Relevant bibliographies by topics / Meteorology. Atmospheric physics

Contents

  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers

Academic literature on the topic 'Meteorology. Atmospheric physics'

Author: Grafiati
Published: 4 June 2021
Last updated: 1 February 2022

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Journal articles on the topic "Meteorology. Atmospheric physics"

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Morris, C. E., D. C. Sands, M. Bardin, R. Jaenicke, B. Vogel, C. Leyronas, P. A. Ariya, and R. Psenner. "Microbiology and atmospheric processes: an upcoming era of research on bio-meteorology." Biogeosciences Discussions 5, no. 1 (January 15, 2008): 191–212. http://dx.doi.org/10.5194/bgd-5-191-2008.

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Abstract. For the past 200 years, the field of aerobiology has explored the abundance, diversity, survival and transport of micro-organisms in the atmosphere. Micro-organisms have been explored as passive and severely stressed riders of atmospheric transport systems. Recently, an interest in the active roles of these micro-organisms has emerged along with proposals that the atmosphere is a global biome for microbial metabolic activity and perhaps even multiplication. As part of a series of papers on the sources, distribution and roles in atmospheric processes of biological particles in the atmosphere, here we describe the pertinence of questions relating to the potential roles that air-borne micro-organisms might play in meteorological phenomena. For the upcoming era of research on the role of air-borne micro-organisms in meteorological phenomena, one important challenge is to go beyond descriptions of abundance of micro-organisms in the atmosphere toward an understanding of their dynamics in terms of both biological and physico-chemical properties and of the relevant transport processes at different scales. Another challenge is to develop this understanding under contexts pertinent to their potential role in processes related to atmospheric chemistry, the formation of clouds, precipitation and radiative forcing. This will require truly interdisciplinary approaches involving collaborators from the biological and physical sciences, from disciplines as disparate as agronomy, microbial genetics and atmosphere physics, for example.
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Keen, B. A. "Soil physics in relation to meteorology." Quarterly Journal of the Royal Meteorological Society 58, no. 245 (September 10, 2007): 229–50. http://dx.doi.org/10.1002/qj.49705824504.

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Baklanov, Alexander, Dominik Brunner, Gregory Carmichael, Johannes Flemming, Saulo Freitas, Michael Gauss, Øystein Hov, et al. "Key Issues for Seamless Integrated Chemistry–Meteorology Modeling." Bulletin of the American Meteorological Society 98, no. 11 (November 1, 2017): 2285–92. http://dx.doi.org/10.1175/bams-d-15-00166.1.

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Abstract Online coupled meteorology–atmospheric chemistry models have greatly evolved in recent years. Although mainly developed by the air quality modeling community, these integrated models are also of interest for numerical weather prediction and climate modeling, as they can consider both the effects of meteorology on air quality and the potentially important effects of atmospheric composition on weather. This paper summarizes the main conclusions from the “Symposium on Coupled Chemistry–Meteorology/Climate Modelling: Status and Relevance for Numerical Weather Prediction, Air Quality and Climate Research,” which was initiated by the European COST Action ES1004 “European Framework for Online Integrated Air Quality and Meteorology Modelling (EuMetChem).” It offers a brief review of the current status of online coupled meteorology and atmospheric chemistry modeling and a survey of processes relevant to the interactions between atmospheric physics, dynamics, and composition. In addition, it highlights scientific issues and emerging challenges that require proper consideration to improve the reliability and usability of these models for three main application areas: air quality, meteorology (including weather prediction), and climate modeling. It presents a synthesis of scientific progress in the form of answers to nine key questions, and provides recommendations for future research directions and priorities in the development, application, and evaluation of online coupled models.
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Anderson, P. S., and W. D. Neff. "Boundary layer physics over snow and ice." Atmospheric Chemistry and Physics Discussions 7, no. 3 (June 4, 2007): 7625–77. http://dx.doi.org/10.5194/acpd-7-7625-2007.

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Abstract. A general understanding of the physics of advection and turbulent mixing within the near surface atmosphere assists the interpretation and predictive power of air chemistry theory. The theory of the physical processes involved in diffusion of trace gas reactants in the near surface atmosphere is still incomplete. Such boundary layer theory is least understood over snow and ice covered surfaces, due in part to the thermo-optical properties of the surface. Polar boundary layers have additional aspects to consider, due to the possibility of long periods without diurnal forcing and enhanced Coriolis effects. This paper provides a review of present concepts in polar boundary layer meteorology, which will generally apply to atmospheric flow over snow and ice surfaces. It forms a companion paper to the chemistry review papers in this special issue of ACP.
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Baklanov, A., K. Schlünzen, P. Suppan, J. Baldasano, D. Brunner, S. Aksoyoglu, G. Carmichael, et al. "Online coupled regional meteorology chemistry models in Europe: current status and prospects." Atmospheric Chemistry and Physics 14, no. 1 (January 10, 2014): 317–98. http://dx.doi.org/10.5194/acp-14-317-2014.

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Abstract. Online coupled mesoscale meteorology atmospheric chemistry models have undergone a rapid evolution in recent years. Although mainly developed by the air quality modelling community, these models are also of interest for numerical weather prediction and regional climate modelling as they can consider not only the effects of meteorology on air quality, but also the potentially important effects of atmospheric composition on weather. Two ways of online coupling can be distinguished: online integrated and online access coupling. Online integrated models simulate meteorology and chemistry over the same grid in one model using one main time step for integration. Online access models use independent meteorology and chemistry modules that might even have different grids, but exchange meteorology and chemistry data on a regular and frequent basis. This article offers a comprehensive review of the current research status of online coupled meteorology and atmospheric chemistry modelling within Europe. Eighteen regional online coupled models developed or being used in Europe are described and compared. Topics discussed include a survey of processes relevant to the interactions between atmospheric physics, dynamics and composition; a brief overview of existing online mesoscale models and European model developments; an analysis on how feedback processes are treated in these models; numerical issues associated with coupled models; and several case studies and model performance evaluation methods. Finally, this article highlights selected scientific issues and emerging challenges that require proper consideration to improve the reliability and usability of these models for the three scientific communities: air quality, numerical meteorology modelling (including weather prediction) and climate modelling. This review will be of particular interest to model developers and users in all three fields as it presents a synthesis of scientific progress and provides recommendations for future research directions and priorities in the development, application and evaluation of online coupled models.
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Anderson, P. S., and W. D. Neff. "Boundary layer physics over snow and ice." Atmospheric Chemistry and Physics 8, no. 13 (July 7, 2008): 3563–82. http://dx.doi.org/10.5194/acp-8-3563-2008.

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Abstract. Observations of the unique chemical environment over snow and ice in recent decades, particularly in the polar regions, have stimulated increasing interest in the boundary layer processes that mediate exchanges between the ice/snow interface and the atmosphere. This paper provides a review of the underlying concepts and examples from recent field studies in polar boundary layer meteorology, which will generally apply to atmospheric flow over snow and ice surfaces. It forms a companion paper to the chemistry review papers in this special issue of ACP that focus on processes linking halogens to the depletion of boundary layer ozone in coastal environments, mercury transport and deposition, snow photochemistry, and related snow physics. In this context, observational approaches, stable boundary layer behavior, the effects of a weak or absent diurnal cycle, and transport and mixing over the heterogeneous surfaces characteristic of coastal ocean environments are of particular relevance.
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Croft, Paul J. "Assessing “The Excitement of Meteorology!” for Young Scholars." Bulletin of the American Meteorological Society 80, no. 5 (May 1, 1999): 879–92. http://dx.doi.org/10.1175/1520-0477-80.5.879.

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The National Science Foundation Young Scholar Program “The Excitement of Meteorology!” successfully brought the atmospheric and related sciences to high school students in Mississippi. The four-week summer program was administered through the Jackson State University Meteorology Program in the Department of Physics, Atmospheric Sciences, and General Science and was supported by the Mississippi Science Partnership program office. This commuter program provided an opportunity to learn, study, and research the field of meteorology. Through instructional sessions, laboratories, field trips, and peer contact participants were exposed to the concepts of atmospheric motion, the development of storms, and the practical application of meteorology during a one-month period. The program was intended to help students make their own career decisions and to foster their interest in the sciences and meteorology. The goals and objectives of the program were to develop basic science skills; make participants aware of the interdisciplinary nature of meteorology; provide participants with the opportunity to see and hear the meteorologist as a researcher, teacher, and communicator; provide the information and incentive necessary for participants to choose a career in meteorology or the sciences; make participants aware of the various employment opportunities in the field; and show the moral and ethical responsibilities and importance of atmospheric science to society. Thirty sophomore and junior high school student participants (22 females and 8 males, nearly all of whom were African–American) completed the program. All were tested on their meteorological knowledge and skills gained during the program and questioned about their field and lecture experiences. They also “graded” the effectiveness of all speakers, presentations, videotapes, and laboratory sessions. Through surveys it was found that the participants' desire to pursue a science career and to go to college were increased by the program. They also indicated that the program objectives had been met and that the program had met their expectations. They were particularly pleased with the opportunity to work in a college setting and with professional scientists.
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Cheruy, F., A. Campoy, J. C. Dupont, A. Ducharne, F. Hourdin, M. Haeffelin, M. Chiriaco, and A. Idelkadi. "Combined influence of atmospheric physics and soil hydrology on the simulated meteorology at the SIRTA atmospheric observatory." Climate Dynamics 40, no. 9-10 (August 19, 2012): 2251–69. http://dx.doi.org/10.1007/s00382-012-1469-y.

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Haupt, Sue Ellen, Robert M. Rauber, Bruce Carmichael, Jason C. Knievel, and James L. Cogan. "100 Years of Progress in Applied Meteorology. Part I: Basic Applications." Meteorological Monographs 59 (January 1, 2018): 22.1–22.33. http://dx.doi.org/10.1175/amsmonographs-d-18-0004.1.

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Abstract The field of atmospheric science has been enhanced by its long-standing collaboration with entities with specific needs. This chapter and the two subsequent ones describe how applications have worked to advance the science at the same time that the science has served the needs of society. This chapter briefly reviews the synergy between the applications and advancing the science. It specifically describes progress in weather modification, aviation weather, and applications for security. Each of these applications has resulted in enhanced understanding of the physics and dynamics of the atmosphere, new and improved observing equipment, better models, and a push for greater computing power.
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Paine, Robert J. "Tenth Joint Conference on Applications of Air Pollution Meteorology." Bulletin of the American Meteorological Society 80, no. 9 (September 1, 1999): 1907–19. http://dx.doi.org/10.1175/1520-0477-80.9.1907.

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The tenth in a continuing series of joint conferences between the American Meteorological Society and the Air and Waste Management Association on meteorological aspects of air pollution was held 11–16 January 1998 in Phoenix, Arizona. Diverse topics in air dispersion modeling, boundary layer meteorology, cloud physics, atmospheric chemistry, fluid mechanics, and engineering were presented at the conference. A summary of the presentations made at the conference is provided.
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Dissertations / Theses on the topic "Meteorology. Atmospheric physics"

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Potvin, 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.

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Froelich, Norma Jeanne. "Modeling of thermotopographic flows in forested terrain." [Bloomington, Ind.] : Indiana University, 2009. 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:3386677.

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Thesis (Ph.D.)--Indiana University, Dept. of Geography, 2009.
Title from PDF t.p. (viewed on Jul 20, 2010). Source: Dissertation Abstracts International, Volume: 70-12, Section: B, page: 7439. Advisers: Scott Robeson; Hans Peter Schmid.
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Malinga, Sandile Bethuel. "A comparative study of atmospheric dynamics in the mesosphere and lower thermosphere (MLT) near Grahamstown (South Africa) and Adelaide (Australia)." Thesis, Rhodes University, 2002. http://hdl.handle.net/10962/d1007307.

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The observations made near Grahamstown (33 .3°S, 26.5°E), South Africa and Adelaide (34.5°S, 138.5°E), Australia over the years 1987 to 1994 are used to study the dynamics of the mesosphere and lower thermosphere (ML T) region with a focus on ∼ 90 km altitude. In particular this thesis deals with on the atmospheric mean flow and the solar diurnal and semi diurnal oscillations with a view to (i) deducing their patterns at the two sites, (ii) comparing the dynamic structures observed at the two sites with special emphases on longitudinal variations, and (iii) putting these observations in a global context by comparing with other ground-based observations, satellite observations and numerical simulations. The main findings are summarised below. The mean flow and the tides at Grahamstown and Adelaide are characteristically variable at planetary time scales. Wavelet spectral and multiresolution analyses reveal that the dominant planetary oscillation is the quasi-16-day oscillation. However, no apparent correlation in the 16-day waves of the mean flow, the diurnal tide and the semidiurnal tide was found. The short-term fluctuations were also investigated using complex demodulation and bispectral techniques and it was found that some of the observed variations in tides could be due to non-linear wave-wave interactions. The long-term trends of the mean flow and tides show patterns that are in broad agreement with theory, results from elsewhere (ground-based and satellite) and the results of the Global-Scale Wave Model and various models by Portnyagin and others. In general the mean flow, the amplitudes and phases of both tides were found to exhibit seasonal and interannual variations which are thought to be related to various factors including (i) changes in the atmospheric mean environment, (ii) thermotidal forcing (iii) gravity wave effects, (iv) planetary scale influence, (v) long-term (e.g. quasi-biennial oscillation) modulation, and (vi) solar activity. There are significant longitudinal differences in the dynamic structure between Grahamstown and Adelaide. More especially, Grahamstown tends to have stronger mean flow and tidal activity than Adelaide. For tides, these differences are thought to be partly due to nonmigrating tidal modes but, in general, migrating modes were found to be dominant.
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Lewis, Michael M. "Development and evolution of cirrus in a mesoscale model." Thesis, Monterey, Calif. : Springfield, Va. : Naval Postgraduate School ; Available from National Technical Information Service, 2006. http://library.nps.navy.mil/uhtbin/hyperion/06Mar%5FLewis.pdf.

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Vellore, Ramesh K. "Challenges in forecasting the cloud-capped marine boundary layer and utilization of satellite data to improve mesoscale modeling." abstract and full text PDF (free order & download UNR users only), 2006. http://0-gateway.proquest.com.innopac.library.unr.edu/openurl?url_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:dissertation&res_dat=xri:pqdiss&rft_dat=xri:pqdiss:3239879.

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Lathem, Terry Lee. "On the water uptake of atmospheric aerosol particles." Diss., Georgia Institute of Technology, 2012. http://hdl.handle.net/1853/50112.

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The feedbacks among aerosols, clouds, and radiation are important components for understanding Earth's climate system and quantifying human-induced climate change, yet the magnitude of these feedbacks remain highly uncertain. Since every cloud droplet in the atmosphere begins with water condensing on a pre-existing aerosol particle, characterizing the ability of aerosols to uptake water vapor and form cloud condensation nuclei (CCN) are key to understanding the microphysics behind cloud formation, as well as assess the impact aerosols have on the Earth system. Through a combination of controlled laboratory experiments and field measurements, this thesis characterizes the ability of atmospheric aerosols to uptake water vapor and become CCN at controlled levels of water vapor supersaturation. The origin of the particle water uptake, termed hygroscopicity, is also explored, being from either the presence of deliquescent soluble material and/or adsorption onto insoluble surfaces. The data collected and presented is comprehensive and includes (1) ground samples of volcanic ash, collected from six recent eruptions re-suspended in the laboratory for analysis, (2) laboratory chamber and flow-tube studies on the oxidation and uptake of surface active organic compounds, and (3) in-situ aircraft measurements of aerosols from the Arctic background, Canadian boreal forests, fresh and aged biomass burning, anthropogenic industrial pollution, and from within tropical cyclones in the Atlantic basin. Having a more thorough understanding of aerosol water uptake will enable more accurate representation of cloud droplet number concentrations in global models, which can have important implications on reducing the uncertainty of aerosol-cloud-climate interactions, as well as additional uncertainties in aerosol transport, atmospheric lifetime, and impact on storm dynamics.
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Han, Weiqing. "Influence of Salinity on Dynamics, Thermodynamics and Mixed-Layer Physics in the Indian Ocean." NSUWorks, 1999. http://nsuworks.nova.edu/occ_stuetd/62.

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A nonlinear, 4½-layer model with active thermodynamics and mixed-layer physics is used to examine salinity effects due to various forcings in the Indian Ocean. Theses forcings include: evaporation (ε) and precipitation (Ρ), river runoff in the Bay of Bengal, the Indonesian Throughflow, and the influx of salty waters from the Persian Gulf and the Red Sea. Solutions with P - ε forcing produce salinity patterns that agree qualitatively with the observations in the upper three layers. Quantitatively, however, salinity values tend to be higher than the observations in most of the basin. In regions where precipitation is strong (P - ε » 0), a thin surface mixed layer (layer 1), and thus a thicker seasonal thermocline (layer 2, a barrier layer), are formed due to decreased entrainment. In these regions, surface currents generally strengthen, T2 warms considerably and SST increases somewhat, resulting in temperature inversions at some locations of the southern Bay and the eastern equatorial ocean. Somewhat surprisingly, P - ε also causes large temperature changes in layer 3 (thermocline) and thickness changes in layers 3 and 4 (intermediate water). The Bay-of-Bengal river runoff improves salinity values significantly in the upper three layers, especially within the Bay and alongC the west coast of India. During the Southwest onsoon (SWM), coastal Kelvin waves driven by the Ganges-Brahmaputra river inflow suppress upwelling along the northeast coast of India, increasing SST by 1°C. During the Northeast Monsoon (NEM), fresh water from the rivers is carried southward by the East India Coastal Current (EICC), raising sea level and thus strengthening the EICGby 10 cm/s. This fresh water can flow directly through the India-Sri Lanka separation in the surface mixed layer, generating a strong salinity gradient along the west Indian coast during winter. The river water decreases entrainment around the perimeter of the Bay during winter, thereby producing a thin surface mixed layer, increasing T2 , and resulting in temperature inversions in the northwestern Bay. Like P - ε, the rivers cause significant thickness and temperature anomalies in layer 3. The Indonesian Throughflow improves salinities in all four layers of the model, especially in the southern tropical ocean. Consistent with previous studies, most of the Throughflow water flows out of the Indian Ocean along the western boundary and near Madagascar. A significant amount of water, however, is advected northward into the Somali basin and subsequently carried eastward into the ocean interior and northward into the Arabian Sea. The Throughflow increases SST primarily along the west Australian coast but warms the thermocline (layer 3) throughout the Indian Ocean, especially in the southern tropical ocean. As a consequence, sea level is raised in the entire basin. Warmer and saltier Persian-Gulf water (PGW) enters the Indian Ocean in layer 3, warming the northern Arabian Sea by 0.2-2°C and increasing the salinity by 0.1-0.6 psu through horizontal mixing. It increases sea-surface salinity (SSS) in a broad region of the Arabian Sea by 0.1- 0.2 psu because entrainment and, to a less extent, coastal upwelling bring PGW into the surface mixed layer, where it spreads over a large region due to advection. High-salinity and high-temperature Red-Sea water (RSW) warms layer-4 (upper intermediate layer) and increases its salinity by a significant amount in most region of the Indian Ocean, especially in the Somali Basin, the interior Arabian Sea, and the central and western equatorial ocean.
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Fenlason, Joel W. "Accuracy of tropical cyclone induced winds using TYDET at Kadena AB." Thesis, Monterey, Calif. : Springfield, Va. : Naval Postgraduate School ; Available from National Technical Information Service, 2006. http://library.nps.navy.mil/uhtbin/hyperion/06Mar%5FFenlason.pdf.

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Munoz, Esparza Domingo. "Multiscale modelling of atmospheric flows: towards improving the representation of boundary layer physics." Doctoral thesis, Universite Libre de Bruxelles, 2013. http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/209363.

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Atmospheric boundary layer flows are characterized by the coexistence of a broad range of scales. These scales cover from synoptic- (100-5000 km) and meso-scales (1-100 km) up to three-dimensional micro-scale turbulence (less than a few kilometers). This multiscale nature inherent to atmospheric flows clearly determines the behaviour of the atmospheric boundary layer, whose structure and evolution are of major importance for the wind energy community. This PhD thesis is focused on the development of a numerical methodology that allows to include contribution from all the above mentioned scales, with the purpose of improving the representation of boundary layer processes. The multiscale numerical methodology is developed based on a numerical weather prediction (NWP) model, the Weather Research and Forecasting (WRF) model.

Prior to the development of the multiscale numerical methodology, one-year of sonic anemometer and wind LiDAR measurements from the FINO1 offshore platform are analyzed. A comprehensive database of offshore measurements in the lowest 250 m of the boundary layer is developed after quality data check and correction for flow distortion effects by the measurement mast, allowing the characterization of the offshore conditions at FINO1. Spectral analysis of high frequency sonic anemometer measurements is used to estimate a robust averaing time for the turbulent fluxes that minimizes non-universal contributions from mesoscale structures but captures the contribution from boundary layer turbulence, employing the Ogive function concept. A stability classification of the measurements is carried out based on the Obukhov length. Results compare well to other surface layer observational studies while vertical wind speed profiles exhibit the expected stability-dependency.

Although NWP models have been extensively used for weather forecasting purposes, a comprehensive analysis of its suitability to meet the wind energy requirements needs to be carried out. The applicability of the WRF mesoscale model to reproduce offshore boundary layer characteristics is evaluated and validated against field measurements from FINO1. The ability of six planetary boundary layer (PBL) parameterizations to account for stability effects is analyzed. Overall, PBL parameterizations are rather accurate in reproducing the vertical structure of the boundary layer for convective and neutral stabilities. However, difficulties are found under stable stratifications, due to the general tendency of PBL formulations to be overdiffusive and therefore, not capable to develope the strong vertical gradients found in the observations. A low-level jet and a very shallow boundary layer cases are simulated to provide further insights into the limits of the parameterizations.

Large-eddy simulations (LES) based on averaged conditions from a convective episode at FINO1 are conducted to understand the mechanisms of transition and equilibration that occur in turbulent one-way nested simulations. The nonlinear backscatter and anisotropy subgrid scale model with a prognostic turbulent kinetic energy equation is found to be capable of providing similar results when performing one-way nested large-eddy simulations to a reference stand-alone domain using periodic lateral boundary conditions. A good agreement is obtained in terms of velocity shear and turbulent fluxes of heat and momentum, while velocity variances are overestimated. A considerable streamwise fetch is needed following each domain transition for appropriate energy levels to be reached at high wavelengths and for the solution to reach quasi-stationary results. A pile-up of energy is observed at low wavelengths on the first nested domain, mitigated by the inclusion of a second nested domain with higher resolution that allows the development of an appropriate turbulent energy cascade.

As the final step towards developing the multiscale capabilities of WRF, the specific problem of the transition from meso- to micro-scales in atmospheric models is addressed. The challenge is to generate turbulence on inner LES domain from smooth mesoscale inflow. Several new methods are proposed to trigger the development of turbulent features. The inclusion of adequate potential temperature perturbations near the inflow boundaries of the LES domain results in a very good agreement of mean velocity profiles, variances and turbulent fluxes, as well as velocity spectra, when compared to periodic stand-alone simulations. This perturbation method allows an efficient generation of fully developed turbulence and is tested under a broad range of atmospheric stabilities: convective, neutral and stable conditions, showing successful results in all the regimes.
Doctorat en Sciences de l'ingénieur
info:eu-repo/semantics/nonPublished

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Monaghan, Andrew J. "Recent variability and trends in antarctic snowfall accumulation and near-surface air temperature." Columbus, Ohio : Ohio State University, 2007. http://rave.ohiolink.edu/etdc/view?acc%5Fnum=osu1173210638.

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Books on the topic "Meteorology. Atmospheric physics"

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Physical meteorology. Cambridge, Mass: MIT Press, 1985.

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Physics of atmospheres. 3rd ed. Cambridge, U.K: Cambridge University Press, 2002.

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Helmis, Costas G., and Panagiotis T. Nastos, eds. Advances in Meteorology, Climatology and Atmospheric Physics. Berlin, Heidelberg: Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-642-29172-2.

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Atmospheric dynamics. Cambridge: Cambridge University Press, 2011.

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Emanuel, Kerry A. Atmospheric convection. New York: Oxford University Press, 1994.

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Tsing-Chang, Chen, ed. Fundamentals of atmospheric energetics. New York: Oxford University Press, 1993.

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Atmospheric dynamics. Cambridge, UK: Cambridge University Press, 1999.

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McIlveen, J. F. R. Basic meteorology: A physical outline. Wokingham, Berkshire, England: Van Nostrand Reinhold (UK), 1986.

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The physics of atmospheres. 2nd ed. Cambridge [Cambridgeshire]: Cambridge University Press, 1986.

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Capitelli, Mario. Plasma Kinetics in Atmospheric Gases. Berlin, Heidelberg: Springer Berlin Heidelberg, 2000.

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Book chapters on the topic "Meteorology. Atmospheric physics"

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Selvam, Amujuri Mary. "Nonlinear Dynamics and Chaos: Applications in Meteorology and Atmospheric Physics." In Springer Atmospheric Sciences, 1–40. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-54546-2_1.

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Karagiannidis, A. F., A. G. Triantafyllou, and T. Karacostas. "The Meteorological Setting of a Particulate Air Pollution Episode During November 2009, in Western Macedonia Industrial Area, Greece." In Advances in Meteorology, Climatology and Atmospheric Physics, 159–67. Berlin, Heidelberg: Springer Berlin Heidelberg, 2012. http://dx.doi.org/10.1007/978-3-642-29172-2_23.

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Kolios, S., and H. Feidas. "Nowcasting a Mesoscale Convective System Over Greece with a Satellite-Based Algorithm." In Advances in Meteorology, Climatology and Atmospheric Physics, 195–201. Berlin, Heidelberg: Springer Berlin Heidelberg, 2012. http://dx.doi.org/10.1007/978-3-642-29172-2_28.

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Bakas, N. A., and P. J. Ioannou. "On a Dynamical Mechanism Underlying the Intensification of Tropical Cyclones." In Advances in Meteorology, Climatology and Atmospheric Physics, 21–26. Berlin, Heidelberg: Springer Berlin Heidelberg, 2012. http://dx.doi.org/10.1007/978-3-642-29172-2_4.

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Chronopoulou, C., and A. Mavrakis. "Indications of Stability of Occurrence of Halcyon Days in the Ancient Greek Drama." In Advances in Meteorology, Climatology and Atmospheric Physics, 403–8. Berlin, Heidelberg: Springer Berlin Heidelberg, 2012. http://dx.doi.org/10.1007/978-3-642-29172-2_57.

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Alexakis, D. D., D. G. Hadjimitsis, S. Michaelides, I. Tsanis, A. Retalis, C. Demetriou, A. Agapiou, et al. "Application of GIS and Remote Sensing Techniques for Flood Risk Assessment in Cyprus." In Advances in Meteorology, Climatology and Atmospheric Physics, 3–8. Berlin, Heidelberg: Springer Berlin Heidelberg, 2012. http://dx.doi.org/10.1007/978-3-642-29172-2_1.

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Efstathiou, G., D. Melas, N. Zoumakis, and P. A. Kassomenos. "Evaluation of WRF-ARW Model in Reproducing a Heavy Rainfall Event Over Chalkidiki, Greece: The Effect of Land-Surface Features on Rainfall." In Advances in Meteorology, Climatology and Atmospheric Physics, 65–71. Berlin, Heidelberg: Springer Berlin Heidelberg, 2012. http://dx.doi.org/10.1007/978-3-642-29172-2_10.

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Rousi, E., C. Anagnostopoulou, K. Tolika, P. Maheras, and A. Bloutsos. "ECHAM5/MPI General Circulation Model Simulations of Teleconnection Indices Over Europe." In Advances in Meteorology, Climatology and Atmospheric Physics, 709–15. Berlin, Heidelberg: Springer Berlin Heidelberg, 2012. http://dx.doi.org/10.1007/978-3-642-29172-2_100.

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Serbis, E., C. J. Lolis, and P. A. Kassomenos. "Atmospheric Circulation Characteristics Associated with high Static Instability Conditions Over the Athens Region." In Advances in Meteorology, Climatology and Atmospheric Physics, 717–22. Berlin, Heidelberg: Springer Berlin Heidelberg, 2012. http://dx.doi.org/10.1007/978-3-642-29172-2_101.

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Skourkeas, A., F. Kolyva-Machera, and P. Maheras. "Construction of Winter Temperature Scenarios over Greece, Using an Alternative Statistical Downscaling Model Based on CCA." In Advances in Meteorology, Climatology and Atmospheric Physics, 723–28. Berlin, Heidelberg: Springer Berlin Heidelberg, 2012. http://dx.doi.org/10.1007/978-3-642-29172-2_102.

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Conference papers on the topic "Meteorology. Atmospheric physics"

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Gordov, Evgeny, Igor Okladnikov, Alexander Titov, and Alexander Fazliev. "Virtual research environment supporting applied meteorology and climatology problem solving." In XXIV International Symposium, Atmospheric and Ocean Optics, Atmospheric Physics, edited by Oleg A. Romanovskii and Gennadii G. Matvienko. SPIE, 2018. http://dx.doi.org/10.1117/12.2504561.

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Smith, Suzanne W., Phillip B. Chilson, Adam L. Houston, and Jamey D. Jacob. "Catalyzing Collaboration for Multi-Disciplinary UAS Development with a Flight Campaign Focussed on Meteorology and Atmospheric Physics." In AIAA Information Systems-AIAA Infotech @ Aerospace. Reston, Virginia: American Institute of Aeronautics and Astronautics, 2017. http://dx.doi.org/10.2514/6.2017-1156.

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You might also be interested in the extended bibliographies on the topic 'Meteorology. Atmospheric physics' for particular source types:
Journal articles Dissertations / Theses Books
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