955 resultados para Venus (Ship)
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Records of Atlantic basin tropical cyclones (TCs) since the late nineteenth century indicate a very large upward trend in storm frequency. This increase in documented TCs has been previously interpreted as resulting from anthropogenic climate change. However, improvements in observing and recording practices provide an alternative interpretation for these changes: recent studies suggest that the number of potentially missed TCs is sufficient to explain a large part of the recorded increase in TC counts. This study explores the influence of another factor—TC duration—on observed changes in TC frequency, using a widely used Atlantic hurricane database (HURDAT). It is found that the occurrence of short-lived storms (duration of 2 days or less) in the database has increased dramatically, from less than one per year in the late nineteenth–early twentieth century to about five per year since about 2000, while medium- to long-lived storms have increased little, if at all. Thus, the previously documented increase in total TC frequency since the late nineteenth century in the database is primarily due to an increase in very short-lived TCs. The authors also undertake a sampling study based upon the distribution of ship observations, which provides quantitative estimates of the frequency of missed TCs, focusing just on the moderate to long-lived systems with durations exceeding 2 days in the raw HURDAT. Upon adding the estimated numbers of missed TCs, the time series of moderate to long-lived Atlantic TCs show substantial multidecadal variability, but neither time series exhibits a significant trend since the late nineteenth century, with a nominal decrease in the adjusted time series. Thus, to understand the source of the century-scale increase in Atlantic TC counts in HURDAT, one must explain the relatively monotonic increase in very short-duration storms since the late nineteenth century. While it is possible that the recorded increase in short-duration TCs represents a real climate signal, the authors consider that it is more plausible that the increase arises primarily from improvements in the quantity and quality of observations, along with enhanced interpretation techniques. These have allowed National Hurricane Center forecasters to better monitor and detect initial TC formation, and thus incorporate increasing numbers of very short-lived systems into the TC database.
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Emissions of exhaust gases and particles from oceangoing ships are a significant and growing contributor to the total emissions from the transportation sector. We present an assessment of the contribution of gaseous and particulate emissions from oceangoing shipping to anthropogenic emissions and air quality. We also assess the degradation in human health and climate change created by these emissions. Regulating ship emissions requires comprehensive knowledge of current fuel consumption and emissions, understanding of their impact on atmospheric composition and climate, and projections of potential future evolutions and mitigation options. Nearly 70% of ship emissions occur within 400 km of coastlines, causing air quality problems through the formation of ground-level ozone, sulphur emissions and particulate matter in coastal areas and harbours with heavy traffic. Furthermore, ozone and aerosol precursor emissions as well as their derivative species from ships may be transported in the atmosphere over several hundreds of kilometres, and thus contribute to air quality problems further inland, even though they are emitted at sea. In addition, ship emissions impact climate. Recent studies indicate that the cooling due to altered clouds far outweighs the warming effects from greenhouse gases such as carbon dioxide (CO2) or ozone from shipping, overall causing a negative present-day radiative forcing (RF). Current efforts to reduce sulphur and other pollutants from shipping may modify this. However, given the short residence time of sulphate compared to CO2, the climate response from sulphate is of the order decades while that of CO2 is centuries. The climatic trade-off between positive and negative radiative forcing is still a topic of scientific research, but from what is currently known, a simple cancellation of global mean forcing components is potentially inappropriate and a more comprehensive assessment metric is required. The CO2 equivalent emissions using the global temperature change potential (GTP) metric indicate that after 50 years the net global mean effect of current emissions is close to zero through cancellation of warming by CO2 and cooling by sulphate and nitrogen oxides.
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We examine to what degree we can expect to obtain accurate temperature trends for the last two decades near the surface and in the lower troposphere. We compare temperatures obtained from surface observations and radiosondes as well as satellite-based measurements from the Microwave Soundings Units (MSU), which have been adjusted for orbital decay and non-linear instrument-body effects, and reanalyses from the European Centre for Medium-Range Weather Forecasts (ERA) and the National Centre for Environmental Prediction (NCEP). In regions with abundant conventional data coverage, where the MSU has no major influence on the reanalysis, temperature anomalies obtained from microwave sounders, radiosondes and from both reanalyses agree reasonably. Where coverage is insufficient, in particular over the tropical oceans, large differences are found between the MSU and either reanalysis. These differences apparently relate to changes in the satellite data availability and to differing satellite retrieval methodologies, to which both reanalyses are quite sensitive over the oceans. For NCEP, this results from the use of raw radiances directly incorporated into the analysis, which make the reanalysis sensitive to changes in the underlying algorithms, e.g. those introduced in August 1992. For ERA, the bias-correction of the one-dimensional variational analysis may introduce an error when the satellite relative to which the correction is calculated is biased itself or when radiances change on a time scale longer than a couple of months, e.g. due to orbit decay. ERA inhomogeneities are apparent in April 1985, October/November 1986 and April 1989. These dates can be identified with the replacements of satellites. It is possible that a negative bias in the sea surface temperatures (SSTs) used in the reanalyses may have been introduced over the period of the satellite record. This could have resulted from a decrease in the number of ship measurements, a concomitant increase in the importance of satellite-derived SSTs, and a likely cold bias in the latter. Alternately, a warm bias in SSTs could have been caused by an increase in the percentage of buoy measurements (relative to deeper ship intake measurements) in the tropical Pacific. No indications for uncorrected inhomogeneities of land surface temperatures could be found. Near-surface temperatures have biases in the boundary layer in both reanalyses, presumably due to the incorrect treatment of snow cover. The increase of near-surface compared to lower tropospheric temperatures in the last two decades may be due to a combination of several factors, including high-latitude near-surface winter warming due to an enhanced NAO and upper-tropospheric cooling due to stratospheric ozone decrease.
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NDIR is proposed for monitoring of air pollutants emitted by ship engines. Careful optical filtering overcomes the challenge of optical detection of NO2 in humid exhaust gas, despite spectroscopic overlap with the water vapour band.
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This paper analyses 10 years of in-situ measurements of significant wave height (Hs) and maximum wave height (Hmax) from the ocean weather ship Polarfront in the Norwegian Sea. The 30-minute Ship-Borne Wave Recorder measurements of Hmax and Hs are shown to be consistent with theoretical wave distributions. The linear regression between Hmax and Hs has a slope of 1.53. Neither Hs nor Hmax show a significant trend in the period 2000–2009. These data are combined with earlier observations. The long-term trend over the period 1980–2009 in annual Hs is 2.72 ± 0.88 cm/year. Mean Hs and Hmax are both correlated with the North Atlantic Oscillation (NAO) index during winter. The correlation with the NAO index is highest for the more frequently encountered (75th percentile) wave heights. The wave field variability associated with the NAO index is reconstructed using a 500-year NAO index record. Hs and Hmax are found to vary by up to 1.42 m and 3.10 m respectively over the 500-year period. Trends in all 30-year segments of the reconstructed wave field are lower than the trend in the observations during 1980–2009. The NAO index does not change significantly in 21st century projections from CMIP5 climate models under scenario RCP85, and thus no NAO-related changes are expected in the mean and extreme wave fields of the Norwegian Sea.
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Large waves pose risks to ships, offshore structures, coastal infrastructure and ecosystems. This paper analyses 10 years of in-situ measurements of significant wave height (Hs) and maximum wave height (Hmax) from the ocean weather ship Polarfront in the Norwegian Sea. During the period 2000 to 2009, surface elevation was recorded every 0.59 s during sampling periods of 30 min. The Hmax observations scale linearly with Hs on average. A widely-used empirical Weibull distribution is found to estimate average values of Hmax/Hs and Hmax better than a Rayleigh distribution, but tends to underestimate both for all but the smallest waves. In this paper we propose a modified Rayleigh distribution which compensates for the heterogeneity of the observed dataset: the distribution is fitted to the whole dataset and improves the estimate of the largest waves. Over the 10-year period, the Weibull distribution approximates the observed Hs and Hmax well, and an exponential function can be used to predict the probability distribution function of the ratio Hmax/Hs. However, the Weibull distribution tends to underestimate the occurrence of extremely large values of Hs and Hmax. The persistence of Hs and Hmax in winter is also examined. Wave fields with Hs>12 m and Hmax>16 m do not last longer than 3 h. Low-to-moderate wave heights that persist for more than 12 h dominate the relationship of the wave field with the winter NAO index over 2000–2009. In contrast, the inter-annual variability of wave fields with Hs>5.5 m or Hmax>8.5 m and wave fields persisting over ~2.5 days is not associated with the winter NAO index.
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During the international FRAMZY expedition in March 2002 in-situ observations of Fram Strait cyclones were made by aircraft, ship and automatic buoys in order to study the interaction between cyclones and sea ice. The atmospheric characteristics of the observed cyclones are presented in this paper. The cyclones were generated in the baroclinic zone at the ice edge and moved NNE-ward along the ice edge. This was supported by warm air advection from WSW by an upper-level wave. The cyclones were rather small (diameter 200– 700 km) and shallow (1–1.5 km e-folding height for the horizontal pressure and temperature difference) with life times between 12 and 36 hours. In spite of the small space and time scales, remarkable extremes were observed within the cyclones. Winds reached maxima above 20 ms−1 lasting for only a few hours. The transition from the cold to the advancing warm air over sea ice occurred within narrow (5–30 km) frontal zones in which vorticity and convergence reached maxima on the order of 10−3 s−1. It is discussed whether the sea ice in spite of its inertia is able to react on these strong sub cyclone-scale processes and, thus, these processes have to be taken into account in models in order to simulate the cyclone-sea ice interaction properly.
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Julia Wilkinson and a Zooniverse citizen-science team examine Arctic auroral data, using observations from the ill-fated 19th-century Arctic exploration ship USS Jeannette.
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In this work, the diurnal evolution of the radiation balance components over the tropical Atlantic Ocean is described and analysed. The analysis is based on measurements carried Out on board a Brazilian Navy ship during the observational campaign of the FluTuA Project (`Fluxos Turbulentos sobre o Atlantico`), from 15 to 23 May 2002. The observations indicated that the albedo responds its expected to atmospheric attenuation effects with a diurnal evolution similar to the Fresnel albedo. In general, the observed longwave radiation values agreed better with the estimated values obtained without longwave reflection. In agreement with the literature, the average surface emissivity was around 0.97. The net radiation, estimated from published equations for albedo, atmospheric transmissivity and surface emissivity, agreed with the observations, indicating that these parameters are representative of the radiometric properties of the air-sea interface in the region between Natal (6 degrees S, 35.2 degrees W) and the Sao Pedro and Sao Paulo Archipelago (1 degrees N, 29.3 degrees W). Copyright (C) 2008 Royal Meteorological Society
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Nas sociedades contemporâneas a cidadania cultural é um tema a ser enfrentado ao lado da defesa por uma melhor qualidade de vida material, ambiental, econômica e social. Assim, o direito à liberdade de criação, informação, expressão da diversidade entre outros, apresentam-se como desafios e fundamentos para uma verdadeira democracia cultural.O presente trabalho encontra-se inserido no campo dos estudos de novas práticas de cidadania exercidas particularmente por movimentos culturais. Nosso objeto de pesquisa foi o cineclube Mate com Angu, localizado na Baixada Fluminense.Por meio de entrevistas temáticas, buscamos aferir como cinco integrantes do grupo formulam e realizam sua proposta de intervenção social e estética, e interagem com sua comunidade Duque de Caxias utilizando a linguagem audiovisual.Os argumentos e as práticas do Mate com Angu revelaram que embora o compromisso central do grupo seja no campo estético, suas atividades trazem implicações também nos campos político e social, influenciando a vida e a cultura da comunidade caxiense. Desse modo constatamos que suas intervenções contribuem para a ampliação do conceito de cidadania, e particularmente para a construção dos direitos culturais.
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Day after day, even small companies and multinationals brands need to compete in a worldwide market. All kind of global strategies have to involve production and regional market knowledge. Still being essential for company have a complete view of it market and it right position to gain competitive advantage. In a global market, get possible for the companies be in touch with last generation technologies and equipment's and all kind of research. Companies like that should develop products focused in customer's desire, even those extremely strict. Specifically in our country, as hard as we could think, the companies have access to credit lines, to the fiscal incentives offered by the states that alliance with the market potential are making possible the appearance of a lot companies and the growth of the companies already existent. However, these resources alone don't produce results to the company if it doesn't possess an internal organization able to assimilate the new market situation. The companies have to be able to apply the maximum resources offered by new technologies and understand how a communications facility means solution for many internal problems. In short terms, technology, financial resources, research and knowledge are available, however, the human resources might be prepared and developed in order to become the whole knowledge in profits. According 'JURAN' and his Total Quality Control philosophy the human resources playing fundamental role in the process, and in my opinion a company is something like a ship where all must be prepared to hold the rudder. I will develop a basic job looking for productivity and company's development through the people's involvement, focused in process of motivation, creativity and staff valorization. I believe that there no good production process without those requirements. Based on real case of a automotive parts and foundry company, located in Bento Gonçalves - RS, this work will look for to organize it mainly in its Industrial Division, adopting in participate administration where, through a information system and personnel involvement we will seek all favorable conditions to politics and strategies in get the growth of company.
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A prática educativa protestante no Brasi I se ex pressou principalmente através de colégios destinados as camadas dominantes da sociedade. No entanto, existiram também outras escolas, para atendimento a alunos provenientes das classes populares. No caso específico dos metodistas, foram cria - das escolas paroquiais e, no Rio de Janeiro, na zona portuária, surgiu o Instituto Central do Povo, com ativida - des ligadas a educação, saúde e higiene, trabalho, lazer, além da pregação religiosa. Este tipo de proposta de trabalho foi liderado por setores da igreja metodista que revelavam especial in teresse pelas questões sociais. De fato, desde sua origem na Inglaterra existem evidências de que os metodistas se preocupavam com as condições sociais a que o povo da epoca estava submetido, como se pode ver nos discursos de seus líderes e mesmo na sua prática. Posteriormente, ao transplantar-se o meto - dismo para a América, persistiram as discussões acerca des sas questoes, inclusive provocando divisões internas. Embora a orientação predominante, trazida para o Brasil pelos missionários, tenha sido a influenciada p~ 10 pietismo e pela fi losofia 1 iberal, em íntima relação com o processo de consolidação do capitalismo na sociedade norte-americana durante o Século XIX, é necessário reconhecer entre os metodistas a existência de grupos que defenderam o envolvimento dos cristãos e da igreja nas lu tas sociais, em defesa dos setores populares. Dentro do quadro do protestantismo norte-americano esses grupos se fil iam à corrente conhecida como Evangelho Social.A tentativa de atuação dos missionários metodis tas, 1 igados a esta tendência, que vieram ao Brasil teve, porem, alcance limitado na medida em que esbarrou em di - versos obstáculos: nos fundamentos teóricos sobre os quais as atividades foram concebidas, nas dificuldades de inser ção num contexto social diferente e na própria situação de inferioridade numérica dessa corrente dentro da Igreja.
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Este trabalho é motivado por uma questão básica, presente, atual: A família nuclear estaria sofrendo uma transformação em sua organização. Especificamente a dissolubilidade dos laços matrimoniais estaria contribuindo para uma diferente ordenação das relações de parentesco. O modelo familiar proposto, aqui no Brasil, pela Igreja e pela higiene, como procuramos demonstrar no texto, está, ao menos no que diz respeito à classe média da população, sendo descaracterizado por um tipo de relacionamento afetivo diverso do casamento tradicional "até que a morte os separe". Esta pergunta se amplia numa questão maior: ou a organização familiar transforma-se através da história, através das diferentes formações sociais, ou a família nuclear, objeto da nossa pesquisa, é um sempre-existente; ou seja, desde que o homem se aculturou a forma de organização familiar se restringiu, com variações que não passariam de meras exceções, meros desvios da estrutura primordial (a família restrita), como querem alguns autores? A nossa resposta a esta questão é claramente a favor do ponto de vista que afirma a transformação da organização familiar através dos tempos, portanto através da história, e o que é mais importante, através de diferentes formações sociais. Assim sendo, fomos levados, não só pela nossa prática, mas principalmente pela íntima ligação que a pesquisa histórica revela entre o surgimento da psicanálise e a sedimentação do modelo da família restrita, pelo novo poder de "gerir a vida", ou seja, um poder que, ao invés de tirar a vida daqueles que não o servem a contento, se interessa em extrair da vida tudo que de melhor ela pode dar, um poder a quem interessa uma qualidade cada vez maior de corpos, a fim de explorar a maior quantidade possível de produção. A família por si só é um problema. Trata-se de uma instituição que obriga a todas as ciências humanas, inclusive a medicina, a se depararem com ela em suas respectivas práticas, seja esta prática empírica ou teórica. Daí, por tratar-se de um trabalho teórico, tornou-se necessário percorrer vários saberes, os mais notáveis no nosso entender, para poder atingir os nossos objetivos.
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Trabalhar embarcado no mesmo navio, pode representar um desafio para os tripulantes estrangeiros e brasileiros da empresa Alfa Navegações, devido às diferenças de valores e crenças dessas culturas manifestas no dia a dia desta tripulação marítima. O principal objetivo nesta dissertação é sinalizar impactos na socialização do convívio a bordo entre tripulação mista. Esta pesquisa investigou a construção de um cotidiano intercultural a partir da convivência entre brasileiros e estrangeiros na filial brasileira da empresa Alfa Navegações. O marco teórico foi construído por meio de fundamentos sobre cultura organizacional, relações interculturais e cultura brasileira para compreensão e análise do cotidiano. A metodologia de pesquisa adotada neste trabalho foi o estudo de caso, com ênfase qualitativa. Foi utilizada a entrevista semiestruturada como instrumento principal de coleta de dados. Concluiu-se que as barreiras culturais na comunicação e na adaptação dos tripulantes no convívio intercultural recaem no idioma. Isto reforça os conceitos expostos no marco teórico sobre a necessidade do treinamento intercultural e aprendizagem de outro idioma para auxiliar o convívio entre culturas diferentes. Com isso, notou-se a necessidade de aprender a lidar com outras culturas, tendo em vista o novo cenário internacional, devido ao aumento do trânsito de pessoas e de ideias de fontes culturais diferentes, e que nas relações sociais a questão intercultural tornou-se crucial. Isto ocorre não somente com aqueles que aceitam o desafio de viver ou trabalhar no exterior, mas também com aqueles que recebem estes profissionais e com eles convivem no cotidiano.