995 resultados para célula do cumulus


Relevância:

20.00% 20.00%

Publicador:

Resumo:

Se expone el proceso de cultivo microbiológico (PCU), cada vez más desarrollado, para el cultivo de células proteínicas unitarias (SCP) para la alimentación de animales y fortificación del alimento de los seres humanos, como una alternativa a la escasez de proteínas presentes en los alimentos. Supone una fabricación sencilla de este constituyente vital alimenticio a un coste muy bajo.

Relevância:

20.00% 20.00%

Publicador:

Resumo:

El artículo forma parte de un monográfico de la revista dedicado a la fase inicial de la secuencia formativa

Relevância:

20.00% 20.00%

Publicador:

Resumo:

El libro de texto como tal viene siendo una representación externa, temática relevante en el campo de la enseñanza de las ciencias desde la historia hasta el mundo de hoy, y es definida según Greca (2000) citado en Henao (2006) como cualquier notación signo o conjunto de símbolos que representan algo del mundo exterior. Existen dos tipos de representaciones, las externas que a su vez se dividen en lingüísticas e icónicas y las internas, pero, de acuerdo a los asuntos que son objeto de estudio en este trabajo, solo se tendrán presente las primeras

Relevância:

20.00% 20.00%

Publicador:

Resumo:

This paper considers the relationship between the mean temperature and humidity profiles and the fluxes of heat and moisture at cloud base and the base of the inversion in the cumulus-capped boundary layer. The relationships derived are based on an approximate form of the scalar-flux budget and the scaling properties of the turbulent kinetic energy (TKE) budget. The scalar-flux budget gives a relationship between the change in the virtual potential temperature across either the cloud base transition zone or the inversion and the flux at the base of the layer. The scaling properties of the TKE budget lead to a relationship between the heat and moisture fluxes and the mean subsaturation through the liquid-water flux. The 'jump relation' for the virtual potential temperature at cloud base shows the close connection between the cumulus mass flux in the cumulus-capped boundary layer and the entrainment velocity in the dry-convective boundary layer. Gravity waves are shown to be an important feature of the inversion.

Relevância:

20.00% 20.00%

Publicador:

Resumo:

Scalar-flux budgets have been obtained from large-eddy simulations (LESs) of the cumulus-capped boundary layer. Parametrizations of the terms in the budgets are discussed, and two parametrizations for the transport term in the cloud layer are proposed. It is shown that these lead to two models for scalar transports by shallow cumulus convection. One is equivalent to the subsidence detrainment form of convective tendencies obtained from mass-flux parametrizations of cumulus convection. The second is a flux-gradient relationship that is similar in form to the non-local parametrizations of turbulent transports in the dry-convective boundary layer. Using the fluxes of liquid-water potential temperature and total water content from the LES, it is shown that both models are reasonable diagnostic relations between fluxes and the vertical gradients of the mean fields. The LESs used in this study are for steady-state convection and it is possible to treat the fluxes of conserved thermodynamic variables as independent, and ignore the effects of condensation. It is argued that a parametrization of cumulus transports in a model of the cumulus-capped boundary layer should also include an explicit representation of condensation. A simple parametrization of the liquid-water flux in terms of conserved variables is also derived.

Relevância:

20.00% 20.00%

Publicador:

Resumo:

Wagner and Graf (2010) derive a population evolution equation for an ensemble of convective plumes, an analogue with the Lotka–Volterra equation, from the energy equations for convective plumes provided by Arakawa and Schubert (1974). Although their proposal is interesting, as the present note shows, there are some problems with their derivation.

Relevância:

20.00% 20.00%

Publicador:

Resumo:

We propose a new modelling framework suitable for the description of atmospheric convective systems as a collection of distinct plumes. The literature contains many examples of models for collections of plumes in which strong simplifying assumptions are made, a diagnostic dependence of convection on the large-scale environment and the limit of many plumes often being imposed from the outset. Some recent studies have sought to remove one or the other of those assumptions. The proposed framework removes both, and is explicitly time-dependent and stochastic in its basic character. The statistical dynamics of the plume collection are defined through simple probabilistic rules applied at the level of individual plumes, and van Kampen's system size expansion is then used to construct the macroscopic limit of the microscopic model. Through suitable choices of the microscopic rules, the model is shown to encompass previous studies in the appropriate limits, and to allow their natural extensions beyond those limits.

Relevância:

20.00% 20.00%

Publicador:

Resumo:

In situ high resolution aircraft measurements of cloud microphysical properties were made in coordination with ground based remote sensing observations of a line of small cumulus clouds, using Radar and Lidar, as part of the Aerosol Properties, PRocesses And InfluenceS on the Earth's climate (APPRAISE) project. A narrow but extensive line (~100 km long) of shallow convective clouds over the southern UK was studied. Cloud top temperatures were observed to be higher than −8 °C, but the clouds were seen to consist of supercooled droplets and varying concentrations of ice particles. No ice particles were observed to be falling into the cloud tops from above. Current parameterisations of ice nuclei (IN) numbers predict too few particles will be active as ice nuclei to account for ice particle concentrations at the observed, near cloud top, temperatures (−7.5 °C). The role of mineral dust particles, consistent with concentrations observed near the surface, acting as high temperature IN is considered important in this case. It was found that very high concentrations of ice particles (up to 100 L−1) could be produced by secondary ice particle production providing the observed small amount of primary ice (about 0.01 L−1) was present to initiate it. This emphasises the need to understand primary ice formation in slightly supercooled clouds. It is shown using simple calculations that the Hallett-Mossop process (HM) is the likely source of the secondary ice. Model simulations of the case study were performed with the Aerosol Cloud and Precipitation Interactions Model (ACPIM). These parcel model investigations confirmed the HM process to be a very important mechanism for producing the observed high ice concentrations. A key step in generating the high concentrations was the process of collision and coalescence of rain drops, which once formed fell rapidly through the cloud, collecting ice particles which caused them to freeze and form instant large riming particles. The broadening of the droplet size-distribution by collision-coalescence was, therefore, a vital step in this process as this was required to generate the large number of ice crystals observed in the time available. Simulations were also performed with the WRF (Weather, Research and Forecasting) model. The results showed that while HM does act to increase the mass and number concentration of ice particles in these model simulations it was not found to be critical for the formation of precipitation. However, the WRF simulations produced a cloud top that was too cold and this, combined with the assumption of continual replenishing of ice nuclei removed by ice crystal formation, resulted in too many ice crystals forming by primary nucleation compared to the observations and parcel modelling.

Relevância:

20.00% 20.00%

Publicador:

Resumo:

Tropical deep convection exhibits a variety of levels of aggregation over a wide range of scales. Based on a multisatellite analysis, the present study shows at mesoscale that different levels of aggregation are statistically associated with differing large-scale atmospheric states, despite similar convective intensity and large-scale forcings. The more aggregated the convection, the dryer and less cloudy the atmosphere, the stronger the outgoing longwave radiation, and the lower the planetary albedo. This suggests that mesoscale convective aggregation has the potential to affect couplings between moisture and convection and between convection, radiation, and large-scale ascent. In so doing, aggregation may play a role in phenomena such as “hot spots” or the Madden-Julian Oscillation. These findings support the need for the representation of mesoscale organization in cumulus parameterizations; most parameterizations used in current climate models lack any such representation. The ability of a cloud system-resolving model to reproduce observed relationships suggests that such models may be useful to guide attempts at parameterizations of convective aggregation.

Relevância:

20.00% 20.00%

Publicador:

Resumo:

Este trabalho apresenta o desenvolvimento de um sistema de medição para a análise biomecânica da força desenvolvida durante a escovação dental, com aquisição e processamento de dados de dinamometria para a análise da escovação dental como um processo eficaz de higiene bucal. Foi desenvolvida uma célula de carga com extensômetros de resistência elétrica, montada em uma escova dental. A célula de carga foi construída com 2 Strain Gages montados em meia ponte de Wheatstone, medindo força em flexão, e 4 Strain Gages montados em ponte completa de Wheatstone medindo força de torque. A aquisição dos dados e análise foi feita através do software SAD2. Foram selecionados 6 indivíduos, dois do sexo masculino e 4 do sexo feminino, todos destros, e instruídos a escovarem os dentes por 1 minuto. Os valores medidos para a força de flexão média variam de 24gf à 526gf e para o esforço de torque médio de –76gfmm à 1890gfmm. A célula de carga desenvolvida mostrou-se repetitiva, com boa sensibilidade e confiável com um erro em flexão de 2,7% e 5,5% em torque. A célula de carga apresentou resultados semelhantes a de outros trabalhos publicados anteriormente, sendo estes válidos para uma análise quantitativa inicial no processo de escovação.

Relevância:

20.00% 20.00%

Publicador:

Resumo:

No presente estudo, foi investigado o mecanismo pelo qual, o isoproterenol hiperpolariza o potencial de membrana (PM) da célula de Sertoli em túbulos seminíferos de ratos, com quinze dias de idade (imaturos). Foram analisadas a modificação do potencial de membrana e a resistência, utilizando-se a técnica de registro intracelular. O isoproterenol (2x10-6M) induziu uma hiperpolarização imediata e significativa na membrana da célula de Sertoli. O antagonista β2-adrenérgico butoxamina (1x10-6M) anulou a ação do isoproterenol. O antagonista β1-adrenérgico metoprolol (1x10-6M) teve efeito de reduzir a ação do isoproterenol, porém sem ser significativo. A inibição dos canais K+ATP, com a sulfoniluréia glibenclamida, suprimiu a ação do isoproterenol. A testosterona, a qual atua despolarizando o potencial de membrana, através do fechamento de canais K+ATP, via PLC-PIP2, impediu a hiperpolarização produzida pelo agonista β-adrenérgico. Os policátions como: espermina e LaCl3 (cloreto de lantâno) reverteram o efeito hiperpolarizante do isoproterenol, despolarizando o potencial de membrana, provavelmente através de interações iônicas que neutralizam a ação do agonista β-adrenérgico nos canais K+ATP. O agonista da adenilato ciclase, forscolina (1x10-7M), rapidamente hiperpolariza o potencial de membrana da célula de Sertoli, mimetizando o efeito do isoproterenol; db-AMPc também hiperpolariza o potencial de membrana destas células. Estes efeitos indicam que o isoproterenol age nos canais K+ATP, provavelmente, envolvendo a cascata: receptor β-adrenérgico/Gs/AC/AMPc/PKA. Estes resultados sugerem que a hiperpolarização induzida por isoproterenol é mediada pela abertura de canais K+ATP, em células de Sertoli. Esta hiperpolarização β-adrenérgica, provavelmente, tem uma papel fisiológico, na modulação do potencial de membrana, opondo-se à despolarização produzida pela testosterona, através do fechamento dos canais K+ATP.