Дисертації з теми "Boundary layer (Meteorology) Australia"
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MacKinnon, Andrew David. "VHF Boundary Layer Radar and RASS." Title page, abstract and table of contents, 2001. http://hdl.handle.net/2440/37807.
Повний текст джерелаThesis (Ph.D.)--Department of Physics and Mathematical Physics, 2001.
Anderson, Philip Stuart. "Aspects of the Antarctic boundary layer." Thesis, Lancaster University, 1993. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.239832.
Повний текст джерелаStevens, David Eric. "An adaptive multilevel method for boundary layer meteorology /." Thesis, Connect to this title online; UW restricted, 1994. http://hdl.handle.net/1773/6776.
Повний текст джерелаSchafer, Robert. "Tropical island boundary layer structure and development /." [Sydney : University of Technology, Sydney], 1998. http://grison.colorado.edu/Robert/paper/phd.pdf.
Повний текст джерелаLee-Thorp, Andrew Michael. "The atmospheric boundary layer above the Agulhas current." Master's thesis, University of Cape Town, 1996. http://hdl.handle.net/11427/19455.
Повний текст джерелаPotvin, Guy. "The application of RASS in urban boundary layer meteorology." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1998. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape11/PQDD_0019/NQ44556.pdf.
Повний текст джерелаWhisenhant, Michelle K. "Turbulence parameterizations for convective boundary layers in high-resolution mesoscale models." Diss., Monterey, Calif. : Springfield, Va. : Naval Postgraduate School ; Available from National Technical Information Service, 2003. http://library.nps.navy.mil/uhtbin/hyperion-image/03Dec%5FWhisenhant%5FPhD.pdf.
Повний текст джерелаMabey, Deborah L. "Variability of refractivity in the suface layer." Monterey, Calif. : Springfield, Va. : Naval Postgraduate School ; Available from National Technical Information Service, 2002. http://library.nps.navy.mil/uhtbin/hyperion-image/02Jun%5FMabey.pdf.
Повний текст джерелаLloyd, Matthew R. "Doppler LiDAR Measurements of Boundary Layer Heights over San Jose, California." Thesis, San Jose State University, 2018. http://pqdtopen.proquest.com/#viewpdf?dispub=10744231.
Повний текст джерелаThere is a need for understanding boundary layer depth and climatology over the urban area of San Jose, California. In this paper, Doppler LiDAR data are observed from San Jose. The adopted methods of vertical velocity variance and skewness are used to determine the estimated height of the convective boundary layer and to analyze sources of turbulence. The use of these methods helped identify a few types of the boundary layer that are common in San Jose. Also examined in this paper is a brief climatology of the mean maximum convective boundary layer height in San Jose over the period of 2013–2015. Vertical velocity variance and skewness is applied to identify seasonal trends in the convective boundary layer height. The influence that the marine layer has on the boundary layer over San Jose is analyzed and a conduit for future work is set forth.
Van, der Kamp Derek. "Ceilometer observations of Vancouver's urban boundary layer : validation and mixed-layer height estimation." Thesis, University of British Columbia, 2008. http://hdl.handle.net/2429/1599.
Повний текст джерелаSullivan, Zachary S. "Karst Landscape Influence on the Planetary Boundary Layer Atmosphere." TopSCHOLAR®, 2016. http://digitalcommons.wku.edu/theses/1638.
Повний текст джерелаJohansson, Cecilia. "Influence of External Factors on the Turbulence Structure in the Atmospheric Boundary Layer." Doctoral thesis, Uppsala University, Department of Earth Sciences, 2003. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-3221.
Повний текст джерелаThe theory used in today’s weather- and climate models to describe processes near the earth’s surface, i.e. transport of heat, moisture and momentum between the ground and the atmosphere, is based on the idea that only local factors are important, such as temperature and wind speed near the ground. However, from measurements made at two sites, one agricultural and one marine, it has been found that large eddies, which are related to the convective boundary layer height, influence the turbulence structure near the ground during unstable conditions more than previously realized. Especially the momentum transport is affected. The large eddies have similar size over land and over the sea, typically 1000 m. The important difference being that over land diurnal variation plays a fundamental role; over the sea such variations are typically absent.
From the marine site it has also been found that the turbulence structure of the temperature field over the Baltic Sea is very different from over land. Instead of having a height dependence as expected from theory, the temperature structure seems to be constant with height within the surface layer.
Typically, the heat flux over the sea is smaller than over land during convective conditions. This gives rise to a turbulence transport regime which is fundamentally different from that observed during daytime convective conditions over land.
Harris, Brad G. "Analysis of lateral boundary effects on inner domain of COAMPS." Thesis, Monterey, Calif. : Springfield, Va. : Naval Postgraduate School ; Available from National Technical Information Service, 2004. http://library.nps.navy.mil/uhtbin/hyperion/04Sep%5FHarris.pdf.
Повний текст джерелаThesis advisor(s): Douglas K. Miller, Beny Neta. Includes bibliographical references (p. 83). Also available online.
Tourigny, Pierre. "Inclusion de la condensation dans un modèle de couche limite." Thesis, McGill University, 1986. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=66104.
Повний текст джерелаGobel, Teresa M. "Aircraft observations of the atmospheric boundary layer in the vicinity of the marginal ice zone under conditions of flow parallel to the ice edge." Thesis, Monterey, California : Naval Postgraduate School, 1990. http://handle.dtic.mil/100.2/ADA241072.
Повний текст джерелаThesis Advisor(s): Shaw, W.J. Second Reader: Nuss, W.A. "September 1990." Description based on title screen as viewed on December 29, 2009. DTIC Identifier(s): Marine atmospheres, marginal ice zones, geostropic wind, atmospheric boundary layer, stratus clouds, cumulus clouds, stratocumulus clouds, wind velocity, temperature inversion, air ice interactions. Author(s) subject terms: Marginal ice zone. Includes bibliographical references (p. 45-46). Also available in print.
Cross, Patrick S. "The California coastal jet : synoptic controls and topographically induced mesoscale structure /." Monterey, Calif. : Springfield, Va. : Naval Postgraduate School ; Available from National Technical Information Service, 2003. http://library.nps.navy.mil/uhtbin/hyperion-image/03Mar%5FCross.phd.pdf.
Повний текст джерелаDerley, Dennis T. "Remote sensing of the refractive environment above the marine stratocumulus-topped boundary layer." Thesis, Monterey, Calif. : Springfield, Va. : Naval Postgraduate School ; Available from National Technical Information Service, 2006. http://library.nps.navy.mil/uhtbin/hyperion/06Sep%5FDerley.pdf.
Повний текст джерелаThesis Advisor(s): Philip A. Durkee. "September 2006." Includes bibliographical references (p. 65). Also available in print.
Svensson, Jacob. "Boundary Layer Parametrization in Numerical Weather Prediction Models." Licentiate thesis, Stockholms universitet, Meteorologiska institutionen (MISU), 2015. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-117134.
Повний текст джерелаDet har visat sig att det är en stor utmaning för numeriska väderprognosmodeller (NWP-modeller) att simulera stabilt skiktade atmosfäriska gränsskikt och gränsskiktets dygnscykel på ett korrekt sätt. Syftet med denna studien är att utvärdera, beskriva och ge förslag på förbättringar av beskrivningen av gränsskiktet i NWP-modeller. Studien innehåller två artiklar. Den första fokuserar på beskrivningen av markytan och interaktionen mellan marken och gränsskiktet i den regionala NWP-modellen COAMPS R . Det visade sig att beskrivningen av markytan har en signifikant inverkan på gränsskiktets struktur. Det framkom också att strålningsberäkningarna endast görs en gång i timmen vilket bland annat orsakar en bias i inkommande solinstrålning vid markytan. Den andra artikeln fokuserar på beskrivningen av den turbulenta transporten i stabila skiktade gränsskikt. En implemenering av en diffusionsparametrisering som bygger på turbulent kinetisk energy (TKE) testas i en endimensionell version av NWP-modellen Integrated Forecast System (IFS), utvecklat vid European Center for Medium Range Weather Forecasts (ECMWF). Den TKE-baserade diffussionsparametriseringen är likvärdigt med den nuvaran de operationella parametriseringen i neutrala och konvektiva gränsskikt, menär mindre diffusivt i stabila gränsskikt. Diffusionens intensitet är beroende påden turbulenta längdskalan. Vidare kan turbulensen i TKE-formuleringen hamna i ett oscillerande läge om turbulensen är svag samtidigt som temperatur- och vindgradienten är kraftig. Denna oscillation kan förhindras om längdskalans minsta tillåtna värde begränsas.
Elge, Murat. "Langmuir circulations in a coastal environment during CBLAST." Thesis, Monterey, Calif. : Springfield, Va. : Naval Postgraduate School ; Available from National Technical Information Service, 2004. http://library.nps.navy.mil/uhtbin/hyperion/04Sept%5FElge.pdf.
Повний текст джерелаThesis advisor(s): Timothy P. Stanton. Includes bibliographical references (p. 95-99). Also available online.
Comstock, Kimberly K. "Mesoscale variability and drizzle in southeast Pacific stratocumulus /." Thesis, Connect to this title online; UW restricted, 2006. http://hdl.handle.net/1773/10013.
Повний текст джерелаBaum, Bryan Alan. "The extension of rapid distortion theory to stratified shear flows." Diss., Georgia Institute of Technology, 1989. http://hdl.handle.net/1853/25971.
Повний текст джерелаEleuterio, Daniel P. "Coastal stratocumulus topped boundary layers and the role of cloud-top entrainment." Monterey, Calif. : Springfield, Va. : Naval Postgraduate School ; Available from National Technical Information Service, 2004. http://library.nps.navy.mil/uhtbin/hyperion/04Jun%5FEleuterio%5PhD.pdf.
Повний текст джерелаAndrae, Ulf. "Turbulence structures in a non-stationary marine atmospheric boundary layer." Thesis, Uppsala universitet, Meteorologiska institutionen, 1996. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-392332.
Повний текст джерелаCarlsson, Magnus. "The stable boundary layer over the ice covered Bothnian Bay." Thesis, Uppsala universitet, Institutionen för geovetenskaper, 2000. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-392449.
Повний текст джерелаArduini, Gabriele. "Wintertime stable boundary-layer processes in Alpine valleys." Thesis, University of Hertfordshire, 2017. http://hdl.handle.net/2299/19706.
Повний текст джерелаMengesha, Yoseph Gebrekidan. "Atmospheric boundary-layer flow over topography data analysis and representations of topography /." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1999. http://www.collectionscanada.ca/obj/s4/f2/dsk2/ftp01/MQ39212.pdf.
Повний текст джерелаLiu, Chun-ho. "Numerical modelling of atmospheric boundary layer with application to air pollutant dispersion /." Hong Kong : University of Hong Kong, 1998. http://sunzi.lib.hku.hk/hkuto/record.jsp?B20158695.
Повний текст джерелаNewton, D. Adam. "COAMPS modeled surface layer refractivity in the Roughness and Evaporation Duct experiment 2001." Thesis, Monterey, Calif. : Springfield, Va. : Naval Postgraduate School ; Available from National Technical Information Service, 2003. http://library.nps.navy.mil/uhtbin/hyperion-image/03Jun%5FNewton.pdf.
Повний текст джерелаThesis advisor(s): Kenneth Davidson, Douglas Miller. Includes bibliographical references (p. 59-60). Also available online.
Ahn, Seungki. "Some unsteady features of turbulent boundary layers." Thesis, Virginia Polytechnic Institute and State University, 1986. http://hdl.handle.net/10919/53090.
Повний текст джерелаMaster of Science
Tastula, Esa-Matti. "Insights into the Challenges of Modeling the Atmospheric Boundary Layer." Scholar Commons, 2015. http://scholarcommons.usf.edu/etd/5782.
Повний текст джерелаMoore, Matthew J. "Evolution of boundary layer height in response to surface and mesoscale forcing." Thesis, Monterey, Calif. : Springfield, Va. : Naval Postgraduate School ; Available from National Technical Information Service, 2005. http://library.nps.navy.mil/uhtbin/hyperion/05Mar%5FMoore.pdf.
Повний текст джерелаHedley, Mark. "The effects of lateral boundary conditions on a two-dimensional cloud model /." Thesis, McGill University, 1986. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=65503.
Повний текст джерелаPapageorgiou, I. G. "Mesoscale modelling of the atmospheric boundary layer including pollutant dispersion of a coastal area." Thesis, University of Reading, 1985. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.356134.
Повний текст джерелаZhou, Jingnan. "Numerical studies of stably stratified planetary boundary-layer flows over topography and their parameterization for large scale numerical model." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1997. http://www.collectionscanada.ca/obj/s4/f2/dsk3/ftp05/mq27395.pdf.
Повний текст джерелаVogel, Christoph Alexander. "An investigation of the role of flux divergence in the turbulent kinetic energy balance of the atmospheric surface layer." Diss., Georgia Institute of Technology, 1992. http://hdl.handle.net/1853/25789.
Повний текст джерелаCurry, Michelle. "An examination of lake breezes in southern Manitoba." Atmosphere-Ocean, 2015. http://hdl.handle.net/1993/31077.
Повний текст джерелаFebruary 2016
Cardon, Sandra Jean. "Obtaining eddy fluxes for a non-homogeneous environment using wavelet cospectra." Laramie, Wyo. : University of Wyoming, 2007. http://proquest.umi.com/pqdweb?did=1320974421&sid=1&Fmt=2&clientId=18949&RQT=309&VName=PQD.
Повний текст джерелаMcCaa, James Robert. "A new parameterization of marine stratocumulus and shallow cumulus clouds for climate models /." Thesis, Connect to this title online; UW restricted, 2001. http://hdl.handle.net/1773/10019.
Повний текст джерелаDusek, Ulrike. "Characterization of marine boundary layer aerosol from north Atlantic and European sources : physical and chemical properties and climate forcing parameters /." Thesis, Connect to this title online; UW restricted, 2002. http://hdl.handle.net/1773/10065.
Повний текст джерелаMauritsen, Thorsten. "On the Arctic Boundary Layer : From Turbulence to Climate." Doctoral thesis, Stockholm : Department of Meteorology, Stockholm University, 2007. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-6585.
Повний текст джерелаSöderberg, Stefan. "Mesoscale dynamics and boundary-layer structure in topographically forced low-level jets." Doctoral thesis, Stockholm University, Department of Meteorology, 2004. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-63.
Повний текст джерелаTwo types of mesoscale wind-speed jet and their effects on boundary-layer structure were studied. The first is a coastal jet off the northern California coast, and the second is a katabatic jet over Vatnajökull, Iceland. Coastal regions are highly populated, and studies of coastal meteorology are of general interest for environmental protection, fishing industry, and for air and sea transportation. Not so many people live in direct contact with glaciers but properties of katabatic flows are important for understanding glacier response to climatic changes. Hence, the two jets can potentially influence a vast number of people.
Flow response to terrain forcing, transient behavior in time and space, and adherence to simplified theoretical models were examined. The turbulence structure in these stably stratified boundary layers was also investigated. Numerical modeling is the main tool in this thesis; observations are used primarily to ensure a realistic model behavior.
Simple shallow-water theory provides a useful framework for analyzing high-velocity flows along mountainous coastlines, but for an unexpected reason. Waves are trapped in the inversion by the curvature of the wind-speed profile, rather than by an infinite stability in the inversion separating two neutral layers, as assumed in the theory. In the absence of blocking terrain, observations of steady-state supercritical flows are not likely, due to the diurnal variation of flow criticality.
In many simplified models, non-local processes are neglected. In the flows studied here, we showed that this is not always a valid approximation. Discrepancies between simulated katabatic flow and that predicted by an analytical model are hypothesized to be due to non-local effects, such as surface inhomogeneity and slope geometry, neglected in the theory. On a different scale, a reason for variations in the shape of local similarity scaling functions between studies is suggested to be differences in non-local contributions to the velocity variance budgets.
Cooper, Grant Alexander. "Variational retrieval of Eastern Pacific atmospheric boundary layer parameters using ATOVS with the COAMPSi mesoscale forecast system /." Monterey, Calif. : Springfield, Va. : Naval Postgraduate School ; Available from National Technical Information Service, 2002. http://library.nps.navy.mil/uhtbin/hyperion-image/02sep%5FCooper%5FPhD.pdf.
Повний текст джерелаDissertation co-advisors: Phillip A. Durkee, Nancy L. Baker. Includes bibliographical references (p. 235-242). Also available online.
Miao, Qun. "Fine-scale vertical structure of clear-air echoes during the International H₂O Project as detected by an airborne Doppler radar." Laramie, Wyo. : University of Wyoming, 2006. http://proquest.umi.com/pqdweb?did=1296094731&sid=1&Fmt=2&clientId=18949&RQT=309&VName=PQD.
Повний текст джерелаDasi, Lakshmi Prasad. "Statistical characteristics of turbulent chemical plumes." Thesis, Georgia Institute of Technology, 2000. http://hdl.handle.net/1853/21256.
Повний текст джерелаMathieu, Nathalie. "A study of atmospheric properties and their impact on the use of the nocturnal boundary layer budget technique for trace gas measurement /." Thesis, McGill University, 2004. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=82291.
Повний текст джерелаCrofoot, Robert F. "Investigations of scalar transfer coefficients in fog during the Coupled Boundary Layers and Air Sea Transfer Experiment : a case study." Thesis, Monterey, California. Naval Postgraduate School, 2004. http://hdl.handle.net/10945/1202.
Повний текст джерелаNappo, Carmen Joseph. "A theoretical investigation of gravity-wave-generated stress and vorticity in the planetary boundary layer." Diss., Georgia Institute of Technology, 1989. http://hdl.handle.net/1853/25697.
Повний текст джерелаKhairoutdinov, Marat. "Large-eddy simulation of stratocumulus-topped boundary layer with an explicit and a new bulk microphysics scheme /." Full-text version available from OU Domain via ProQuest Digital Dissertations, 1997.
Знайти повний текст джерелаPark, Sungsu. "ENSO-related marine cloud variation and new single column marine boundary layer cloud modeling /." Thesis, Connect to this title online; UW restricted, 2002. http://hdl.handle.net/1773/10080.
Повний текст джерелаHobson-Dupont, Maximillian. "The development of a small scale wind tunnel simulating the atmospheric boundary layer in support of a stochastic wind model." Thesis, San Jose State University, 2015. http://pqdtopen.proquest.com/#viewpdf?dispub=1593083.
Повний текст джерелаThere has been much success in atmospheric boundary layer simulation with medium sized closed-circuit wind tunnels with test section dimensions of approximately 1 x 1 m. However, smaller, blower-type wind tunnels are more common in university laboratories due to the lower cost and smaller space requirements. A small size, open flow wind tunnel with a 1 x 1 foot test section was modified to simulate the atmospheric boundary layer with a combination of upstream spires and cubic roughness elements. The primitive spire geometry detailed in the literature was found to yield poor agreement with the power law velocity profile of interest, and a novel iterative algorithm was developed to produce nonlinear spire geometry. The geometry generated by the algorithm was tested in the wind tunnel and found to simulate the desired velocity profile based on a Hellman exponent of 0.20 with a high degree of agreement, having a maximum velocity error of 4%. This confirmed the suitability of small-sized wind tunnels for simulating the atmospheric boundary layer.