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Libros sobre el tema "Processus convectifs"

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Publicado: 23 de febrero de 2024

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1

Gao, Shouting. Cloud-resolving modeling of convective processes. [Dordrecht]: Springer, 2008.

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2

Li, Xiaofan y Shouting Gao. Cloud-Resolving Modeling of Convective Processes. Cham: Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-26360-1.

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3

Gao, Shouting y Xiaofan Li. Cloud-Resolving Modeling of Convective Processes. Dordrecht: Springer Netherlands, 2008. http://dx.doi.org/10.1007/978-1-4020-8276-4.

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4

NATO Advanced Study Institute on Disorder and Mixing (1987 Cargèse, France). Disorder and mixing: Convection, diffusion, and reaction in random materials and processes. Dordrecht: Kluwer Academic Publishers, 1988.

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5

Leal, L. Gary. Laminar flow and convective transport processes: Scaling principles and asymptotic analysis. Boston: Butterworth-Heinemann, 1992.

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6

S, Figliola R., Kaviany M, Ebadian M. A, American Society of Mechanical Engineers. Winter Meeting y American Society of Mechanical Engineers. Heat Transfer Division., eds. Convection heat transfer and transport processes: Presented at the Winter Annual Meeting of the American Society of Mechanical Engineers, San Francisco, California, December 10-15, 1989. New York, N.Y: The Society, 1989.

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7

Zhang, Yanwu. Spectral feature classification of oceanographic processes using an autonomous underwater vehicle. Cambridge, Mass: Massachusetts Institute of Technology, 2000.

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8

Meeting, American Society of Mechanical Engineers Winter. Bifurcation phenomena in thermal processes and convection: Presented at the Winter Annual Meeting of the American Society of Mechanical Engineers, Boston, Massachusetts, December 13-20, 1987. New York, N.Y. (345 E. 47th St., New York 10017): ASME, 1987.

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9

Ruedas, Thomas. Convection and melting processes in a mantle plume under a spreading ridge, with application to the Iceland plume. Berlin: Logos Berlin, 2004.

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10

S, Kain John y United States. National Aeronautics and Space Administration., eds. Annual performance report for the period 15 April 1996 - 14 April 1997 for NASA grant no. NAG 5-2927 entitled evaluating and understanding parameterized convective processes and their role in the development of mesoscale precipitation systems. University Park, PA: Pennsylvania State University, Office of Sponsored Programs, 1997.

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11

Micro ways: Recipes for busy days, lazy days, holidays, every day : includes convection/microwave recipes and tips, plus food processor techniques. Montreal, Canada: J & N Pub. Ltd., 1989.

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12

Li, Xiaofan. Cloud-Resolving Modeling of Convective Processes. Springer, 2018.

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13

Laminar Flow and Convective Transport Processes. Elsevier, 1992. http://dx.doi.org/10.1016/c2009-0-26910-8.

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14

Li, Xiaofan y Shouting Gao. Cloud-Resolving Modeling of Convective Processes. Springer, 2009.

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15

Mesoscale-Convective Processes in the Atmosphere. Cambridge Univ Pr, 2013.

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16

Li, Xiaofan y Shouting Gao. Cloud-Resolving Modeling of Convective Processes. Springer, 2016.

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17

Li, Xiaofan y Shouting Gao. Cloud-Resolving Modeling of Convective Processes. Springer Netherlands, 2010.

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18

Trapp, Robert J. Mesoscale-Convective Processes in the Atmosphere. Cambridge University Press, 2013.

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19

Trapp, Robert J. Mesoscale-Convective Processes in the Atmosphere. Cambridge University Press, 2013.

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20

Trapp, Robert J. Mesoscale-Convective Processes in the Atmosphere. Cambridge University Press, 2013.

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21

Li, Xiaofan y Shouting Gao. Cloud-Resolving Modeling of Convective Processes. Springer London, Limited, 2016.

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22

Leal, L. Gary. Advanced Transport Phenomena: Fluid Mechanics and Convective Transport Processes. Cambridge University Press, 2007.

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23

Leal, L. Gary. Advanced Transport Phenomena: Fluid Mechanics and Convective Transport Processes. Cambridge University Press, 2010.

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24

Leal, L. Gary. Advanced Transport Phenomena: Fluid Mechanics and Convective Transport Processes. Cambridge University Press, 2007.

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25

Leal, L. Gary. Advanced Transport Phenomena: Fluid Mechanics and Convective Transport Processes. Cambridge University Press, 2007.

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26

Leal, L. Gary. Advanced Transport Phenomena: Fluid Mechanics and Convective Transport Processes. Cambridge University Press, 2010.

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27

Leal, L. Gary. Advanced Transport Phenomena: Fluid Mechanics and Convective Transport Processes. Cambridge University Press, 2012.

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28

Luo, Zhengzhao Johnny, George Tselioudis y William B. Rossow. Studies of Cloud, Convection and Precipitation Processes Using Satellite Observations. WORLD SCIENTIFIC, 2022. http://dx.doi.org/10.1142/12862.

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29

Luo, Zhengzhao Johnny, George Tselioudis y William Brigance Rossow. Studies of Cloud, Convection and Precipitation Processes Using Satellite Observations. World Scientific Publishing Co Pte Ltd, 2022.

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30

Luo, Zhengzhao Johnny, George Tselioudis y William Brigance Rossow. Studies of Cloud, Convection and Precipitation Processes Using Satellite Observations. World Scientific Publishing Co Pte Ltd, 2022.

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31

Brenner, Howard. Laminar Flow and Convective Transport Processes: Scaling Principles and Asymptotic Analysis. Elsevier Science & Technology Books, 2016.

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32

Pomeau, Yves, J. P. Nadal y E. Guyon. Disorder and Mixing: Convection, Diffusion and Reaction in Random Materials and Processes. Springer, 2012.

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33

Disorder and Mixing: Convection, Diffusion and Reaction in Random Materials and Processes. Springer, 2012.

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34

(Editor), E. Guyon, J. P. Nadal (Editor) y Yves Pomeau (Editor), eds. Disorder and Mixing: Convection, Diffusion and Reaction in Random Materials and Processes (NATO Science Series E: (closed)). Springer, 1988.

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35

Advanced Transport Phenomena: Fluid Mechanics and Convective Transport Processes (Cambridge Series in Chemical Engineering). Cambridge University Press, 2007.

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36

Chung, Se-Won. Analysis of radiative and convective energy transport processes in ultrahigh temperature vapor core reactors. 1992.

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37

Birfurcation Phenomena in Thermal Processes and Convection (Book No G00417-Htd V94-Amd V89). Amer Society of Mechanical, 1987.

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38

Pardo, Samiro Khodayar. High-resolution Analysis of the Initiation of Deep Convection Forced by Boundary-layer Processes. Saint Philip Street Press, 2020.

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39

National Aeronautics and Space Administration (NASA) Staff. Evaluating and Understanding Parameterized Convective Processes and Their Role in the Development of Mesoscale Precipitation Systems. Independently Published, 2018.

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40

Locatelli, Francesco, Celestina Manzoni, Giuseppe Pontoriero, Vincenzo La Milia y Salvatore Di Filippo. Haemofiltration and haemodiafiltration. Editado por Jonathan Himmelfarb. Oxford University Press, 2018. http://dx.doi.org/10.1093/med/9780199592548.003.0260_update_001.

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Many observational studies have consistently shown that high-flux haemodialysis (hf-HD) has positive effects on the survival and morbidity of uraemic patients when compared with low-flux haemodialysis, and mainly considering the results of Membrane Permeability Outcome (MPO) studies there is evidence favouring high-flux treatments. A further improvement in convective treatments is represented by the on-line modality. On-line preparation from fresh dialysate by a cold-sterilizing filtration process is a cost-effective method of providing large volumes of infusion solution. Randomized, controlled, large-sized trials with long follow-up in haemofiltration (HF) are unfortunately lacking, possibly suggesting the difficulties in performing these trials, mainly in providing the same urea Kt/V considered adequate in HD. On-line haemodiafiltration (HDF) is considered the most efficient technique of using high-flux membranes, and clearances of small solutes like urea are higher in HDF than in HF and of middle solutes like β‎‎‎2-microglobulin are higher than in hf-HD. Thus HDF, as a strategy based on simultaneous diffusive and convective transport, may combine the beneficial effects of diffusive standard HD with the possible advantages of convective HF. Five large, randomized controlled trials just concluded are inconclusive in definitively clarifying the impact of on-line HDF on chronic kidney disease stage 5 patient outcomes.
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41

Potter, Stephen Edward. Modelling of three-dimensional transient conjugate convection-conduction-radiation heat transfer processes and turbulence in building spaces. 1998.

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42

Zeitlin, Vladimir. Geophysical Fluid Dynamics. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198804338.001.0001.

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The book explains the key notions and fundamental processes in the dynamics of the fluid envelopes of the Earth (transposable to other planets), and methods of their analysis, from the unifying viewpoint of rotating shallow-water model (RSW). The model, in its one- or two-layer versions, plays a distinguished role in geophysical fluid dynamics, having been used for around a century for conceptual understanding of various phenomena, for elaboration of approaches and methods, to be applied later in more complete models, for development and testing of numerical codes and schemes of data assimilations, and many other purposes. Principles of modelling of large-scale atmospheric and oceanic flows, and corresponding approximations, are explained and it is shown how single- and multi-layer versions of RSW arise from the primitive equations by vertical averaging, and how further time-averaging produces celebrated quasi-geostrophic reductions of the model. Key concepts of geophysical fluid dynamics are exposed and interpreted in RSW terms, and fundamentals of vortex and wave dynamics are explained in Part 1 of the book, which is supplied with exercises and can be used as a textbook. Solutions of the problems are available at Editorial Office by request. In-depth treatment of dynamical processes, with special accent on the primordial process of geostrophic adjustment, on instabilities in geophysical flows, vortex and wave turbulence and on nonlinear wave interactions follows in Part 2. Recently arisen new approaches in, and applications of RSW, including moist-convective processes constitute Part 3.
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43

Kolmičkovs, Antons. Electric Field Effect on Combustion of Pelletized Biomass in Swirling Flow. RTU Press, 2022. http://dx.doi.org/10.7250/9789934227257.

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The Doctoral Thesis examines the control of the swirling flame flow dynamics with an external static electric field by firing the gaseous products of thermal decomposition of pelletized straw, woody biomass, and peat with the aim of more efficient heat production with a decrease of flue gas emissions. The intensification of the downward vortex in the electric field has been determined, ensuring improved mixing of the air vortex with the biomass thermal decomposition gas flow, intensifying the convective mass transfer towards the heating surfaces, and increasing the amount of heat energy produced in the biomass thermochemical conversion process.
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44

Speer, Kevin y Scott Goodrick, eds. Wildland Fire Dynamics. Cambridge University Press, 2022. http://dx.doi.org/10.1017/9781108683241.

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Wildland fires are among the most complicated environmental phenomena to model. Fire behavior models are commonly used to predict the direction and rate of spread of wildland fires based on fire history, fuel, and environmental conditions; however, more sophisticated computational fluid dynamic models are now being developed. This quantitative analysis of fire as a fluid dynamic phenomenon embedded in a highly turbulent flow is beginning to reveal the combined interactions of the vegetative structure, combustion-driven convective effects, and atmospheric boundary layer processes. This book provides an overview of the developments in modeling wildland fire dynamics and the key dynamical processes involved. Mathematical and dynamical principles are presented, and the complex phenomena that arise in wildland fire are discussed. Providing a state-of-the-art survey, it is a useful reference for scientists, researchers, and graduate students interested in wildland fire behavior from a broad range of fields.
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45

Stachowska-Pietka, Joanna, Jacek Waniewski y Bengt Lindholm. Peritoneal dialysis. Editado por Jonathan Himmelfarb. Oxford University Press, 2015. http://dx.doi.org/10.1093/med/9780199592548.003.0264.

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The principles of peritoneal dialysis are based on the physiological processes and their driving forces which permit the exchange of water (by ultrafiltration and fluid absorption) and solutes (by diffusion and convective transport) between the peritoneal microvasculature and the dialysate. In peritoneal dialysis, the peritoneal transport system—mesenchymal cells, interstitium, microvasculature, and lymphatics—is repeatedly exposed to high concentrations of an osmotic agent, and a volume load, leading to increased intraperitoneal hydrostatic and osmotic pressure. This results in immediate as well as long-term structural and functional changes of the peritoneal transport system. Clinical tests supplemented with mathematical modelling have been developed to monitor the quantitative characteristics of the peritoneal transport system, allowing detection and diagnosis of various problems and guidance when predicting consequences of changes in prescription.
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46

Furbish, David Jon. Fluid Physics in Geology. Oxford University Press, 1997. http://dx.doi.org/10.1093/oso/9780195077018.001.0001.

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Fluid Physics in Geology is aimed at geology students who are interested in understanding fluid behavior and motion in the context of a wide variety of geological problems, and who wish to pursue related work in fluid physics. The book provides an introductory treatment of the physical and dynamical behaviors of fluids by focusing first on how fluids behave in a general way, then looking more specifically at how they are involved in certain geological processes. The text is written so students may concentrate on the sections that are most relevant to their own needs. Helpful problems following each chapter illustrate applications of the material to realistic problems involving groundwater flows, magma dynamics, open-channel flows, and thermal convection. Fluid Physics in Geology is ideal for graduate courses in all areas of geology, including hydrology, geomorphology, sedimentology, and petrology.
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47

Atlanta, Ga ). American Society of Mechanical Engineers Winter Meeting (1991 :. Convection Heat Transfer and Transport Processes: Presented at the Winter Annual Meeting of the American Society of Mechanical Engineers, San Francisco, ... of the Asme Heat Transfer Division). Amer Society of Mechanical, 1989.

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48

Mast, Christof, Friederike Möller, Moritz Kreysing, Severin Schink, Benedikt Obermayer, Ulrich Gerland y Dieter Braun. Toward living nanomachines. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780199674923.003.0039.

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How does inanimate matter become transformed into animate matter? Living systems evolve by replication and selection at the molecular level and this chapter considers how to establish a synthetic, minimal system that can support molecular evolution and thus life. Molecular evolution cannot be explained by starting with high concentrations of activated chemicals that react toward their chemical equilibrium; persistent non-equilibria are required to maintain continuous reactivity and we especially consider thermal gradients as an early driving force for Darwinian molecular evolution. The temperature difference across water-filled compartments implements a laminar fluid convection with periodic temperature oscillations that allow for the melting and replication of DNA. Simultaneously, dissolved molecules are moved along the thermal gradient by an effect called thermophoresis. The combined result is an efficient molecule trap that exponentially favors long over short DNA and thus maintains complexity. Future experiments will reveal how thermal gradients could actively drive the Darwinian process of replication and selection.
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49

Wang, Bin. Intraseasonal Modulation of the Indian Summer Monsoon. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.616.

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The strongest Indian summer monsoon (ISM) on the planet features prolonged clustered spells of wet and dry conditions often lasting for two to three weeks, known as active and break monsoons. The active and break monsoons are attributed to a quasi-periodic intraseasonal oscillation (ISO), which is an extremely important form of the ISM variability bridging weather and climate variation. The ISO over India is part of the ISO in global tropics. The latter is one of the most important meteorological phenomena discovered during the 20th century (Madden & Julian, 1971, 1972). The extreme dry and wet events are regulated by the boreal summer ISO (BSISO). The BSISO over Indian monsoon region consists of northward propagating 30–60 day and westward propagating 10–20 day modes. The “clustering” of synoptic activity was separately modulated by both the 30–60 day and 10–20 day BSISO modes in approximately equal amounts. The clustering is particularly strong when the enhancement effect from both modes acts in concert. The northward propagation of BSISO is primarily originated from the easterly vertical shear (increasing easterly winds with height) of the monsoon flows, which by interacting with the BSISO convective system can generate boundary layer convergence to the north of the convective system that promotes its northward movement. The BSISO-ocean interaction through wind-evaporation feedback and cloud-radiation feedback can also contribute to the northward propagation of BSISO from the equator. The 10–20 day oscillation is primarily produced by convectively coupled Rossby waves modified by the monsoon mean flows. Using coupled general circulation models (GCMs) for ISO prediction is an important advance in subseasonal forecasts. The major modes of ISO over Indian monsoon region are potentially predictable up to 40–45 days as estimated by multiple GCM ensemble hindcast experiments. The current dynamical models’ prediction skills for the large initial amplitude cases are approximately 20–25 days, but the prediction of developing BSISO disturbance is much more difficult than the prediction of the mature BSISO disturbances. This article provides a synthesis of our current knowledge on the observed spatial and temporal structure of the ISO over India and the important physical processes through which the BSISO regulates the ISM active-break cycles and severe weather events. Our present capability and shortcomings in simulating and predicting the monsoon ISO and outstanding issues are also discussed.
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50

Yang, Kun. Observed Regional Climate Change in Tibet over the Last Decades. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.587.

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The Tibetan Plateau (TP) is subjected to strong interactions among the atmosphere, hydrosphere, cryosphere, and biosphere. The Plateau exerts huge thermal forcing on the mid-troposphere over the mid-latitude of the Northern Hemisphere during spring and summer. This region also contains the headwaters of major rivers in Asia and provides a large portion of the water resources used for economic activities in adjacent regions. Since the beginning of the 1980s, the TP has undergone evident climate changes, with overall surface air warming and moistening, solar dimming, and decrease in wind speed. Surface warming, which depends on elevation and its horizontal pattern (warming in most of the TP but cooling in the westernmost TP), was consistent with glacial changes. Accompanying the warming was air moistening, with a sudden increase in precipitable water in 1998. Both triggered more deep clouds, which resulted in solar dimming. Surface wind speed declined from the 1970s and started to recover in 2002, as a result of atmospheric circulation adjustment caused by the differential surface warming between Asian high latitudes and low latitudes.The climate changes over the TP have changed energy and water cycles and has thus reshaped the local environment. Thermal forcing over the TP has weakened. The warming and decrease in wind speed lowered the Bowen ratio and has led to less surface sensible heating. Atmospheric radiative cooling has been enhanced, mainly through outgoing longwave emission from the warming planetary system and slightly enhanced solar radiation reflection. The trend in both energy terms has contributed to the weakening of thermal forcing over the Plateau. The water cycle has been significantly altered by the climate changes. The monsoon-impacted region (i.e., the southern and eastern regions of the TP) has received less precipitation, more evaporation, less soil moisture and less runoff, which has resulted in the general shrinkage of lakes and pools in this region, although glacier melt has increased. The region dominated by westerlies (i.e., central, northern and western regions of the TP) received more precipitation, more evaporation, more soil moisture and more runoff, which together with more glacier melt resulted in the general expansion of lakes in this region. The overall wetting in the TP is due to both the warmer and moister conditions at the surface, which increased convective available potential energy and may eventually depend on decadal variability of atmospheric circulations such as Atlantic Multi-decadal Oscillation and an intensified Siberian High. The drying process in the southern region is perhaps related to the expansion of Hadley circulation. All these processes have not been well understood.
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