Water quality data and land use information were analyzed within the Alafia River watershed in Florida to determine spatial and temporal trends in these variables over a 16 year time period from 1991-2006. Monthly water quality data (for dissolved oxygen, turbidity, fecal coliform, total phosphorus, and total nitrogen) were statistically analyzed using the modified seasonal Kendall nonparametric test for trends that accounts for serial correlation. The statistical trend analysis was conducted for the entire study period, but monthly, seasonal, and land use trends were also examined. Land use information was examined using Geographic Information Systems to determine the percent change in land use proportion from 1990 to 1999, 1999 to 2006, and 1990 to 2006. The proportions of each land use and their percent change were then related to the trends in water quality. The results of this analysis showed that water quality for the parameters turbidity and total phosphorus have been shown to be improving with statistically significant decreasing trends for turbidity at stations 74, 111, 116, and 139 and for total phosphorus at stations 74, 114, and 115. A statistically significant decreasing trend in dissolved oxygen was determined for stations 116 and an increasing trend in total nitrogen for stations 114, 115, and 151 implying water quality for these parameters is degrading. Other noted trends were high fecal coliform and total nitrogen at station 111, which has higher proportions of agricultural land use and an increasing proportion of urban and built-up land use. Also, low dissolved oxygen was noted at station 74. The proportions of land use for the entire study area have changed from predominantly wetlands to now urban and built-up land use. While agricultural, rangeland, and wetlands land use have shown a reduction in the proportion of coverage in the contributing zone of almost every station, urban and built-up land use has increased in proportion at every station.

This thesis considers the problem of hypothesis testing for umbrella alternatives when there are two groups, or strata, of observations. The proposed methods extend a previously established general framework of hypothesis testing based on rankings to stratified datasets by first aligning the strata. The tests based on the Spearman and Kendall distances between ranking vectors lead to the traditional aligned-rank tests and new methods which account for “misalignment” under the alternative hypothesis. Asymptotic null distributions and simulation studies are given for the Spearman distance. Diagnostic tools for the misalignment issue are illustrated alongside the proposed tests on a dataset of IQ scores of coma patients. Extensions to three or more strata and ”adaptive” tests are provided as future research directions.

No description available.

In the southern of the Amazon basin, extensive deforestation associated with global climate change have impacted the regional water cycle. Predictions indicate that future alteration might cause even higher pressure over regional water resources. The goal of this study was to perform a detailed evaluation of past changes in the water resources of the upper Xingu basin, a region which is broadly representative of southern Amazon. The evaluation consisted of characterizing alterations in medium and long-term time series of rainfall, river discharge, evapotranspiration and total water storage change. The study employed not only in situ measurements, but also remotely sensed data. Remote sensing products including rainfall, evapotranspiration and water storage change were employed in the evaluation of the regional water balance. A thirteen years\' time series derived from RS products was submitted to a trend analysis, to detect significant variations in the water balance. Furthermore, uncertainties in each remote sensing product were retrieved, mostly comparing in situ measurements with RS estimates. To describe limitations of such products to evaluate the regional water balance, river discharge was calculated as the residual of the water balance. Later on, the estimated river discharge was compared to in situ measurements and uncertainties in the water balance were defined. The analysis of long-term alterations considered in situ measurements of rainfall and river discharge, from the period of 1976-2015. In this case, a group of hydro-climatological indicators was derived and then submitted to Mann-Kendall and Petit test. Due to the relevance of forest cover on river flow regulation, land use changes (LUC) were mapped every five years from 1985 to 2015. LUC results were then compared to the hydro-climatological data, to identify similarities in changing patterns. The evaluation of water balance components based on remote sensing products described fairly well the spatial variability in the study site. The uncertainties in P, ET and TWSC products corresponded to 41, 25 and 18 mm month-1, respectively. Due to these uncertainties, it was not possible to perform the water balance closure based on RS data. No significant changes were observed in the time series derived from these products. Contrastingly, the evaluation of a 40-years\' time series presented a decrease of 245 mm in rainfall, with intensity and number of rainy events being reduced. This phenomenon is most likely resultant from two process, the reduction in water recycling due to deforestation, as well as the Pacific Ocean decadal oscillation, which influences the large-scale atmospheric circulation. Although deforestation tends to increase river discharge, the reduction in rainfall in the Upper Xingu Basin was high enough to mask this effect. / O desmatamento em larga escala na região sul da bacia amazônica brasileira, associado às mudanças climáticas globais, tem impactado o ciclo hidrológico regional. Previsões futuras indicam uma pressão ainda maior sobre os recursos hídricos regionais. O objetivo deste estudo foi realizar uma avaliação detalhada das possíveis alterações nos recursos hídricos da bacia do Alto Xingu, uma região extremamente representativa do sul da Amazônia. Para tanto, foram empregadas séries temporais de longa e média duração, correspondentes à precipitação (P), vazão (Q), evapotranspiração (ET) e variação do armazenamento de água (TWSC). O estudo empregou medições in situ, bem como dados de sensoriamento remoto (SR). As estimativas de sensoriamento remoto foram empregadas na avaliação do balanço hídrico regional. As séries temporais de treze anos derivadas de produtos de SR foram submetidas a uma análise de tendência, com o objetivo de detectar variações significativas nos componentes do balanço hídrico. Além disso, as incertezas em cada produto foram obtidas comparando-se medições in situ com as estimativas de SR. Com o objetivo de descrever as limitações de tais produtos para a realização do balanço hídrico regional, a vazão do rio Xingu foi estimada com base na fórmula do balanço hídrico. Posteriormente, tal estimativa foi comparada com as medições in situ, gerando um indicativo da incerteza no fechamento do balanço hídrico. Já a análise das alterações a longo prazo considerou as medidas in situ da precipitação e vazão, no período de 1976-2015. Neste caso, um grupo de indicadores hidro-climatológicos foi calculado e posteriormente submetido aos testes de Mann-Kendall e Pettit. Devido à relevância das florestas na regulação da vazão dos rios, as mudanças no uso e ocupação da terra foram mapeadas a cada cinco anos, durante 1985-2015. Os resultados foram comparados aos dados hidro-climatológicos, buscando assim semelhanças nos padrões de alteração. Os produtos de sensoriamento remoto descreveram razoavelmente bem a variabilidade espacial dos componentes do balanço hídrico. As incertezas nas estimativas de P, ET e TWSC corresponderam a 41, 25 e 18 mm mês-1. Devido a incertezas nos produtos de SR, não foi possível realizar o fechamento do balanço hídrico. Com relação as séries temporais derivadas dos dados de SR, nenhuma mudança significativa foi observada. Por outro lado, a avaliação das séries temporais de longa duração, apresentaram diminuição de 245 mm na precipitação, com as chuvas tendo intensidade e número de eventos reduzidos. Este fenômeno é provavelmente resultante de dois processos, sendo um deles a redução na ciclagem da água devido ao desmatamento. O segundo corresponde a oscilação decadal na temperatura da superfície do Oceano Pacífico, a qual influencia a circulação atmosférica em grande escala. Embora o desmatamento cause aumento na vazão do rio, a redução da precipitação na Bacia do Alto Xingu foi suficientemente alta para mascarar esse efeito. Os dados aqui apresentados não só apresentam um diagnóstico sobre os recursos hidrícos do Alto Xingu, como também são extremamente relevantes para a compreensão da interação entre a paisagem e os componentes do balanço hídrico.

Os modelos de Daley-Kendall e Maki-Thompson são os dois modelos estocásticos para difusão de rumores mais citados até o momento. Em ambos, uma população finita fechada e totalmente misturada é subdividida em três classes de indivíduos denominados ignorantes, informantes e contidos. Depois de um rumor ser introduzido na população, difunde-se através desta seguindo determinadas regras que dependem da classe à qual a pessoa que sabe do rumor pertence. Tanto a proporção final de indivíduos que nunca chegam a conhecer o rumor quanto o tempo que este demora em ser difundido são variáveis de interesse para os modelos propostos. As técnicas encontradas na literatura para estudar modelos de rumores são o princípio de difusão de constantes arbitrárias; argumentos de martingais; o método de funções geradoras e a análise de versões determinísticas do processo. Neste trabalho apresentamos uma alternativa para essas técnicas baseando-nos na teoria de cadeias de Markov \"density dependent\'\'. O uso desta nova abordagem nos permite apresentar resultados assintóticos para um modelo geral que tem como casos particulares os famosos modelos de Daley-Kendall e Maki-Thompson, além de variações de modelos de rumores apresentados na literatura recentemente. / Daley-Kendall and Maki-Thompson models are the two most cited stochastic models for the spread of rumours phenomena, in scientific literature. In both, a closed homogeneously mixing population is subdivided into three classes of individuals called ignorants, spreaders and stiflers. After a rumor is introduced in the population, it spreads by following certain rules that depend on the class to which the individual who knows the rumor belongs. Both the final proportion of the population never hearing the rumor and the time it takes are variables of interest for the proposed models. The main tools used to study stochastic rumours have been the principle of the diffusion of arbitrary constants, martingale arguments, generating functions and the study of analogue deterministic versions. Relying on the theory of density dependent Markov chains, we present an alternative to these tools. This approach allows us to establish asymptotical results for a general model that has as particular cases the classical Daley-Kendall and Maki-Thompson models, and other variations for rumour models reported in the literature recently.

Submitted by Valquíria Barbieri (kikibarbi@hotmail.com) on 2018-05-11T20:59:15Z No. of bitstreams: 1 DISS_2015_Karen Janones da Rocha.pdf: 4327569 bytes, checksum: 1207959001ffdfc221d56edf601d488a (MD5) / Approved for entry into archive by Jordan (jordanbiblio@gmail.com) on 2018-05-24T14:50:15Z (GMT) No. of bitstreams: 1 DISS_2015_Karen Janones da Rocha.pdf: 4327569 bytes, checksum: 1207959001ffdfc221d56edf601d488a (MD5) / Made available in DSpace on 2018-05-24T14:50:15Z (GMT). No. of bitstreams: 1 DISS_2015_Karen Janones da Rocha.pdf: 4327569 bytes, checksum: 1207959001ffdfc221d56edf601d488a (MD5) Previous issue date: 2015-02-06 / CAPES / O objetivo geral do presente estudo foi caracterizar um fragmento secundário de Floresta Estacional Semidecidual localizado em Tapurah-MT, quanto a sua estrutura e composição florestal, verificar a formação de grupos florísticos e, ainda, explorar possíveis relações com o ambiente. Aplicou-se o método de área fixa com conglomerados retangulares de dimensões de 10 x 250 m, foram alocados e medidos cinco conglomerados com cinco subunidades cada de 10 X 50 m. Em cada subunidade amostral foi considerada todas as espécies arbóreas e arbustivas com diâmetro à altura do peito (DAP) superior ou igual a 10 cm. A composição florística foi analisada quanto ao número de famílias, gêneros e espécies botânicas encontradas no levantamento do componente arbóreo e a suficiência amostral do levantamento florístico foi verificada pelo procedimento Bootstrap. A similaridade florística entre as subunidades amostrais foi obtida através do Índice de Jaccard e a diversidade de espécies nas subunidades amostrais foi medida pelo Índice de Shannon (H’) e pelo Índice de Equabilidade de Pielou (J’). A caracterização da estrutura horizontal da vegetação foi feita a partir dos parâmetros fitossociológicos e a estrutura diamétrica pelo procedimento de Spiegel. A presença de grupos florísticos foi verificada pelo método de associação das espécies e o número de grupos foi estabelecido pelo coeficiente de concordância de Kendall, onde para cada grupo florístico foi analisada a estrutura horizontal, o padrão de distribuição espacial das espécies pelo índice de Payandeh e a estrutura diamétrica dos indivíduos pelo procedimento de Spiegel. A construção da matriz das variáveis edáficas foi realizada através de uma análise preliminar para identificar variáveis semelhantes entre as subunidades amostrais, as quais não apresentaram influência foram retiradas. A correlação entre os dados de vegetação e dados ambientais foi realizada por meio da Análise de Correlação Canônica, que permitiu confirmar se os nutrientes do solo influenciam na presença das espécies e pela Análise de Redundância Canônica para avaliar quais as variáveis ambientais apresentaram maior influência sobre os indivíduos. No fragmento foi verificada uma alta variabilidade florística e estrutural, que pode ser explicada pelos históricos de perturbação local a que este fragmento foi submetido no passado. De uma forma geral, a vegetação corresponde a de florestas secundárias jovens e apresenta uma comunidade estável e autorregenerativa, além de preservar características da estrutura original. Através da análise de agrupamento foi verificado que as características autoecológicas das espécies assim como os DAP’s médios de cada espécie foram os principais responsáveis pela associação e similaridade entre os grupos. Também foi verificada que apesar das perturbações no ambiente que salientam a saturação do sítio florestal, o fragmento está se recuperando. A heterogeneidade das variáveis edáficas relacionadas influencia no comportamento florístico-estrutural do fragmento secundário de Floresta Estacional Semidecidual. Sendo, as espécies das famílias Fabaceae, Lauraceae, Moraceae e Vochysiaceae as mais influentes para o presente estudo. Destacando a Qualea paraensis Ducke quanto à importância ecológica e a sua adaptabilidade ao ambiente. / The general objective of this study was to characterize a secondary fragment of semideciduous forest located in Tapurah-MT, as its structure and forest composition, verify the formation of floristic groups and also explore possible relationships with the environment. Was applied the fixed area method with five rectangular clusters of 10 x 250 m, they were measured and allocated to five subunits of 10 x 50 m each. In each sample subunit was considered all tree and shrub species with diameter at breast height (DBH) greater than or equal to 10 cm. The floristic composition was analyzed for the number of families, genera and plant species found in the survey of the tree component and sampling sufficiency of floristic survey was tested by bootstrap procedure. The floristic similarity between plots was obtained through the Jaccard index and the diversity of species in the sample subunits was measured by the Shannon Index (H') and equability index of Pielou (J'). The characterization of the horizontal structure of vegetation was made from the phytosociological parameters and the structure diameter by Spiegel procedure. The presence of floristic groups was verified by the association method of species and the number of groups was established by Kendall concordance coefficient, where for each floristic group was analyzed horizontal structure, the pattern of spatial distribution of species by Payandeh index and the diameter distribution of individuals by Spiegel procedure. The construction of the matrix of the soil variables was performed in a preliminary analysis to identify variables similar to the sample subunits, which showed no influence were dropped. The correlation between the data of vegetation and environmental data was performed by Canonical Correlation Analysis, which allowed confirm that soil nutrients influence the presence of the species and the Canonical Redundancy Analysis to evaluate which environmental variables had the greatest influence on the individuals. In the studied fragment was observed high variability floristic and structural, which can be explained by historical local disturbance that this fragment was in the past. In general, the vegetation corresponds to young secondary forests and presents a stable and self-regenerative community, besides preserving the original structure characteristics. Through cluster analysis it was found that the ecological self characteristics of the species as well as the average DBH of each species were mainly responsible for the association and similarity between the groups. We also observed that despite the disturbances in the environment that emphasize the saturation of forest site, the fragment is recovering. The soil variables heterogeneity related influence the floristic-structural behavior of the secondary fragment of semideciduous forest. Being, the species of the families: Fabaceae, Lauraceae, Moraceae and Vochysiaceae the most influential for the present study. Highlighting the Qualea paraensis Ducke about its ecological significance and adaptability to the environment.

Os modelos de Daley-Kendall e Maki-Thompson são os dois modelos estocásticos para difusão de rumores mais citados até o momento. Em ambos, uma população finita fechada e totalmente misturada é subdividida em três classes de indivíduos denominados ignorantes, informantes e contidos. Depois de um rumor ser introduzido na população, difunde-se através desta seguindo determinadas regras que dependem da classe à qual a pessoa que sabe do rumor pertence. Tanto a proporção final de indivíduos que nunca chegam a conhecer o rumor quanto o tempo que este demora em ser difundido são variáveis de interesse para os modelos propostos. As técnicas encontradas na literatura para estudar modelos de rumores são o princípio de difusão de constantes arbitrárias; argumentos de martingais; o método de funções geradoras e a análise de versões determinísticas do processo. Neste trabalho apresentamos uma alternativa para essas técnicas baseando-nos na teoria de cadeias de Markov \"density dependent\'\'. O uso desta nova abordagem nos permite apresentar resultados assintóticos para um modelo geral que tem como casos particulares os famosos modelos de Daley-Kendall e Maki-Thompson, além de variações de modelos de rumores apresentados na literatura recentemente. / Daley-Kendall and Maki-Thompson models are the two most cited stochastic models for the spread of rumours phenomena, in scientific literature. In both, a closed homogeneously mixing population is subdivided into three classes of individuals called ignorants, spreaders and stiflers. After a rumor is introduced in the population, it spreads by following certain rules that depend on the class to which the individual who knows the rumor belongs. Both the final proportion of the population never hearing the rumor and the time it takes are variables of interest for the proposed models. The main tools used to study stochastic rumours have been the principle of the diffusion of arbitrary constants, martingale arguments, generating functions and the study of analogue deterministic versions. Relying on the theory of density dependent Markov chains, we present an alternative to these tools. This approach allows us to establish asymptotical results for a general model that has as particular cases the classical Daley-Kendall and Maki-Thompson models, and other variations for rumour models reported in the literature recently.

In the southern of the Amazon basin, extensive deforestation associated with global climate change have impacted the regional water cycle. Predictions indicate that future alteration might cause even higher pressure over regional water resources. The goal of this study was to perform a detailed evaluation of past changes in the water resources of the upper Xingu basin, a region which is broadly representative of southern Amazon. The evaluation consisted of characterizing alterations in medium and long-term time series of rainfall, river discharge, evapotranspiration and total water storage change. The study employed not only in situ measurements, but also remotely sensed data. Remote sensing products including rainfall, evapotranspiration and water storage change were employed in the evaluation of the regional water balance. A thirteen years\' time series derived from RS products was submitted to a trend analysis, to detect significant variations in the water balance. Furthermore, uncertainties in each remote sensing product were retrieved, mostly comparing in situ measurements with RS estimates. To describe limitations of such products to evaluate the regional water balance, river discharge was calculated as the residual of the water balance. Later on, the estimated river discharge was compared to in situ measurements and uncertainties in the water balance were defined. The analysis of long-term alterations considered in situ measurements of rainfall and river discharge, from the period of 1976-2015. In this case, a group of hydro-climatological indicators was derived and then submitted to Mann-Kendall and Petit test. Due to the relevance of forest cover on river flow regulation, land use changes (LUC) were mapped every five years from 1985 to 2015. LUC results were then compared to the hydro-climatological data, to identify similarities in changing patterns. The evaluation of water balance components based on remote sensing products described fairly well the spatial variability in the study site. The uncertainties in P, ET and TWSC products corresponded to 41, 25 and 18 mm month-1, respectively. Due to these uncertainties, it was not possible to perform the water balance closure based on RS data. No significant changes were observed in the time series derived from these products. Contrastingly, the evaluation of a 40-years\' time series presented a decrease of 245 mm in rainfall, with intensity and number of rainy events being reduced. This phenomenon is most likely resultant from two process, the reduction in water recycling due to deforestation, as well as the Pacific Ocean decadal oscillation, which influences the large-scale atmospheric circulation. Although deforestation tends to increase river discharge, the reduction in rainfall in the Upper Xingu Basin was high enough to mask this effect. / O desmatamento em larga escala na região sul da bacia amazônica brasileira, associado às mudanças climáticas globais, tem impactado o ciclo hidrológico regional. Previsões futuras indicam uma pressão ainda maior sobre os recursos hídricos regionais. O objetivo deste estudo foi realizar uma avaliação detalhada das possíveis alterações nos recursos hídricos da bacia do Alto Xingu, uma região extremamente representativa do sul da Amazônia. Para tanto, foram empregadas séries temporais de longa e média duração, correspondentes à precipitação (P), vazão (Q), evapotranspiração (ET) e variação do armazenamento de água (TWSC). O estudo empregou medições in situ, bem como dados de sensoriamento remoto (SR). As estimativas de sensoriamento remoto foram empregadas na avaliação do balanço hídrico regional. As séries temporais de treze anos derivadas de produtos de SR foram submetidas a uma análise de tendência, com o objetivo de detectar variações significativas nos componentes do balanço hídrico. Além disso, as incertezas em cada produto foram obtidas comparando-se medições in situ com as estimativas de SR. Com o objetivo de descrever as limitações de tais produtos para a realização do balanço hídrico regional, a vazão do rio Xingu foi estimada com base na fórmula do balanço hídrico. Posteriormente, tal estimativa foi comparada com as medições in situ, gerando um indicativo da incerteza no fechamento do balanço hídrico. Já a análise das alterações a longo prazo considerou as medidas in situ da precipitação e vazão, no período de 1976-2015. Neste caso, um grupo de indicadores hidro-climatológicos foi calculado e posteriormente submetido aos testes de Mann-Kendall e Pettit. Devido à relevância das florestas na regulação da vazão dos rios, as mudanças no uso e ocupação da terra foram mapeadas a cada cinco anos, durante 1985-2015. Os resultados foram comparados aos dados hidro-climatológicos, buscando assim semelhanças nos padrões de alteração. Os produtos de sensoriamento remoto descreveram razoavelmente bem a variabilidade espacial dos componentes do balanço hídrico. As incertezas nas estimativas de P, ET e TWSC corresponderam a 41, 25 e 18 mm mês-1. Devido a incertezas nos produtos de SR, não foi possível realizar o fechamento do balanço hídrico. Com relação as séries temporais derivadas dos dados de SR, nenhuma mudança significativa foi observada. Por outro lado, a avaliação das séries temporais de longa duração, apresentaram diminuição de 245 mm na precipitação, com as chuvas tendo intensidade e número de eventos reduzidos. Este fenômeno é provavelmente resultante de dois processos, sendo um deles a redução na ciclagem da água devido ao desmatamento. O segundo corresponde a oscilação decadal na temperatura da superfície do Oceano Pacífico, a qual influencia a circulação atmosférica em grande escala. Embora o desmatamento cause aumento na vazão do rio, a redução da precipitação na Bacia do Alto Xingu foi suficientemente alta para mascarar esse efeito. Os dados aqui apresentados não só apresentam um diagnóstico sobre os recursos hidrícos do Alto Xingu, como também são extremamente relevantes para a compreensão da interação entre a paisagem e os componentes do balanço hídrico.

No description available.

Η παρούσα εργασία διαπραγματεύεται την επεξεργασία ετήσιων και εποχικών χρονοσειρών βροχόπτωσης από 12 σταθμούς της Δυτικής Ελλάδας για την περίοδο 1975-2004. Επιπλέον για τους 8 από τους συνολικά 12 σταθμούς όπου υπήρχε η δυνατότητα, η επεξεργασία αφορά μια περίοδο 50 ετών (1956-2005). Χρησιμοποιώντας ως κλιματικό δείκτη το ετήσιο βροχομετρικό ύψος προκύπτει ότι το σύνολο των 12 σταθμών χαρακτηρίζεται εν γένει από έναν συνδυασμό ημίυγρου ή υγρού κλιματικού τύπου. Χρησιμοποιώντας τον μη-παραμετρικό έλεγχο των Mann-Kendall για την εξακρίβωση παρουσίας τάσεων σε βάθος χρόνου, για την περίοδο 1975-2004 δεν διαφαίνεται η ύπαρξη κάποιας σημαντικής τάσης εκτός από τις ετήσιες βροχοπτώσεις του Πύργου που εμφανίζουν μία σημαντικά αρνητική τάση. Την περίοδο από το 1956-2005 προκύπτουν σημαντικά αρνητικές τάσεις τόσο σε εποχική βάση (κυρίως την άνοιξη) όσο και σε ετήσια για τους μισούς από τους οκτώ σταθμούς που εξετάστηκαν. Η Γάμμα κατανομή είναι εκείνη που περιγράφει καλύτερα το φυσικό μέγεθος ύψος βροχόπτωσης και στην περίπτωση μας προσδιορίζονται ανά σταθμό και για την περίοδο 1975-2004 (σε εποχική και ετήσια βάση), οι παράμετροι της με την βοήθεια της μεθόδου μέγιστης πιθανοφάνειας. Στα πλαίσια της φασματικής ανάλυσης, για να εξακριβωθεί η ύπαρξη ή οχι περιοδικότητας στην τιμή της διασποράς των εποχικών και ετήσιων τιμών βροχόπτωσης χρησιμοποιούνται οι 7 σταθμοί για τους οποίους υπάρχει επάρκεια μετρήσεων με εξεταζόμενη περίοδο την πεντηκονταετία 1955-2004 και κάνοντας χρήση της μεθόδου Blackman-Tukey. Προκύπτει με την εν λόγω μέθοδο ότι κατά την διάρκεια του φθινοπώρου και της άνοιξης δεν διαφαίνονται κάποια σαφή στοιχεία περιοδικότητας στην διασπορά των υψών υετού των 7 σταθμών. Αυτό δεν ισχύει όμως για τον χειμώνα αλλά και σε ετήσια βάση, όπου στα φάσματα των τιμών υετού των σταθμών αποκαλύπτονται τρεις περιοχές συχνοτήτων περιοδικότητας που μοιάζουν αρκετά μεταξύ τους. Αυτό αντανακλά το γεγονός ότι σε γενικές γραμμές οι σταθμοί της Δυτικής Ελλάδας επηρεάζονται από τα ίδια περιπου βαρομετρικά συστήματα και άρα είναι φυσιολογικό να εμφανίζουν παρόμοιες συνιστώσες περιοδικότητας στις διασπορές των τιμών υετού τους. / This work deals with the processing of annual and seasonal precipitation series from 12 stations of West Greece for a 30-year study period (1975-2004). Moreover for 8 out for τηε 12 stations where possible, the processing uses a 50-year study period (1956-2005). By using the annual precipitation height as an climatic index it follows that the total of the twelve stations is characterized generally by a combination of semi-wet and wet climatic type. Making use of nonparametric Mann-Kendall test for ascertaining the existence of trend, it doesn't follow any significant trend for the 30-year period (1975-2004), with the exception of the annual precipitation heights of Pirgos that show a significant negative trend. During the 50-year period (1956-2005) significant negative trends occur in seasonal (mainly during spring) and annual basis as well, for half of the eight stations which have been examined. Gamma distribution is tha type of statistical distribution that describes more effectively the physical quantity precipitation height, and in our case its parameters per station are being computed for the period 1975-2004, by using the maximum likelihood method. Under the framework of a Spectral analysis of the precipitation series (for the verification of periodicity in the variances of precipitation rates) , 7 stations are used for a 50-year study period (1955-2004) by using the Blackman-Tukey method. It follows after this method has been used, that precipitation series don't appear any periodicity during autumn and spring seasons. This is in contrast with the winter season and the annual rainfall values as well, where three parts of periodicity in the spectra of the stations appear that bear a common resemblance. This depicts the fact that genarally the total of West Greece stations are influenced by almost the same barometric pressure systems which leads to the variances of precipitation rates to appear common periodicity components.