887 resultados para SIERRA NEVADA DE SANTA MARTA


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Global amphibian decline by chytridiomycosis is a major environmental disaster that has been attributed to either recent fungal spread or environmental change that promotes disease. Here, we present a population genetic comparison of Batrachochytrium dendrobatidis isolates from an intensively studied region of frog decline, the Sierra Nevada of California. In support of a novel pathogen, we find low diversity, no amphibian-host specificity, little correlation between fungal genotype and geography, local frog extirpation by a single fungal genotype, and evidence of human-assisted fungus migration. In support of endemism, at a local scale, we find some diverse, recombining populations. Therefore neither epidemic spread nor endemism alone explains this particular amphibian decline. Recombination raises the possibility of resistant sporangia and a mechanism for rapid spread as well as persistence that could greatly complicate global control of the pathogen.

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This chapter reviews the concepts of organizational culture and climate and applies them to environmental sustainability. Though culture and climate are often used interchangeably, the chapter identifies key distinctions between them and highlights how they can complement one another. The two concepts are used to discuss how the organizational context for environmental sustainability, and employee perceptions thereof, influence individual pro-environmental behavior. Organizational climate is integrated with a dynamic model of organizational culture to describe how pro-environmental cultures and climates emerge. The chapter also highlights how organizations with different motivations can create pro-environmental cultures and climates. The chapter uses the Sierra Nevada Brewing Company as an archetype of an organization with a pro-environmental culture and climate. In the course of the discussion, the chapter nominates several imperatives for research and recommendations for practice.

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I. Foehn winds of southern California.
An investigation of the hot, dry and dust laden winds occurring in the late fall and early winter in the Los Angeles Basin and attributed in the past to the influences of the desert regions to the north revealed that these currents were of a foehn nature. Their properties were found to be entirely due to dynamical heating produced in the descent from the high level areas in the interior to the lower Los Angeles Basin. Any dust associated with the phenomenon was found to be acquired from the Los Angeles area rather than transported from the desert. It was found that the frequency of occurrence of a mild type foehn of this nature during this season was sufficient to warrant its classification as a winter monsoon. This results from the topography of the Los Angeles region which allows an easy entrance to the air from the interior by virtue of the low level mountain passes north of the area. This monsoon provides the mild winter climate of southern California since temperatures associated with the foehn currents are far higher than those experienced when maritime air from the adjacent Pacific Ocean occupies the region.

II. Foehn wind cyclo-genesis.
Intense anticyclones frequently build up over the high level regions of the Great Basin and Columbia Plateau which lie between the Sierra Nevada and Cascade Mountains to the west and the Rocky Mountains to the east. The outflow from these anticyclones produce extensive foehns east of the Rockies in the comparatively low level areas of the middle west and the Canadian provinces of Alberta and Saskatchewan. Normally at this season of the year very cold polar continental air masses are present over this territory and with the occurrence of these foehns marked discontinuity surfaces arise between the warm foehn current, which is obliged to slide over a colder mass, and the Pc air to the east. Cyclones are easily produced from this phenomenon and take the form of unstable waves which propagate along the discontinuity surface between the two dissimilar masses. A continual series of such cyclones was found to occur as long as the Great Basin anticyclone is maintained with undiminished intensity.

III. Weather conditions associated with the Akron disaster.
This situation illustrates the speedy development and propagation of young disturbances in the eastern United States during the spring of the year under the influence of the conditionally unstable tropical maritime air masses which characterise the region. It also furnishes an excellent example of the superiority of air mass and frontal methods of weather prediction for aircraft operation over the older methods based upon pressure distribution.

IV. The Los Angeles storm of December 30, 1933 to January 1, 1934.
This discussion points out some of the fundamental interactions occurring between air masses of the North Pacific Ocean in connection with Pacific Coast storms and the value of topographic and aerological considerations in predicting them. Estimates of rainfall intensity and duration from analyses of this type may be made and would prove very valuable in the Los Angeles area in connection with flood control problems.

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O objetivo desta tese é discutir como os moradores de favelas no Rio de Janeiro fazem para experimentar segurança em meio ao cotidiano marcado por inseguranças, violência e vulnerabilidade social. Minha hipótese central é que os moradores destas localidades visualizam nas lealdades primordiais (GEERTZ, 2008 [1973]), nas relações de vizinhança e em redes formadas em torno do pertencimento a instituições religiosas, sobretudo as pentecostais e neopentecostais a base da segurança necessária para organizarem suas vidas, suas rotinas. Busquei responder às questões que me animavam a partir de um investimento etnográfico em duas favelas cariocas, a saber, Santa Marta, localizada no bairro de Botafogo, Zona Sul, e, principalmente, Acari, localizada entre bairros da Zona Norte da cidade. Ao longo da etnografia realizei entrevistas semi-estruturadas com moradores evangélicos, traficantes, homens, mulheres, jovens e idosos, lideranças políticas e culturais. A partir destas entrevistas, assim como das conversas informais com moradores nestas favelas, pude observar a grande dificuldade que os moradores das referidas localidades têm, face à violência, para experimentar constantemente segurança e confiança, mesmo no caso dos moradores que desfrutam de densas redes de solidariedade e proteção baseadas no parentesco e/ou na partilha de identidade religiosa pentecostal. A paranóia, o medo da fofoca e do inimigo à espreita tomam conta do cotidiano de moradores (e também de traficantes). Neste contexto, identifiquei nas suas tentativas de consolidação de vínculos sociais e afetivos, mas também em seus diversos cálculos em termos de evitação da violência suas principais estratégias para viver o dia-a-dia com certa tranqüilidade. O curso da etnografia possibilitou, ainda, refletir sobre a importância da articulação analítica de dois eixos temáticos para o estudo da favela como fenômeno urbano/social hoje: religião e violência. Esta avaliação é fruto da observação das aproximações entre traficantes que passaram, nessas localidades, a experimentar novas formas de expressão de fé. Se, nas décadas de 1980-1990, os traficantes de Acari expunham em seus corpos, em suas casas e nos muros da favela imagens e orações que remetiam ao universo religioso afro-brasileiro, na atualidade, acionam uma gramática pentecostal e pintam nos muros da favela salmos e outras passagens bíblicas. Se antes pediam proteção às mães-de-santo, agora pedem proteção às lideranças evangélicas e à comunidade de irmãos, assim como comemoram seus aniversários em cultos de ação de graça. A interface entre traficantes e evangélicos nas favelas estudadas, com destaque para Acari, vem produzindo, sustento, reequilíbrios de poder no interior do campo político e religioso local e, até, supralocal.

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O presente trabalho tem como objetivo compreender a experiência da maternidade a partir do discurso narrativo de jovens moças, residentes no Morro Santa Marta favela situada no coração da Zona Sul do Rio de Janeiro e que estão experimentando a gestação pela primeira vez. Para tanto, foi importante investigar o conceito de maternidade, sob uma perspectiva sócio-histórica, para dar ênfase a um olhar winnicottiano, no qual o ambiente tem um caráter fundamental na construção da subjetividade. A experiência da maternidade nas classes trabalhadoras e um breve histórico das favelas cariocas foram igualmente traçados, dando destaque ao Morro Santa Marta. A fim de refletir sobre os aspectos subjetivos relacionados com a experiência de tornar-se mãe, uma pesquisa qualitativa foi desenvolvida com cinco mulheres escolhidas aleatoriamente. Tomou-se um grande cuidado em ultrapassar estereótipos e estigmas que recaem sobre a população, priorizando, na escuta, os valores, percepções, opiniões e hábitos culturais que podem ser expressos de forma verbal e/ou não verbal.

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EXTRACT (SEE PDF FOR FULL ABSTRACT): The early-Holocene warm period, ca. 9000 years ago, is a realistic analog for the possible effects of greenhouse warming. At that time the vegetation of the western Sierra Nevada resembled that currently found east of the crest. ... Tourism, water supply, and the logging industry will be negatively effected if climate changes during the next century are in the direction and magnitude of those of the early Holocene. Increased precipitation in the eastern Sierra could offset some of the effects.

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EXTRACT (SEE PDF FOR FULL ABSTRACT): There is considerable seasonal-to-interannual variability in the runoff of major watersheds in the Sierra Nevada, Coastal, and Cascade ranges of California and southwestern Oregon. This variability is reflected in both the amount and timing of runoff. This study examines that variability using long historical streamflow records and seasonal mean temperature and precipitation. ... Precipitation is the only significant predictor for both amount and timing of runoff in the low elevation basins. As elevation increases, the models rely more and more on temperature to explain amount and timing of runoff.

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Cross-spectral analysis of regional tree-ring data suggests the spatial pattern of correlation between moisture variations in the Sierra Nevada of central California and in other parts of the western United States is frequency dependent. Short wavelengths (2.8 to 10.7 years), perhaps associated with El Niño/Southern Oscillation, are strongly coherent both to the north (Oregon) and to the south (Southern California). Longer wavelengths (45 to 75 years) are strongly coherent only to the north. Frequency bands corresponding to annual sunspot series were associated with relatively weak patterns of spatial correlation.

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EXTRACT (SEE PDF FOR FULL ABSTRACT): We estimate monthly runoff for a 2-dimensional solution domain containing those areas tributary to Pyramid Lake, Nevada (the Truckee River drainage basin) at a 1-kilometer grid cell spacing. ... To calculate the effect of snow on the hydrologic system, we perform two experiments. In the first we assume that all precipitation falls as rain; in the second we assume that some precipitation falls as snow, thus available water is a combination of rain and snowmelt. We find that considering the effect of snow results in a more accurate representation of mean monthly flow rates, in particular the peak flow during the melt season in the Sierra Nevada. These preliminary results indicate that a relatively simple snow model can improve the representation of Truckee River basin hydrology, significantly reducing errors in modeled seasonal runoff.

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The purpose of this paper is to summarize the biggest northern California floods of the 20th century. Flooding in California can occur from different causes. At least three types of floods occur: 1. Winter general floods, which cover a large area. 2. Spring and early summer snowmelt floods unique to the higher-elevation central and southern Sierra Nevada, which occur about once in 10 years on the average. 3. Local floods from strong thunderstorms, with intense rain over a relatively small area. These originate in moist tropical or subtropical air and include the flash floods of the desert and other areas of southern California when remnants of eastern Pacific hurricanes get carried into the state.

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In recent years seismic tomography has become a powerful tool for studying the three-dimensional crust and mantle structure. In this study, we collected a large number of regional and teleseismic travel-time data and used seismic tomography method to study the relationship between earthquake occurrence and crustal heterogeneity for the 1992 Landers earthquake, heterogeneity and evolution of lithosphere under North China Craton and Southern California, and deep structure and origin of the Changbai intraplate volcano in Northeast China. Our results show a correlation between the seismic rupture zone and crustal heterogeneity. The distribution of the Landers aftershocks is cluster-like and separated or terminated in areas where low-velocity anomalies exist.Most of the large earthquakes with magnitudes >4.0 occurred in or around areas with high P-wave velocity.The possibility is that high-velocity areas are brittle and strong parts which can sustain seismogenic stress,and so can generate earthquakes. Our tomographic images show a very heterogeneous structure in the crust and upper mantle beneath Southern California. Three major anomalies in the upper mantle are revealed clearly beneath the southern Sierra Nevada, Transverse Ranges and Salton Trough. We consider that the high-velocity anomaly beneath the Transverse Ranges was formed through asymmetrical two-side convergence of subcrustal lithosphere and sinking to asthenosphere. Formation of the dense crust root and “drip structure” caused the high-velocity anomaly under the southern Sierra Nevada. The Salton Trough low is the response to the lithospheric extension when the Pacific plate was rifted away from the North American Plate. The tomograpic images beneath the North China Craton show that there exist different lithospheric structures under the different blocks. Complex, prominent low-velocity and high-velocity anomalies are imaged beneath the North China Basin, Trans-North China Orogen (TNCO), and Ordos Block which correspond to rifted, orogenic and cratonic lithospheres, respectively. The thickness of the three-type lithospheres is about 70, 90 and >250 km, respectively. Our results suggest that lithospheric thinning under the eastern part of North China Craton is due to long-term replacement and chemical and thermal erosion of the ancient lithosphere by the hot asthenosphere. The remains of ancient lithosphere exist either in the present upper mantle or have sunk into the mantle transition zone. Our tomographic result of the Changbai volcanic area suggests that the origin of the Changbai volcano is related to the deep dehydration of the subducted Pacific slab and corner flow in the big mantle wedge (BMW) above the stagnant Pacific slab.

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68 hojas : ilustraciones.

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31 hojas : ilustraciones, fotografías a color

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Se presenta una propuesta desarrollada en el Departamento del Magdalena, Distrito Cultural e Histórico de Santa Marta. A finales del año 2002 se hizo un análisis de los bajos resultados presentados por los estudiantes de grado Once en las diferentes pruebas aplicadas por el ICFES, específicamente en el área de Matemática durante los años 2001 y 2002. A partir de estos resultados se organizó un equipo de trabajo donde se asumió que la evaluación es un proceso continuo e integral en la enseñanza de la matemática que no solo basta dar información a diario, sino conocer realmente si los estudiantes están aprendiendo, si verdaderamente los alumnos son competentes a la hora de evaluarlos y además si se cumplen los estándares mínimos exigidos por MEN. Para lograr tal fin se diseño un plan estratégico a mediano plazo que ayuda a fortalecer los niveles de desempeño en el desarrollo de sus competencias tanto integrales ((interpretativa, argumentativa, propositiva) como básicas (la comunicación, el razonamiento y la solución de problemas), obteniéndose a partir del año 2006 resultados satisfactorios en el área.