Dissertations / Theses on the topic 'Wind shear'
Create a spot-on reference in APA, MLA, Chicago, Harvard, and other styles
Consult the top 50 dissertations / theses for your research on the topic 'Wind shear.'
Next to every source in the list of references, there is an 'Add to bibliography' button. Press on it, and we will generate automatically the bibliographic reference to the chosen work in the citation style you need: APA, MLA, Harvard, Chicago, Vancouver, etc.
You can also download the full text of the academic publication as pdf and read online its abstract whenever available in the metadata.
Browse dissertations / theses on a wide variety of disciplines and organise your bibliography correctly.
Belderrain, José Luiz Rocha. "Desempenho ótimo de aviões voando em "wind-shear"." Instituto Tecnológico de Aeronáutica, 1991. http://www.bd.bibl.ita.br/tde_busca/arquivo.php?codArquivo=1785.
Full textGuldsten, Jon Didriksen. "Influence on wind shear and turbulence in flow over obstacles." Thesis, Norwegian University of Science and Technology, Department of Energy and Process Engineering, 2010. http://urn.kb.se/resolve?urn=urn:nbn:no:ntnu:diva-10029.
Full textA wind tunnel study of speed-up effects above the very crest of a sharp-edged escarpment and a hill peak in a simulated atmospheric boundary layer has been carried out. It was desired to do a part-deep simulation of an atmospheric boundary that could be found above sea or coastal area exposed to the open sea. Because of the limited work section length was it used a modified roughness, barrier and mixing-device developed by Counihan to accelerate the boundary layer growth. The mean velocity, integral length scales, power spectrum and turbulence intensity in the simulated boundary layer were compared with full scale empirical data. It showed good agreement except for the turbulence intensity which was too low. Speed-up effects for the mean horizontal velocity and the longitudinal turbulence intensity above the very crest of an escarpment and a hill peak were investigated in the simulated atmospheric boundary layer. From the results it was observed that the speed-up effect gave a decrease in the turbulence intensity and a more uniform profile with height. A considerably increase of the horizontal mean velocity in the lowest part of the flow was also observed. Scaled-up data from the wind tunnel experiment were compared with estimations from the Norwegian standard and potential flow with varying degree of agreement.
Zarraonandia, Gaizka. "Influence on wind shear and turbulence in flow over obstacles." Thesis, Norwegian University of Science and Technology, Department of Energy and Process Engineering, 2010. http://urn.kb.se/resolve?urn=urn:nbn:no:ntnu:diva-10165.
Full textA wind tunnel study of speed-up effects above the very crest of a sharp-edged escarpment and a hill peak in a simulated atmospheric boundary layer has been carried out. It was desired to do a part-depth simulation of an atmospheric boundary that could be found above sea or coastal area exposed to the open sea. Because of the limited work section length it was used a modified roughness, barrier and mixing-device method developed by Counihan to accelerate the boundary layer growth. The mean velocity, integral length scales, power spectrum and turbulence intensity in the simulated boundary layer were compared with full scale empirical data. It showed good agreement except for the turbulence intensity which was too low. Speed-up effects for the mean horizontal velocity and the longitudinal turbulence intensity above the very crest of an escarpment and a hill peak were investigated in the simulated atmospheric boundary layer. From the results it was observed that the speed-up effect gave a decrease in the turbulence intensity and a more uniform profile with height. In addition, it was observed a considerably increase of the horizontal mean velocity in the lowest part of the atmospheric boundary layer. Scaled-up data from the wind tunnel experiment were compared with estimations from the Norwegian standard and potential flow with varying degree of agreement.
Caeiro, Olaio Valente Maria Antonia. "Effects of directional wind shear on orographic gravity wave drag." Thesis, University of Reading, 2000. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.325212.
Full textIndriyanto, Toto. "Nonlinear flight control system for lateral manoeuvres in wind shear." Thesis, Cranfield University, 2000. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.273525.
Full textGuarino, Maria Vittoria. "Mountain wave breaking in atmospheric flows with directional wind shear." Thesis, University of Reading, 2017. http://centaur.reading.ac.uk/75850/.
Full textBaseer, Mohammed Abdul. "Wind resource assessment and GIS-based site selection methodology for efficient wind power deployment." Thesis, University of Pretoria, 2017. http://hdl.handle.net/2263/61314.
Full textThesis (PhD)--University of Pretoria, 2017.
Mechanical and Aeronautical Engineering
PhD
Unrestricted
Stival, Leandro Jose Lemes. "A study on wind assessment on the wind power performance : wind shear and turbulence intensity effects besides the wake modeling for a single wind turbine." reponame:Repositório Institucional da UFPR, 2017. http://hdl.handle.net/1884/49088.
Full textCoorientador : Prof. Dr. Fernando Oliveira Andrade
Dissertação (mestrado) - Universidade Federal do Paraná, Setor de Tecnologia, Programa de Pós-Graduação em Engenharia de Recursos Hídricos e Ambiental. Defesa: Curitiba, 04/04/2017
Inclui referências : f.91-97
Resumo: A energia eólica cresceu significativamente, porém a eficiência de geração da fonte eólica gira em torno de 30% da energia cinética disponível no vento. Por este motivo é de extrema importância que estudos sejam elaborados afim de aumentar a eficiência na geração de energia. Este estudo visa investigar odesempenho da geração de energia eólica em dois parques eólicos situadosna América do Norte, através da investigação dos dados de vento e modelagem da esteira turbulenta. Os dados analisados são provenientes da turbina, SCADA, e dados coletados pelo LiDAR. A partir das análises dos dados de vento foram estimados parâmetros como tensão de cisalhamento do vento, rosa dos ventos, perfil de velocidade do vento e intensidade de turbulência. Portanto, aumentando a intensidade de turbulência, a energia gerada é superestimada em moderadas velocidades do vento e subestimada em altas velocidades do vento. Enquanto isso, os coeficientes de cisalhamento do vento variaram entre 0 e 0.2 para altas velocidades. Além disso, coeficientes de cisalhamento com valores elevados, perto de 0.4, foram encontrados em baixas velocidades do vento. Este trabalho visou também comparar modelos de esteira turbulenta de PARK (Jensen), Frandsen, Larsen and Eddy Viscosity (Ainslie) com resultados obtidos pelo LiDAR, além disso foi realizado uma simulação numérica da esteira turbulenta utilizando Fluent CFD com as equações médias de Reynolds (RANS) que resolvem o modelos de duas equações diferenciais para obter a viscosidade turbulenta. A turbulência foi fechada pelo modelo ?????, sendo o modelo de esteira turbulenta desenvolvido para uma única turbina num terreno plano. O modelo de PARK obteve os melhores resultados para linha de centro longitudinal em relação as velocidades de 6 a 8 ms-1. Entretanto, para velocidade de 9 a 12 ms-1 , o modelo de EDDY VISCOSITY apresentou o melhor desempenho. As análises de seção transversal apresentaram o modelo de PARK como melhor resultado para 500 m. Enquanto isso, para 700 m de seção transversal, o melhor desempenho foi obtido pelo modelo de LARSEN. Palavras-chave: Energia Eólica, Modelo de Esteira Turbulenta, LiDAR, Análises do Vento.
Abstract: Wind power has gained significant share in the global power production. However, the wind power output efficiency is only about 30% of the wind kinetic energy. Because of that, it is essential to study the efficiency of these power generation systems by assessing the effects that wind parameters and wakes will have on the whole system. Hence, a complete assessment of wind resources is crucial to retain full advantage of wind power. This study aims to investigate the efficiency of wind energy generation in two North American Wind Farms, through wind data investigation and wake modeling. The data analyzed are the SCADA data and the data collected by LiDAR measurements. The wind data analysis has estimated parameters as wind shear, wind rose, wind speed profile and turbulence intensity. Therefore increasing turbulence intensity the power output is overestimated at moderate wind speeds and underestimated at higher wind speeds. Meanwhile, the wind shear coefficients were found to vary between 0 and 0.2 at higher inflow velocities. High wind shear values, close to 0.4, were recorded for lower inflow velocities. The goal of the wake models is to simulate the turbine induced wind speed deficits and the ratio of restoration to the free stream velocity. This work has compared the PARK (Jensen), Frandsen, Larsen and Eddy Viscosity (Ainslie) models with LiDAR wake measurements, besides that it has performed a numerical simulation of the wind turbine wake using the Fluent CFD with the Reynolds Averaged Navier Stokes (RANS) equations that solves two differential equation model to obtain turbulent viscosity. The turbulence was closed by the ????? model, where the wake modeling has been developed for a single turbine on a flat terrain. In terms of centerline wake analysis, the PARK wake model yielded the best velocity simulations for inflow winds from 6 to 8 ms-1. However, the EDDY VISCOSITY wake model yielded the best performance for wind speed bins from 9 to 12 ms-1. The cross section wake analysis presented for the 500 m cross section, the domination by the PARK model. Meanwhile, along the 700 m cross section, the LARSEN wake model produced the best simulations. Key-words: Wind Power, Wake Modeling, LiDAR, Wind Analysis.
Sycuro, Stephen J. "Radar turbulence estimates : effects of wind shear and reflectivity factor gradients." Thesis, Massachusetts Institute of Technology, 1985. http://hdl.handle.net/1721.1/58128.
Full textMicrofiche copy available in Archives and Science.
Bibliography: leaf 43.
by Stephen J. Sycuro.
M.S.
Mu, K. L. "Investigation of tropospheric turbulence using the Adelaide VHF radar /." Title page, abstract and contents only, 1991. http://web4.library.adelaide.edu.au/theses/09SM/09smm941.pdf.
Full textSmith, Debra K. "Tropical cyclone development and intensification under moderate to strong vertical wind shear." Thesis, Monterey, California. Naval Postgraduate School, 1994. http://hdl.handle.net/10945/28618.
Full textA study was conducted to understand the physical mechanisms by which a tropical cyclone is able to develop and be maintained under moderate to strong vertical wind shear. The general approach was to describe case studies of three tropical cyclones in the western North Pacific that developed and/or intensified in the lee of another tropical cyclone. The data resources include high temporal and spatial resolution visible and infrared satellite imagery, operational subjective and objective analyses, plus special Tropical Cyclone Motion (TCM-90) high resolution (50 km) analyses and multi-quadric analyses. The three tropical cyclones developed and/or intensified under moderate to strong vertical wind shear that exceeded threshold values. The vertical wind shear was time dependent due to complex interactions with the leading tropical cyclone outflow, adjacent tropical upper tropospheric trough, and large-scale environment. Diurnal variability in strength of convection and outflow against the impinging flow led to fully exposed, partially exposed, or covered middle to lower tropospheric cyclonic circulation. Special characteristics of the monsoon trough circulation must create and sustain the tropical cyclone circulation against the tendency for the vertical wind shear to ventilate the vertical thermal and convective structure
Woo, Tak Kwong. "Transitory control of separated shear layer using impulsive jet actuation." Diss., Georgia Institute of Technology, 2014. http://hdl.handle.net/1853/52980.
Full textIannotti, Veronica. "Studio del fenomeno del "wind shear" e analisi dei principali sistemi di rilevamento." Bachelor's thesis, Alma Mater Studiorum - Università di Bologna, 2019. http://amslaurea.unibo.it/19047/.
Full textSiveski, Zlatan. "Non-linear structural analysis of shear connected cavity walls subject to wind load." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1997. http://www.collectionscanada.ca/obj/s4/f2/dsk2/ftp04/mq23496.pdf.
Full textNinnemann, Todd A. "Aspirating probes for measurement of mean concentration and fluctuating quantities in supersonic air/helium shear layer." Thesis, This resource online, 1990. http://scholar.lib.vt.edu/theses/available/etd-12232009-020346/.
Full textJacobi, Christoph, and Manfred Ern. "Gravity waves and vertical shear of zonal wind in the summer mesosphere-lower thermosphere." Universität Leipzig, 2013. https://ul.qucosa.de/id/qucosa%3A16408.
Full textAmplituden von Schwerewellen und zugehörigen Impulsflüsse werden zusammen mit Windmessungen des Meteorradars Collm analysiert. Die Impulsflussdivergenz, abgeleitet aus SABER-Temperaturprofilen, hat ein Maximum welches im solaren Minimum nach oben verschoben ist. Dadurch werden auch die Vertikalprofile des Zonalwindes und der Windscherung nach oben verschoben, wodurch die ansonsten negative Sonnenfleckenzyklusabhängigkeit des zonalen Windes in der Mesosphäre/unteren Thermosphäre im solaren Minimum umgekehrt wird.
Vessby, Johan. "Shear walls for multi-storey timber buildings." Licentiate thesis, Växjö University, School of Technology and Design, 2008. http://urn.kb.se/resolve?urn=urn:nbn:se:vxu:diva-2420.
Full textWind loads acting on wooden building structures need to be dealt with adequately in order to ensure that neither the serviceability limit state nor the ultimate limit state is exceeded. For the structural designer of tall buildings, avoiding the possibly serious consequences of heavy wind loading while taking account at the same time of the effects of gravitation can be a real challenge. Wind loads are usually no major problem for low buildings, such as one- to two-storey timber structures involving ordinary walls made by nailing or screwing sheets of various types to the frame, but when taller structures are designed and built, serious problems may arise.
Since wind speed and thus wind pressure increases with height above the ground and the shear forces transmitted by the walls increase accordingly, storey by storey, considerable efforts can be needed to handle the strong horizontal shear forces that are exerted on the bottom floor in particular. The strong uplift forces that can develop on the wind side of a structure are yet another matter that can be critical. Accordingly, a structure needs to be anchored to the substrate or to the ground by connections that are properly designed. Since the calculated uplift forces depend very much upon the models employed, the choice of models and simplifications in the analysis that are undertaken also need to be considered carefully.
The present licentiate thesis addresses questions of how wind loads acting on multi-storey timber buildings can be best dealt with and calculated for in the structural design of such buildings. The conventional use of sheathing either nailed or screwed to a timber framework is considered, together with other methods of stabilizing timber structures. Alternative ways of using solid timber elements for stabilization are also of special interest.
The finite element method was employed in simulating the structural behaviour of stabilizing units. A study was carried out of walls in which sheathing was nailed onto a timber frame. Different structural levels were involved, extending from modelling the performance of a single fastener and of the connection of the sheathing to frame, to the use of models of this sort for studying the overall structural behaviour of wall elements that possess a stabilizing function. The results of models used for simulating different load cases for walls agreed reasonably well with experimental test results. The structural properties of the fasteners binding the sheathing to the frame, as well as of the connections between the members of the frame were shown to have a strong effect on the simulated behaviour of shear wall units.
Regarding solid wall panels, it was concluded that walls with a high level of both stiffness and strength can be produced by use of such panels, and also that the connections between the solid wall panels can be designed in such a way that the shear forces involved are effectively transmitted from one panel to the next.
Schroder, Ulf P. "Development of a weather radar signal simulator to examine sampling rates and scanning schemes." Thesis, Monterey, Calif. : Springfield, Va. : Naval Postgraduate School ; Available from National Technical Information Service, 2005. http://library.nps.navy.mil/uhtbin/hyperion/05Sep%5FSchroder.pdf.
Full textVessby, Johan. "Analysis of shear wallsfor multi-storey timber buildings." Doctoral thesis, Linnéuniversitetet, Institutionen för teknik, TEK, 2011. http://urn.kb.se/resolve?urn=urn:nbn:se:lnu:diva-11489.
Full textPan, Da-Gang Lin Yeong-Jer. "Structure and evolution of a midwestern storm during VORTEX-95 as determined from airborne doppler data /." SLU electronic book. Click to access, 1999. http://proquest.umi.com/pqdweb?did=731937091&sid=1&Fmt=2&clientId=26447&RQT=309&VName=PQD.
Full textWu, Peng, Xiquan Dong, Baike Xi, Yangang Liu, Mandana Thieman, and Patrick Minnis. "Effects of environment forcing on marine boundary layer cloud-drizzle processes." AMER GEOPHYSICAL UNION, 2017. http://hdl.handle.net/10150/624343.
Full textEppanapelli, Lavan Kumar. "Investigation of wind potential variation at three measurement sites based on atmospheric stability and power production." Thesis, KTH, Kraft- och värmeteknologi, 2013. http://urn.kb.se/resolve?urn=urn:nbn:se:kth:diva-136935.
Full textPereira, Maurício Vieira da Rocha. "Impacto da altura de aerogeradores sobre a velocidade do vento, energia, efeito de esteira e intensidade de turbulência : estudos de caso em três projetos eólicos localizados no Brasil." reponame:Biblioteca Digital de Teses e Dissertações da UFRGS, 2016. http://hdl.handle.net/10183/134892.
Full textThe wind energy sector has been under consolidation in Brazil since the early 2000s. Opportunities for researches and developments are present at all stages of the process. This paper presents a link among wind speed, energy, wake effect and turbulence intensity parameters and the height of existing wind turbine models in Brazil, considering three distinct regions as Triunfo/PE, São João do Cariri/PB and São Martinho da Serra/RS. This paper also aims to support developers and investors in the decision making process in the wind turbines height that should be considered in its wind farms. To this end, the references of similar studies as well as the theoretical basis for the study, including the main equations and models, are presented. The calculation methodology is theoretical and it has been applied to the computational tools WAsP (wind modeling) and WindFarmer (evaluate the energy production), considering specific adaptations for each project. Statistical procedures are performed in order to ensure that the analyses contain the lowest possible level of uncertainty in the characterization of the wind resources in each region. The results are presented comparatively among the seven tested turbine models and also among the three studied areas. The turbine models behavior is considerably different for all options. The wind turbine models A and D are those with the highest percentage energy increase with increasing the turbine height. Their average values are 0.42% and 0.44% per meter height. The models C and D present the most considerable improvements in terms of turbulence intensity and wake effect reductions with increasing the turbine height. The different locations also present distinguished wind resources among them. Triunfo wind farm is the one with the highest energy generation, 24.2% higher than in São Martinho da Serra and 45.0% higher than in São João do Cariri. It is also noted that if the long term mean wind speed was doubled in the project locations, the energy would have an increase of 88% in Triunfo, 170% in São Martinho da Serra and 220% in São João do Cariri.
Russell, Frances Marion. "Semi-permanent zones of radar radial shear within the planetary boundary layer : observations and effects on high intensity precipitation in the wider Auckland region, New Zealand : a thesis submitted to the Victoria University of Wellington in partial fulfilment of the requirements for the degree of Master of Science in Geophysics /." ResearchArchive@Victoria e-Thesis, 2009. http://hdl.handle.net/10063/1215.
Full textMilbank, Juliette, and milbank@turbulenflow com au. "Investigation of fluid-dynamic cavity oscillations and the effects of flow angle in an automotive context using an open-jet wind tunnel." RMIT University. Aerospace, Mechanical & Manufacturing Engineering, 2005. http://adt.lib.rmit.edu.au/adt/public/adt-VIT20090723.121800.
Full textMauk, Rachel Grant. "Tropical Cyclone Formation in Environments with Cool SST and High Wind Shear over the Northeastern Atlantic Ocean (1975-2005)." The Ohio State University, 2010. http://rave.ohiolink.edu/etdc/view?acc_num=osu1275445016.
Full textHe, Yuxin. "Crop residue management and its impacts on soil properties." Diss., Kansas State University, 2015. http://hdl.handle.net/2097/19043.
Full textAgronomy
DeAnn R. Presley
Crop residue removal for livestock feeding and biofuel production at large scales must be evaluated to assess impacts on soil productivity and properties. Among all the potential negative impacts, wind erosion is a major concern in the central Great Plains. We conducted an on-farm study from 2011 to 2013 by removing crop residue at five levels (0, 25, 50, 75, and 100%) to determine the effects of crop residue removal on soil wind erosion parameters such as dry aggregate size distribution including soil wind erodible fraction (EF <0.84 mm aggregates), geometric mean diameter (GMD) and geometric standard deviation (GSD), dry aggregate stability, and soil surface roughness. The sub-model of Wind Erosion Prediction System (WEPS) developed by the USDA-ARS, Single-event Wind Erosion Evaluation Program (SWEEP) is a stand-alone companion software package that can be applied to simulate soil loss and dust emission from a single windstorm event. We applied measured data (i.e. EF, GMD, GSD, and roughness) to SWEEP for predicting wind velocity that can initiate wind erosion and soil loss under each crop residue removal condition with wind velocity at 13 m sˉ¹. The threshold wind velocity to initiate wind erosion generally decreased with increase in crop residue removal levels, particularly for residue removal >75%. The total amount of soil loss in 3 hours ranged from about 0.2 to 2.5 kg mˉ² and depends on soil condition and crop residue cover. On the other hand, high-yielding crops can produce abundant crop residue, which then raises the question that if a farmer wants to reduce residue, what could they do without removing it? The application of fertilizer on crop residue to stimulate microbial activity and subsequent decomposition of the residue is often debated. We conducted wheat straw decomposition field experiments under different fertilizer rates and combinations at three locations in western Kansas following wheat harvest in 2011 and 2012. A double shear box apparatus instrumented with a load cell measured the shear stress required to cut wheat straw and photomicrography was used to measure the cross-sectional area of wheat straw after shearing. Total C and N were also analyzed. The fertilizer rate and timing of application during summer 2012 and Fall 2013 at the Hays site had impacts on wheat straw shear stress at break point. Across site years, earlier (fall) fertilizer application generally resulted in lower remaining aboveground biomass as compared to a spring application. Multivariate and linear regressions suggested that N and C:N ratio partially explain the results observed with respect to treatment effects on winter wheat residue decomposition.
Kunwar, Sushil. "Comprehensive Evaluation of Composite Core Walls for Low-Seismic Force and Wind Load Applications." University of Cincinnati / OhioLINK, 2020. http://rave.ohiolink.edu/etdc/view?acc_num=ucin1613750905724949.
Full textOLIVEIRA, Gabrielle Bezerra. "Análise de padrões temporais da dinâmica do vento associadas ao ambiente de formação das linhas de instabilidade amazônica." Universidade Federal de Campina Grande, 2017. http://dspace.sti.ufcg.edu.br:8080/jspui/handle/riufcg/1757.
Full textMade available in DSpace on 2018-09-19T20:06:03Z (GMT). No. of bitstreams: 1 GABRIELLE BEZERRA OLIVEIRA – DISSERTAÇÃO (PPGMet) 2017.pdf: 2219344 bytes, checksum: b1c40baaf11a5f1e293aa66cdc9139b9 (MD5) Previous issue date: 2017-02-24
CNPq
O enfoque deste trabalho é contribuir para a compreensão dos mecanismos responsáveis pela formação das Linhas de Instabilidade Tropicais da Amazônia. Analisou-se 3 anos de dados de reanálises investigando as características dinâmicas dos perfis verticais do vento zonal e meridional a partir da média do período e das médias trimestrais dos dias com e sem a formação de LI. Mostrou-se que o JBN é uma característica intrínseca do ambiente amazônico, entretanto nos dias com a formação de LI esse jato é mais intenso e profundo. Os trimestres março-abril-maio e junho-julho-agosto não apresentam um JBN bem definido, principalmente em relação à sua profundidade. Destaca-se ainda que o cisalhamento vertical do vento é mais intenso nos dias com a formação de LI. Já o maior cisalhamento direcional da componente meridional do vento é visto nos perfis dos dias sem LI. Para auxiliar o entendimento da variabilidade temporal dos perfis verticais do vento foi aplicada a técnica de Análise Fatorial em Componentes Principais com o intuito de investigar a existência de padrões atmosféricos associados à ocorrência de LI. As três primeiras componentes principais da componente zonal do vento explicaram aproximadamente 89% da variância total dos dados, enquanto que os 93% da variância total da componente meridional foi explicado pelas cinco primeiras componentes principais. A análise dos padrões temporais associados a cada fator sugere que os trimestres DJF e SON são influenciados pela variação sazonal da ZCIT e os trimestres MAM e JJA pela ASAS e DOL.
The aim of this work is to contribute to the understanding the mechanisms responsible for the formation of Amazon Tropical Squall Lines (ASL). 3 years of reanalysis data were analyzed investigating the dynamic characteristics of vertical profiles of the zonal and meridional wind from the a average of period and quarterly of the days with and without the ASL formation. It has been shown that low level jet (LLJ) is an intrinsic characteristic of Amazonian environment, however in the days with the formation of SL this LLJ is more intense and deep. The quarters March-April-May and June-July-August do not present a well defined LLJ, mainly in relation their depth. It was also pointed out that vertical shear of wind is more intense on days with ASL formation. However, the greatest directional shear of meridional component wind is seen in the profiles of days without ASL. To aid the understanding of temporal variability of vertical profiles wind were applied the method Principal Components Fatorial Analysis in order to investigate the existence of atmospheric patterns associated with the occurrence of ASL. The first three Principal Components of the zonal wind component explained approximately 89% of the total variance of the data, while the 89% of the total variance of the meridional wind component were explained by the first five principal components. The analysis of the time patterns associated with each factor suggests that the DJF and SON quarters are influenced by the seasonal variation of the ITCZ and the quarters MAM and JJA by South Atlantic Subtropical High (SASH) and Easterly Wave Disturbances (EWD).
Woldemikael, Biruk Worku. "Effects of cracking of coupling beams onhigh rise towers subjected to wind load." Thesis, KTH, Betongbyggnad, 2020. http://urn.kb.se/resolve?urn=urn:nbn:se:kth:diva-290589.
Full textI höghus används hisschakt av armerad betong tillsammans med kopplingsbalkar i stor utsträckning som främsta konstruktionselement för att motstå horisontella laster. Tornets horisontella bärförmåga är beroende av analytiska studier och studier med finita element metoden styvheten hos de bärande väggarna, och kopplingsbalkarna som förbinder dem. För att studera minskningen av styvheten i höghustorn på grund av sprickbildning i kopplingsbalkar, variationen i armeringsmängden, betongkvaliteten och effekten av ledflexibilitet vid balk-vägg-knutpunkten, presenterar detta examensarbete kopplingsbalkarnas effektiva styvhet och höghusets globala stabilitet. En omfattande parametrisk studie på 240 olika kombinationer av armerade kopplingsbalkar och 32 modeller av ett höghus har genomförts för att härleda den effektiva styvheten i de armerade kopplingsbalkarna från last-deformationskurvan. Som ett resultat beräknas styvheten och den ekvivalenta höjden av kopplingsbalkarna och plottas som funktion av betongkvaliteten och armeringsmängden. Dessutom modelleras höghuset för både spruckna & armerade kopplingsbalkar samt oarmerade & ospruckna kopplingsbalkar för att erhålla utböjningen av höghusets topp. Resultatet plottas som funktion av betongkvaliteten och armeringsmängden. De erhållna resultaten visar att styvhetsförhållandet och förhållandet mellan ekvivalent höjd till normal höjd ökar med mer längsgående armering och tvärsnittsförhållandet men minskar med en ökning av betongkvaliteten för både den analytiska och finita elementmetoden. Utböjningen av höghusets topp påverkas inte nämnbart av en ökning av armeringsmängden i de slanka kopplingsbalkarna och vice versa för både den analytiska och finita elementmetoden. Oberoende av slankheten av kopplingsbalkarna ökar styvheten betydligt med en ökning av betongkvaliteten. Dessa resultat visar en bra bild på hur man väljer ekvivalent höjd i modellen utan armering. Därmed kommer det framtagna diagrammet vara en mer praktisk metod för att i ett tidigt skede konstruera en hel byggnad. Tjocka kopplingsbalkar måste armeras för att nå tvärsnittets styvhet medan smala tvärsnitt kommer att ha en högre styvhet med armering. Detta skulle hjälpa konstruktören att hitta en mer rationell modell utan armering. Med hjälp av Hans Peterssons analytiska metod, angående ledflexibiliteten vid balk-väggknutpunkten, bör styvheten minskas för att utnyttja den fulla kapaciteten hos en betongkopplingsbalk. För globala modeller, oberoende av de slanka kopplingsbalkarna, ökar styvheten betydligt med en ökning av betongkvaliteten.
Fytterer, Tilo, Christina Arras, and Christoph Jacobi. "Terdiurnal signatures in midlatitude sporadic E layers occurrence rates." Universität Leipzig, 2013. https://ul.qucosa.de/id/qucosa%3A16409.
Full textRadiookultationsmessungen auf der Basis von GPS-Messungen der FORMOsa SATellite mission-3/Constellation Observing System for Meteorology, Ionosphere and Climate-Satelliten wurden verwendet, um die Signatur der 8-stündigen Gezeiten in den Auftrittsraten von sporadischen E (Es)-Schichten zu analysieren. Nach der allgemein anerkannten Windscherungstheorie treten Es-Schichten im Bereich negativer vertikaler Windscherung auf, welche in der unteren Thermosphäre hauptsächlich durch solare Gezeiten hervorgerufen werden. Speziell werden hier 4-jährige Mittelwerte saisonal gemittelter Auftrittsraten untersucht um die 8-stündige Signatur zu finden. Ein Vergleich mit Radarmessungen des Windes über Collm zeigt, dass die saisonale und tägliche Variabilität der 8-stündigen Komponente der Es-Raten sehr gut mit derjenigen der gemessenen Windscherung übereinstimmt.
Memon, Muhammad Omar. "Wingtip Vortices and Free Shear Layer Interaction in the Vicinity of Maximum Lift to Drag Ratio Lift Condition." University of Dayton / OhioLINK, 2017. http://rave.ohiolink.edu/etdc/view?acc_num=dayton1492701624726378.
Full textSementi, Joshua Paul. "A study of jet exhaust-wing interaction /." Thesis, Connect to this title online; UW restricted, 2005. http://hdl.handle.net/1773/10002.
Full textBennaceur, Iannis. "Etude numérique de la diffusion d'une onde acoustique par une couche de cisaillement turbulente à l'aide d'une simulation aux grandes échelles." Thesis, Aix-Marseille, 2017. http://www.theses.fr/2017AIXM0187/document.
Full textDuring open jet wind tunnel measurements, the acoustic waves emitted by a device or an acoustic source located inside the flow propagate inside the turbulent shear layer that develops at the periphery of the jet before being received by microphones located outside the flow. The acoustic wave interacts with the turbulent velocity field leading to a change of directivity, a phase and amplitude modulation as well as a spectral re-distribution of the acoustic energy over a band of frequencies. This phenomenon is known as acoustic scattering. This work has consisted in the study of the scattering of an acoustic wave by a turbulent shear layer using large-eddy simulation. The first step of the study has consisted in the large-eddy simulation of a turbulent shear layer in its self-similar state. In a second second step, the direct computation of the interaction between the acoustic wave and the turbulent flow has been performed in order to study the characteristics of the resulting scattered pressure field. It has been shown that the numerical simulation is able to accurately predict the frequencies on which the main part of the scattered energy is redistributed, as well as the shape of the scattered pressure spectrum. Finally, the turbulent velocity field which is correlated with the envelope of the scattered pressure field is reconstructed using the linear stochastic estimation method. This method has enabled the visualization of the large turbulent structures that mainly take part in the acoustic scattering mechanism
Kuo, Matthew Yih-Han. "Deep ocean clay crusts : behaviour and biological origin." Thesis, University of Cambridge, 2011. https://www.repository.cam.ac.uk/handle/1810/240506.
Full textChemlali, Alexander, and Rickard Norberg. "Shear cracks in reinforced concrete in serviceability limit state." Thesis, KTH, Betongbyggnad, 2015. http://urn.kb.se/resolve?urn=urn:nbn:se:kth:diva-169591.
Full textNovozámský, Adam. "Střih větru jako nebezpečný jev v letectví." Master's thesis, Vysoké učení technické v Brně. Fakulta strojního inženýrství, 2014. http://www.nusl.cz/ntk/nusl-231313.
Full textFabiánová, Lucie. "Přepočet a variantní návrh nosných konstrukcí objektů administrativního centra." Master's thesis, Vysoké učení technické v Brně. Fakulta stavební, 2014. http://www.nusl.cz/ntk/nusl-226643.
Full textTomala, Daniel. "Návrh letounu podle předpisu FAR 103." Master's thesis, Vysoké učení technické v Brně. Fakulta strojního inženýrství, 2008. http://www.nusl.cz/ntk/nusl-227917.
Full textHong, Wei_Chuan, and 洪偉川. "Flight Path and Wind Field Reconstruction in Wind Shear Flow." Thesis, 2006. http://ndltd.ncl.edu.tw/handle/35240381464274118558.
Full text國立成功大學
航空太空工程學系碩博士班
94
The objective of this research is to reconstruct the wind field and the flight path for aircraft in wind shear flow encounter. Wind field experienced by the flying aircraft is generated by a microburst mathematical model and the aircraft position. Two-step method is introduced, in which the Genetic Algorithm is used in conjunction with the Extended Kalman Filter to identify the system error parameters and to estimate the state variables. The first-step identification uses flight data obtained in smooth air, whereas the second-step assumes the error factors associated with the air data are invariant when analyzing the flight data in turbulence. The objective function is derived using the Maximum Likelihood principle, and the system error parameters are obtained by optimizing this objective function. The use of Genetic Algorithm aims to solve the numerical stiffness and the initial guess problems associated with the gradient search methods. In this research a Boeing 747-100 airplane encountered with 3 different wind shear fields during approaching are simulated. The results of constant bias and scale factors estimated by the present Genetic Algorithm were satisfactory. The state variables and flight paths and the wind shear fields are successfully reconstructed, indicating the appropriateness of applying the present method to wind shear flight data analysis.
Wu, Jia-Hong, and 吳嘉鴻. "Resiliency of Concentric Eyewall Vortex against Vertical Wind Shear." Thesis, 2007. http://ndltd.ncl.edu.tw/handle/50772562761376763354.
Full text國立臺灣大學
大氣科學研究所
95
This study, with the aid of two-layer shallow water model, explore the vortex resiliency of concentric eyewall against vertical wind shear. In particular, we focus on (1)moat width ; (2)outer eyewall width ; and (3)intensity parameters on the vortex. The resiliency ability against the vertical wind shear is defined as a ratio in compare to the control run(radius=100km; intensity = Zc=1.8e-3s-1 ) which shows “tilt-align” in vertical structure when vertical wind shear reach the maximum(Uc=11m/s). The result shows both intensity and structure of concentric vortex are important factors for vortex resiliency against vertical wind shear. The numerical simulations indicate that: (1)vertical wind shear destroys the concentric eyewall structure in most of the cases simulated, (2)vortex resiliency of concentric eyewall vortex is weaker than the similar non-concentric eyewall counterpart, (3)vertical resiliency decreases with the increase of the baroclinicity of the concentric vortex, (4)vortex resiliency against vertical wind shear increases with the intensity of the core vortex, (5)other parameters being equal, the vortex resiliency increases with the increase of outer eyewall circulation, (6)other parameters being equal, the vortex resiliency decreases with the increase of outer eyewall width, and (7)other parameters being equal, the vortex resiliency decreases with the increase of moat width.
Yu, Cheng-Da, and 余政達. "Study on Particle Continuous Saltation Mechanism under Wind Shear." Thesis, 2003. http://ndltd.ncl.edu.tw/handle/53284431880911917446.
Full text國立交通大學
土木工程系
91
Under wind shear, the particle motion of soil on the surface including the particle suspension, saltation and surface creeping, in which saltation is the key factor, results in the landform erosion. The powerful dropping thrust of particles is the main factor for the cause of the aeolian sand motion and the landform erosion. The wind tunnel experiment is conducted to visualize and analyze the particle saltant motion. To measure the motion orbit, motion speed, and the collision angle of the particle continuous saltant process under different wind velocity the high speed photographic technique is applied. Based on the observed data, the physical phenomenon and the statistical characteristics for the particle motion are explored. In the sequence 2-D mathematical model of particle continuous saltation is established. The particle continuous saltation model established in this study includes two parts: the single-step saltant model and the collision model. The simulation results reveal that the trajectory and saltant characteristics can be interpreted under the given conditions of the ejection velocity and the size of particle. Moreover, from the analysis and find that the inter-particle collision behavior not only follows the Newton’s laws but also is controlled by random processes. Finally, the confidence level for the average saltant length and height is compared with the experimental data, showing that the proposed model is able to simulate the particle continuous saltation reasonably.
Wong, Wai-Mun, and 黃偉民. "Numerical Analysis of Wind Shear Effect in Spin Coating." Thesis, 1997. http://ndltd.ncl.edu.tw/handle/39668584916337359438.
Full text國立中央大學
機械工程學系
85
The process of spin coating has been extensively studied. However,to our knowledge, all studies related has either neglected or just appliedCochran's solution for the shear stress at the interface between the over-lying gas and the film surface. It is suitable when applied to a spin coaterunder free space and an infinite disk. However, for a real model where thereis an enclosure or a hub and a finite radius is taken into account, shearstress may differ from that of Cochran's solution. This study intends to in-investigate the effect of the enclosure, as well as, a hub on the shear stress . Results show the distribution of shear stress along the disk may not alike that of Cochran's solution, and may have to be re-evaluated.
Gallina, Gregory M. "Environmental vertical wind shear and tropical cyclone intensity change utilizing enhanced satellite derived wind information." 2002. http://catalog.hathitrust.org/api/volumes/oclc/50084050.html.
Full textTypescript. eContent provider-neutral record in process. Description based on print version record. Includes bibliographical references (leaves 78-79).
Meanor, Denis H. "Vertical wind shear as a predictor of tropical cyclone motion." Thesis, 1987. http://hdl.handle.net/10945/22846.
Full textWang, Shiang-Yi, and 王翔儀. "Effects of the Vertical Wind Shear on Tropical Cyclone Intensity." Thesis, 2006. http://ndltd.ncl.edu.tw/handle/53601267731961381204.
Full textTalgo, Kevin D. "Tropical Atlantic vertical wind shear variability in a future climate." 2009. http://www.lib.ncsu.edu/theses/available/etd-10302009-105719/unrestricted/etd.pdf.
Full textChieh-JuJuan and 阮婕如. "System Analysis and Alert for Real Time Airport Wind Shear Detection." Thesis, 2016. http://ndltd.ncl.edu.tw/handle/c4756w.
Full text國立成功大學
航空太空工程學系碩士在職專班
104
Low level wind shear has been recognized as a serious hazard to aviation safety, especially when it occurs during aircraft take-offs and landings. In these flight phases, the aircraft flight altitude and airspeed are approaching to their critical margin. The sudden variation of wind speed and wind direction may affect aircraft performance greatly. Pilots’ misjudge or retardation may bring aircraft into catastrophic states. Low level wind shear and small-scale microburst detection over the runway or within 3 nautical miles on both direction extensions may find some effective early warning signals to pilots. A simple barometric data detection system is proposed and established in Sung-Shan Airport to collect atmospheric pressure changes in real time and convert the statistical micro-changes to identify the wind burst. This thesis uses the barometric data of an established system to analyze the ground atmospheric pressure changes along runway. Based on the collected weather data, the fluctuation and standard deviation of the barometric pressure changes are calculated and detected. When the time span and frequency of the weather parameters exceed one statistics sigma, the correlated wind shear alert will be alarmed from the ground station. The analytical results demonstrate the effectiveness of the proposed detection mechanism to enforce aviation safety.
Krallis, George A. "Modeling the mean shear component of wind-induced mixing in lakes /." Diss., 2000. http://gateway.proquest.com/openurl?url_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:dissertation&res_dat=xri:pqdiss&rft_dat=xri:pqdiss:9982866.
Full textChen, Kuan-Ting, and 陳冠廷. "Climatology of ionospheric Sporadic E Layer : Examination of Wind Shear Theory." Thesis, 2013. http://ndltd.ncl.edu.tw/handle/10140004731560594998.
Full text國立中央大學
太空科學研究所
101
On the basis of GPS radio occultation (RO) technique, we develop a method to extract ionospheric sporadic E (Es) layer from COSMIC-measured ionospheric data (e.g., GPS signal signal-to-noise ratio, L1 and L2 excess phases and RO-retrieved electron density) to investigate the climatology of the Sporadic E layer. The results show that there is salient summer-winter asymmetry in the occurrence rate of the Es layer, namely, higher in summer hemisphere and lower in winter hemisphere. In addition, there is a strong tendency for the Es layer to descend with local time that is in harmony with the diurnal or semi-diurnal tidal motion, depending on season and latitude region. In order to realize the physical process responsible for the climatology of the COSMIC-measured Es layer, we simulate the temporal and global distribution of the occurrence of the Es layer in accordance with wind shear Theory. We calculate vertical ion drift velocity based on empirical models of the ionosphere, including HWM07, MSIS00, IGRF. The ferric ion (Fe+) density calculated from Whole Atmosphere Community Climate Model(WACCM) is used to obtain ferric ion vertical flux. The simulation results show that the seasonal asymmetry of the Sporadic E layer occurrence rate between the summer and winter hemispheres is very likely caused by the neutral wind shear in the Es region.