύνσεις πόλωσης της ταχύτερης συνιστώσας των εγκαρσίων κυμάτων ακολουθούν μία μέση διεύθυνση ΒΒΔ-ΝΝΑ. Η μέση διεύθυνση της ταχύτερης συνιστώσας δεν είναι σύμφωνη με τα χαρακτηριστικά του πεδίου των τάσεων στην περιοχή, όπως προσδιορίστηκαν από τους Konstantinou et al. (2011) και Hollenstein et al. (2008), με μία μέση διεύθυνση οριζόντιας συμπιεστικής τάσης Α-Δ. Η ΒΒΔ-ΝΝΑ διεύθυνση πόλωσης της ταχύτερης συνιστώσας οφείλεται πιθανόν στη δράση ενός πεδίου τάσεων γύρω και κάτω από τη θέση καταγραφής με τοπικά χαρακτηριστικά. Τέλος, παρατηρήθηκε μία αύξηση στις τιμές των χρόνων καθυστέρησης μετά την εκδήλωση του σεισμού της 8ης Ιουνίου. Η μέση τιμή των χρόνων καθυστέρησης πριν την εκδήλωση του σεισμού ήταν περίπου 27.3 ms, ενώ μετά την εκδήλωσή του 41.7 ms. H αύξηση των χρόνων καθυστέρησης, υποδηλώνει μία μεταβολή των ιδιοτήτων του μέσου στον ανώτερο φλοιό εξαιτίας της εκδήλωσης του σεισμού. Η εκδήλωση του σεισμού της 8ης Ιουνίου προκάλεσε πιθανόν την διεύρυνση και την επιμήκυνση των προϋπαρχόντων μικρο-διαρρήξεων του φλοιού, τη δημιουργία νέων και την επιπλέον πλήρωσή τους με ρευστά. / On June 8, 2008, at 15:25 local time (12:25 GMT) an Mw 6.4 earthquake occurred in the area of northwest Peloponnesus, Western Greece. The epicenter was located near Mihoi village, in the municipality of Movri, about 35 km southwest of Patras. In this paper, a crustal anisotropy analysis was performed in the epicentral area of Movri Mountain earthquake. Specifically, there was a study to detect shear-wave splitting phenomenon and its temporal evolution in relation to the occurrence of Movri Mountain earthquake. For the needs of the study, we used seismic records from the seismological station of Riolos (RLS). Riolos station is the nearest station from the epicenter of Movri Mountain earthquake which was in continuous operation during the periods before and after the occurrence of the earthquake. The method that was used to study shear-wave splitting phenomenon was the cross-correlation method (Ando et al., 1983; Fukao, 1984; Kuo et al., 1994). Through the data processing, splitting parameters φ (polarization direction of the fastest component of shear waves) and dt (time delay between the two components) were measured for each seismic event. Shear-wave splitting is a phenomenon in which shear-waves are separated into two components with different polarization directions and velocities. The phenomenon in the upper crust is caused by the existence of stress-aligned, fluid-filled micro-cracks/micro-fractures. The polarization directions of the fast components are usually parallel or sub-parallel to the direction of the maximum horizontal compressive stress (Crampin, 1993). Data analysis revealed the existence of shear-wave splitting phenomenon in the study area. Both before and after the occurrence of Movri Mountain earthquake, the polarization directions of the fast component of shear waves follow a general NNW-SSE direction. The observed mean fast polarization direction is not consistent with the estimated characteristics of the regional stress field of the broader area, as identified by Kontsantinou et al. (2011) and Hollenstein et al. (2008), who report a general E-W direction of the maximum horizontal compressive stress. The difference between the estimated fast polarization directions and the properties of the regional stress field shows the presence of a local stress field in the study area. Finally, an increase in time delays was observed after the occurrence of Movri Mountain earthquake. The average value of delay times before the occurrence of the earthquake was about 27.3ms, while after the occurrence was about 41.7ms. The increase in delay times which was observed after the occurrence of Movri Mountain earthquake possibly indicates changes in the properties of the medium in the upper crust. The occurrence of Movri Mountain earthquake caused the expansion/ lengthening of micro-cracks and its further filling with fluids.

Alpine valleys are rarely closed systems, implying that the atmospheric boundary layer of a particular valley section is influenced by the surrounding terrain and large-scale flows. A detailed characterisation and quantification of these effects is required in order to design appropriate parameterisation schemes for complex terrains. The focus of this work is to improve the understanding of the effects of surrounding terrain (plains, valleys or tributaries) on the heat and mass budgets of the stable boundary layer of a valley section, under dry and weak large-scale wind conditions. Numerical simulations using idealised and real frameworks are performed to meet this goal. Several idealised terrains (configurations) were considered: an infinitely long valley (i.e. two-dimensional), and upstream valleys opening either on a plain (valley-plain), on a wider valley (draining) or on a narrower valley (pooling). In three-dimensional valleys, two main regimes can be identified for all configurations: a transient regime, before the down-valley flow develops, followed by a quasi-steady regime, when the down-valley flow is fully developed. The presence of a downstream valley reduces the along-valley temperature difference, therefore leading to weaker down-valley flows. As a result, the duration of the transient regime increases compared to the respective valley-plain configuration. Its duration is longest for the pooling configuration. For strong pooling the along-valley temperature difference can reverse, forcing up-valley flows from the narrower towards the wider valley. In this regime, the average cooling rate at the valley-scale is found to be a maximum and its magnitude is dependent on the configuration considered. Therefore pooling and draining induce colder and deeper boundary layers than the respective valley-plain configurations. In the quasisteady regime the cooling rate is smaller than during the transient regime, and almost independent of the configuration considered. Indeed, as the pooling character is more pronounced, the warming contribution from advection to the heat budget decreases because of weaker down-valley flows, and so does the cooling contribution from the surface sensible heat flux. The mass budget of the valley boundary layer was found to be controlled by a balance between the convergence of downslope flows at the top of the boundary layer and the divergence of the down-valley flow along the valley axis, with negligible contributions of subsidence far from the valley sidewalls. The mass budget highlighted the importance of the return current above the down-valley flow, which may contribute significantly to the inflow of air at the top of the boundary layer. A case-study of a persistent cold-air pool event which occurred in February 2015 in the Arve River Valley during the intensive observation period 1 (IOP1) of the PASSY- 2015 field campaign, allowed us to quantify the effects of neighbouring valleys on the heat and mass budgets of a real valley atmosphere. The cold-air pool persisted as a result of warm air advection at the valley top, associated with the passage of an upper-level ridge over Europe. The contributions from each tributary valley to the mass and heat budgets of the valley atmosphere were found to vary from day to day within the persistent stage of the cold-air pool, depending on the large-scale flow. Tributary flows had significant impact on the height of the inversion layer and the strength of the cold-air pool, transporting a significant amount of mass within the valley atmosphere throughout the night. The strong stratification of the near-surface atmosphere prevented the tributary flows from penetrating down to the valley floor. The evolution of the large-scale flow during the episode had a profound impact on the near-surface circulation of the valley. The channelling of the large-scale flow at night, can lead to the decrease of the horizontal temperature difference driving the near-surface down-valley flow, favouring the stagnation of the air close to the ground.

Depuis les années 1980, de nombreuses études ont montré l’importance des peuplements forestiers très matures et de leurs attributs constitutifs (arbres de gros diamètre, bois morts…) pour la conservation de la biodiversité forestière. Ces travaux ont permis d’initier un processus en faveur d’une meilleure reconnaissance de la fonction écologique des forêts. La plupart de ces études ne tiennent cependant pas compte de la notion d’ancienneté des forêts, i.e. de la continuité temporelle de l’état boisé. Cette notion apparaît pourtant pertinente pour expliquer la répartition de certaines espèces. Ainsi, une forêt ancienne, même rajeunie par une perturbation, pourrait jouer un rôle pour la conservation de la biodiversité tout aussi important qu’une forêt récente constituée de peuplements très matures. Cette relation a priori contrastée entre biodiversité et maturité d’une part et biodiversité et ancienneté d’autre part, soulève de nombreuses questions quant aux choix stratégiques à mettre en place pour une conservation et une gestion optimale de la biodiversité en forêts. Plus généralement, ces notions permettent de questionner l’influence relative des activités humaines passées et actuelles sur la biodiversité forestière. Afin de préciser les effets relatifs de l’ancienneté et de la maturité sur la biodiversité, une approche combinant géohistoire et sciences de l’environnement a été mise en place. Un dispositif d’étude de 70 sites, croisant des forêts anciennes ou récentes avec des peuplements peu matures ou très matures, a été développé dans les Préalpes francçaises (Vercors, Chartreuse et Bauges). Pour chacun des sites, l’ancienneté et la maturité ont été caractérisées et quatre groupes taxinomiques ont été inventoriés : flore vasculaire, coléoptères saproxyliques, collemboles et macrolichens épiphytes. Nos résultats indiquent une absence flagrante d’effet d’héritage dû aux usages passés, à la fois dans les sols et sur la biodiversité. Les espèces étaient avant tout influencées par la maturité des peuplements, notamment la diversité des bois morts pour les coléoptères saproxyliques et l’ouverture de la canopée pour la flore vasculaire. Le sol, à travers le pH et les formes d’humus, avait également un rôle structurant fort sur la flore vasculaire et les collemboles, et le climat, à travers les températures, sur les coléoptères saproxyliques. Cet effet limité de l’ancienneté, comparativement aux études antérieures, est à mettre en relation avec le contexte écologique, paysager et historique des forêts de montagne : fort taux de boisement, forte proportion de forêts anciennes, surfaces boisées peu fragmentées, usage ancien peu impactant et gestion forestière actuelle assez extensive. Nos résultats montrent ainsi que l’effet des usages anciens sur la biodiversité dépend fortement du contexte. Ils soulignent l’importance de la prise en compte des conditions environnementales locales, attributs de maturité mais aussi conditions climatiques et édaphiques, pour une compréhension plus fine des patrons de biodiversité en forêts de montagne / Since the 1980s, numerous studies had shown the importance of stand maturity, especially old-growth habitat features (very large trees, deadwood…) for forest biodiversity conservation. This work led to a better recognition of the ecological function of forests. However, most of these studies do not take account of forest continuity, i.e. the temporal continuity in forested condition. Forest continuity has been used to explain some species distribution. Therefore, ancient forests, even rejuvenated by disturbances, may be of greater conservation interest for biodiversity than recent forests composed of overmature stands. This a priori contrasting relationship between biodiversity and stand maturity on the one hand and biodiversity and forest continuity on the other hand, raises many questions about the most appropriate policy choices to conserve and manage adequately forest biodiversity. More generally, these concepts allow the questioning of the relative influence of past and present human-induced environmental changes on forest biodiversity. To clarify the relative effects of forest continuity and stand maturity on biodiversity, we developed an approach in which we combined historical ecology and environmental sciences. We established 70 sites in the French Prealps (Vercors, Chartreuse and Bauges) in which we crossed ancient or recent forests with mature or overmature stands. For each site we characterized forest continuity and stand maturity and assessed the response of four taxonomic groups: vascular plants, saproxylic beetles, springtails and epiphytic macrolichens. Results showed an obvious lack of legacy effect on both soil conditions and biodiversity. Species were above all influenced by stand maturity, especially deadwood diversity for saproxylic beetles and canopy openness for vascular plants. Soil conditions, through pH and humus forms, had also a great structuring role on vascular plants and springtails, and climatic conditions, through temperature, on saproxylic beetles. Comparatively to previous studies, this quite limited effect of forest continuity can be linked with the ecological, landscape and historical context of mountain forests: high percentage of forest cover, high proportion of ancient forests, low-fragmented wooded areas, past land use being low impacting and current extensive forest management. Overall, our results show that the effect of forest continuity on biodiversity is context dependent and underline the necessity to better account for local environmental conditions, stand maturity attributes but also climatic and edaphic conditions, to improve our understanding of biodiversity patterns in mountain forests

abstract: ABSTRACT The elephant tree, Bursera microphylla, is at the northern limit of its range in central Arizona. This species is sensitive to frost damage thus limiting its occurrence in more northern areas of the southwest. Marginal populations of B. microphylla are found in mountain ranges of Central Arizona and are known to occur in the rugged mountain range system of the South Mountain Municipal Park (SMMP). Little is known of the distribution of this species within the park and details relevant to the health of both individual plants and the population such as diameter and number of trunks, height, and presence of damage have not been examined. This study was designed, in part, to test the hypothesis that favorable microhabitats at SMMP are created by particular combinations of abiotic features including aspect, slope, elevation and solar radiation. Data on abiotic factors, as well as specific individual plant locations and characteristics were obtained for 100 individuals. Temperature data was collected in vertical transects at different altitudinal levels. Some of these data were used in spatial analyses to generate a habitat suitability model using GIS software. Furthermore, collected data was analyzed using Matlab© software to identify potential trends in the variation of morphological traits. In addition, for comparative purposes similar information at one hundred computer-generated randomly chosen points throughout SMMP was obtained. The GIS spatial analyses indicated that aspect, slope, elevation, and relative solar radiance are strongly associated as major climatic components of the microhabitat of B. microphylla. Temperature data demonstrated that there are significant differences in ambient temperature among different altitudinal gradients with middle elevations being more favorable. Furthermore, analyses performed using Matlab© to explore trends of elevation as a factor indicated that multiple trunk plants are more commonly found at higher elevations than single trunk plants, there is a positive correlation of trunk diameter with elevation, and that canopy volume has a negative correlation with respect to elevation. It was concluded that microhabitats where B. microphylla occurs at the northern limit of its range require a particular combination of abiotic features that can be easily altered by climatic changes. / Dissertation/Thesis / M.S. Applied Biological Sciences 2011