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Dissertations / Theses on the topic 'Global circulation models'

Author: Grafiati

Published: 4 June 2021

Last updated: 4 February 2022

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1

Dodd, James Paul. "Diagnostics and models of the global atmospheric water." Thesis, University of Reading, 1994. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.260662.

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2

Christidis, Nikolaos. "Halocarbon radiative forcing in radiation and general circulation models." Thesis, University of Reading, 1999. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.312563.

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3

Thorpe, Sally Elaine. "Variability of the Southern Antarctic circumpolar current in the Scotia Sea and its implications for transport to South Georgia." Thesis, University of East Anglia, 2001. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.368389.

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4

Anderson, Laurence Anthony. "The determination of Redfield ratios for use in global oceanic nutrient cycle models." [Princeton, N.J.] : Princeton University, Dept. of Geological and Geophysical Sciences, Program in Atmospheric and Oceanic Sciences, 1993. http://catalog.hathitrust.org/api/volumes/oclc/75401374.html.

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5

Beres, Jadwiga H. "Gravity waves generated by tropical convection : generation mechanisms and implications for global circulation models /." Thesis, Connect to this title online; UW restricted, 2002. http://hdl.handle.net/1773/10048.

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6

Phoon, Syin Yi. "Application of global circulation model results on hydrological conceptual models that simulate future river flows feeding Lake Victoria, East Africa." Thesis, University of Birmingham, 2006. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.443641.

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7

Beaumet, Julien. "Changement climatique en Antarctique : études à l'aide d'un modèle atmosphérique de circulation générale à haute résolution régionale." Thesis, Université Grenoble Alpes (ComUE), 2018. http://www.theses.fr/2018GREAU050/document.

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L'augmentation du bilan de masse en surface de la calotte polaire Antarctique causée par celle des chutes de neige est la seule contribution négative à l'élévation du niveau de mer attendue dans le courant du 21ème siècle dans le cadre du réchauffement climatique causé par les activités humaines. La régionalisation dynamique de projections climatiques issues de modèles couplés océans-atmosphère est la méthode la plus couramment utilisée pour estimer les variations futures du climat Antarctique. Néanmoins, de nombreuses incertitudes subsistent suite à l'application de ces méthodes, en particuli

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8

Lee, Graham Kim Huat. "Glass rain : modelling the formation, dynamics and radiative-transport of cloud particles in hot Jupiter exoplanet atmospheres." Thesis, University of St Andrews, 2017. http://hdl.handle.net/10023/11740.

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The atmospheres of exoplanets are being characterised in increasing detail by observational facilities and will be examined with even greater clarity with upcoming space based missions such as the James Webb Space Telescope (JWST) and the Wide Field InfraRed Survey Telescope (WFIRST). A major component of exoplanet atmospheres is the presence of cloud particles which produce characteristic observational signatures in transit spectra and influence the geometric albedo of exoplanets. Despite a decade of observational evidence, the formation, dynamics and radiative-transport of exoplanet atmosphe

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9

Neale, Richard Brian. "A study of the tropical response in an idealised global circulation model." Thesis, University of Reading, 1999. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.301957.

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10

Hosoe, Taro. "Stability of the global thermohaline circulation in an intermediate complexity ocean model." Thesis, University of Southampton, 2004. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.401832.

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11

Moffat, Tracy. "The UCL Martian thermosphere and ionosphere global circulation model : development and validation." Thesis, University College London (University of London), 2005. http://discovery.ucl.ac.uk/1445697/.

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Simulations of the Martian upper atmosphere have been produced from a self consis tent three dimensional numerical model of the Martian thermosphere and ionosphere called MarTIM. This model has been developed at UCL to cover an altitude range of 60km - 250km+. A radiation scheme is included that allows the main sources of heat input, EUV/UV and IR absorption by CO2 and CO, to be calculated. MarTIM self consistently calculates the composition of three of the main gases, CO2, N2 and 0, which are mutually diffused. These are treated as the major gases in the model. The other species densities (th

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12

Stemmler, Irene. "The role of the ocean in global cycling of persistent organic contaminants refinement and application of a global multicompartment chemistry transport model." Berlin Heidelberg Springer, 2009. http://d-nb.info/996662642/04.

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13

Pankine, Alexey A. "Low order model of Martian circulation and interannual variability of global dust storms." Diss., Pasadena, Calif. : California Institute of Technology, 2001. http://resolver.caltech.edu/CaltechETD:etd-11072001-160517.

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14

Betts, Richard Arthur. "Modelling the influence of the vegetated land surface on climate and climate change." Thesis, University of Reading, 1999. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.312335.

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15

Durgadoo, Jonathan V. "Circulation at the South-West Indian Ridge in a high-resolution global ocean model." Master's thesis, University of Cape Town, 2008. http://hdl.handle.net/11427/6469.

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Includes bibliographical references (leaves 76-86)<br>This study explores the use of the 1/4° and the 1/12° Ocean Circulation and Climate Advanced Modelling (OCCAM) project. The model's representation of the dynamic nature of this region is assessed. On average 2 - 3 intense and well-defined eddies are generated per year within the model; having mean longevities of 4.89 ± 2.20 months with average advection speeds of 5.51 ± 1.57 km day¯¹

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16

Demory, Marie-Estelle. "Sensitivity of the global hydrological cycle to horizontal resolution in an atmospheric general circulation model." Thesis, University of Reading, 2012. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.654493.

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17

Beraki, Asmerom Fissehatsion. "ECHAM4.5 global circulation model as a seasonal forecasting system for southern Africa : coupled vs. uncoupled." Thesis, University of Pretoria, 2015. http://hdl.handle.net/2263/53535.

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The predictive skill of seasonal forecast arises from the slowly evolving climate processes where the signature, that noticeably influence the mean state of weather conditions, mainly resides in the ocean. The interaction of the ocean and atmosphere is therefore the minimum level of complexity required for seasonal timescale. The practice of contemporary seasonal prediction is presumably achievable with the use of two distinct GCM (Global Climate Model) configurations commonly referred to as one- and two-tiered forecasting systems based on the manner in which the atmosphere and ocean exchange

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18

Kim, Joong Tae. "Enhancing the resolution of sea ice in long-term global ocean general circulation model (gcm) integrations." Texas A&M University, 2003. http://hdl.handle.net/1969.1/5746.

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Open water in sea ice, such as leads and polynyas, plays a crucial role in determining the formation of deep- and bottom-water, as well as their long-term global properties and circulation. Ocean general circulation models (GCMs) designed for studies of the long-term thermohaline circulation have typically coarse resolution, making it inevitable to parameterize subgrid-scale features such as leads and convective plumes. In this study, a hierarchy of higher-resolution sea-ice models is developed to reduce uncertainties due to coarse resolution, while keeping the ocean component at coarse resolu

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19

Schalge, Bernd Verfasser], and Klaus [Akademischer Betreuer] [Fraedrich. "Nonlinear Dynamics and Predictability in a Global Circulation Model of the Atmosphere / Bernd Schalge. Betreuer: Klaus Fraedrich." Hamburg : Staats- und Universitätsbibliothek Hamburg, 2014. http://d-nb.info/104928156X/34.

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20

Schalge, Bernd [Verfasser], and Klaus [Akademischer Betreuer] Fraedrich. "Nonlinear Dynamics and Predictability in a Global Circulation Model of the Atmosphere / Bernd Schalge. Betreuer: Klaus Fraedrich." Hamburg : Staats- und Universitätsbibliothek Hamburg, 2014. http://d-nb.info/104928156X/34.

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21

Brix, Holger. "North Atlantic deep water and antarctic bottom water their interaction and influence on modes of the global ocean circulation /." [S.l.] : [s.n.], 2001. http://deposit.ddb.de/cgi-bin/dokserv?idn=96315799X.

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22

Tsuboda, Yukimasa. "Analysis of the effect of solar irradiance variability on global sea surface temperature and climate : an investigation using the NASA, Goddard Institute for Space Studies General Circulation Model /." Access Digital Full Text version, 1995. http://pocketknowledge.tc.columbia.edu/home.php/bybib/12250417.

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Thesis (Ed.D.)--Teachers College, Columbia University, 1995.<br>Typescript; issued also on microfilm. Sponsor: Warren E. Yasso. Dissertation Committee: O. Roger Anderson. Includes bibliographical references (leaves 95-109).

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23

DOUTRIAUX, BOUCHER MARIE. "La couverture nuageuse globale : comparaison d'observations, validation de modeles de circulation generale et simulation de nouvelles technologies d'observations." Paris 6, 1997. http://www.theses.fr/1997PA066647.

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La couverture nuageuse est l'un des parametres majeurs de l'etude du systeme climatique. Le manque de connaissance sur cette couverture nuageuse represente une des incertitudes principales dans la modelisation du climat et la prevision des changements climatiques. En particulier, la repartition verticale des nuages dans l'atmosphere est un facteur determinant du bilan radiatif de la terre. Dans le but d'etudier cette structure verticale, nous utilisons deux jeux de donnees, les observations de surface (donnees warren et al. ) et les observations satellitales (donnees isccp) que nous commencons

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24

Lin, Nai Shi. "The response of the width of the Hadley cell to global warming-like thermal forcing in a simple general circulation model." Thesis, McGill University, 2011. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=97070.

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The response of the Hadley Cell (HC) width to the global warming is investigated using a set of dry global circulation model (GCM) integrations. In the model, global warming is mimicked by two thermal forcings: a warming in the tropical upper troposphere (THR) and a warming in polar lower atmosphere (PHR). A set of model integrations for the THR case, the PHR case and both of these cases combined (TPH) are performed with both the axisymmetric (2D) and non-axisymmetric (3D) model configurations. It is found that THR results in a clear poleward expansion of the Hadley circulation. By contrast, t

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25

Levine, Richard Chaim. "Changes in shelf waters due to air-sea fluxes and their influence on the Arctic Ocean circulation as simulated in the OCCAM global ocean model." Thesis, University of Southampton, 2005. https://eprints.soton.ac.uk/25111/.

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In this study we look at the ocean circulation of the Arctic Ocean in the high-resolution OCCAM global ocean model. The Arctic Ocean consists of deep basins surrounded by a large area of continental shelves, where cooling and ice formation play an important role in dense water formation. In the model these dense waters are transported by a circumpolar boundary current into the deep convection sites of the North Atlantic Ocean. The boundary current is thought to be a continuous feature in the real ocean, however the driving force is still unknown. We provide evidence that buoyancy fluxes that o

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26

Brand, Sascha. "Klimavariabilität der Tropo- und Stratosphäre in einem globalen gekoppelten Atmosphäre-Ozean-Modell mit vereinfachter stratosphärischer Chemie." Phd thesis, Universität Potsdam, 2007. http://opus.kobv.de/ubp/volltexte/2008/1660/.

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In dieser Arbeit wurde die Variabilität der Atmosphäre in einem neuen gekoppelten Klimamodell (ECHO-GiSP) untersucht, welches eine vereinfachte Stratosphärenchemie (bis 80 km Höhe) enthält. Es wurden 2 Simulationen über 150 Jahre durchgeführt. In einer der Simulationen wurde die atmosphärische Chemie modelliert, hatte aber keinen Einfluß auf die Dynamik des Klimamodelles. In der zweiten Simulation wurde hingegen die Wirkung der Chemie auf die Klimadynamik explizit berücksichtigt, die über die Strahlungsbilanz des Modelles erfolgt. Dies ist die erste Langzeitsimulation mit einem voll gekoppelt

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27

Schemann, Vera, Bjorn Stevens, Verena Grützun, and Johannes Quaas. "Scale dependency of total water variance and its implication for cloud parameterizations." Universitätsbibliothek Leipzig, 2015. http://nbn-resolving.de/urn:nbn:de:bsz:15-qucosa-177479.

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The scale dependency of variance of total water mixing ratio is explored by analyzing data from a general circulation model (GCM), a numerical weather prediction model (NWP), and large-eddy simulations (LESs). For clarification, direct numerical simulation (DNS) data are additionally included, but the focus is placed on defining a general scaling behavior for scales ranging from global down to cloud resolving. For this, appropriate power-law exponents are determined by calculating and approximating the power density spectrum. The large-scale models (GCM and NWP) show a consistent scaling with

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28

Dean, John Robert. "Improving Summer Drought Prediction in the Apalachicola-Chattahoochee- Flint River Basin with Empirical Downscaling." Digital Archive @ GSU, 2008. http://digitalarchive.gsu.edu/geosciences_theses/12.

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The Georgia General Assembly, like many states, has enacted pre-defined, comprehensive, drought-mitigation apparatus, but they need rainfall outlooks. Global circulation models (GCMs) provide rainfall outlooks, but they are too spatially course for jurisdictional impact assessment. To wed these efforts, spatially averaged, time-smoothed, daily precipitation observations from the National Weather Service cooperative network are fitted to eight points of 700 mbar atmospheric data from the NCEP/NCAR Reanalysis Project for climate downscaling and drought prediction in the Apalachicola-Chattahooche

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29

Cherian, Ribu, Chandrasekhar Venkataraman, Johannes Quaas, and Srinivasan Ramachandran. "GCM simulations of anthropogenic aerosol-induced changes in aerosol extinction, atmospheric heating and precipitation over India." Universitätsbibliothek Leipzig, 2015. http://nbn-resolving.de/urn:nbn:de:bsz:15-qucosa-176395.

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The influence of anthropogenic emissions on aerosol distributions and the hydrological cycle are examined with a focus on monsoon precipitation over the Indian subcontinent, during January 2001 to December 2005, using the European Centre for Medium-Range Weather Forecasts-Hamburg (ECHAM5.5) general circulation model extended by the Hamburg Aerosol Module (HAM). The seasonal variability of aerosol optical depth (AOD) retrieved from the MODerate Resolution Imaging Spectroradiometer (MODIS) on board the Terra and Aqua satellite is broadly well simulated (R 0.6–0.85) by the model. The spatial dist

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30

Preiss, Nicolas. "Etude du 210Pb d'origine atmosphérique dans l'air, la neige, les sols et les sédiments : mesures, inventaires et interprétation à l'échelle globale." Phd thesis, Grenoble 1, 1997. http://tel.archives-ouvertes.fr/tel-00765239.

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L'étude présentée ici concerne la répartition du 210Pb atmosphérique à l'échelle globale dans l'environnement. Ce travail débute par une étude expérimentale concernant les mesures de flux de dépôt atmosphérique de 210Pb dans les pluies, les sols et la neige. Une base de données a ensuite été construite en regroupant les mesures effectuées ces quatre dernières décennies. Celle-ci se focalise sur les concentrations de 210Pb dans l'air de surface et sur les flux de dépôt d'origine atmosphérique mesurés aux interfaces atmosphère-surface terrestre (collecteurs artificiels, sols et neige) et eau-séd

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31

Zhang, Feng. "Climate change assessment for the southeastern United States." Diss., Georgia Institute of Technology, 2011. http://hdl.handle.net/1853/45770.

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Water resource planning and management practices in the southeastern United States may be vulnerable to climate change. This vulnerability has not been quantified, and decision makers, although generally concerned, are unable to appreciate the extent of the possible impact of climate change nor formulate and adopt mitigating management strategies. Thus, this dissertation aims to fulfill this need by generating decision worthy data and information using an integrated climate change assessment framework. To begin this work, we develop a new joint variable spatial downscaling technique for stat

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32

Schemann, Vera, Bjorn Stevens, Verena Grützun, and Johannes Quaas. "Scale dependency of total water variance and its implication for cloud parameterizations: Scale dependency of total water variance and its implication for cloudparameterizations." American Meteorological Society, 2013. https://ul.qucosa.de/id/qucosa%3A13462.

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The scale dependency of variance of total water mixing ratio is explored by analyzing data from a general circulation model (GCM), a numerical weather prediction model (NWP), and large-eddy simulations (LESs). For clarification, direct numerical simulation (DNS) data are additionally included, but the focus is placed on defining a general scaling behavior for scales ranging from global down to cloud resolving. For this, appropriate power-law exponents are determined by calculating and approximating the power density spectrum. The large-scale models (GCM and NWP) show a consistent scaling with

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33

Cherian, Ribu, Chandrasekhar Venkataraman, Johannes Quaas, and Srinivasan Ramachandran. "GCM simulations of anthropogenic aerosol-induced changes in aerosol extinction, atmospheric heating and precipitation over India." Wiley, 2013. https://ul.qucosa.de/id/qucosa%3A13437.

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The influence of anthropogenic emissions on aerosol distributions and the hydrological cycle are examined with a focus on monsoon precipitation over the Indian subcontinent, during January 2001 to December 2005, using the European Centre for Medium-Range Weather Forecasts-Hamburg (ECHAM5.5) general circulation model extended by the Hamburg Aerosol Module (HAM). The seasonal variability of aerosol optical depth (AOD) retrieved from the MODerate Resolution Imaging Spectroradiometer (MODIS) on board the Terra and Aqua satellite is broadly well simulated (R 0.6–0.85) by the model. The spatial dist

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34

Baquero, Bernal Astrid. "Interannual climate variability in the tropical Indian Ocean : a study with a hierarchy of coupled general circulation models = Interannuale Klimavariabilität im tropischen Indischen Ozean : eine Untersuchung mit einer Hierarchie von globalen gekoppelten Ozean-Atmosphären-Modellen /." Hamburg : Max-Planck-Institut für Meteorologie, 2004. http://mpimet.mpg.de/de/web/download.php?src=max_erdsystem&file=pdfupload&id=15&filename=BzE_8.pdf.

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35

Cosme, Emmanuel. "Cycle du soufre des moyennes et hautes latitudes Sud dans un modèle de circulation générale atmosphérique." Phd thesis, Université Joseph Fourier (Grenoble), 2002. http://tel.archives-ouvertes.fr/tel-00705168.

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L'objectif de ce travail est de contribuer à la compréhension du cycle atmosphérique du soufre en Antarctique par l'utilisation d'un Modèle de Circulation Générale Atmosphérique (MCGA). Les versions "Antarctique" et "soufre" du MCGA LMD-ZT ("Laboratoire de Météorologie Dynamique- Zoom Traceurs") ont été fusionnées pour l'étude à haute résolution Antarctique du cycle du soufre dans les moyennes et hautes latitudes Sud. Une méthode de forçage "latéral" de la circulation atmosphérique antarctique par des analyses du Centre Européen de Prévision Météorologique à Moyen Terme (CEPMMT) a été spécifiq

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36

Hamdad, Hichem. "Recherche d'une description optimum des sources et systèmes vibroacoustiques pour la simulation du bruit de passage des véhicules automobiles." Thesis, Le Mans, 2018. http://www.theses.fr/2018LEMA1032/document.

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Pour commercialiser un véhicule, les constructeurs automobiles doivent se soumettre à la réglementation sur le bruit extérieur. Le règlement de la commission économique pour l'Europe, ECE R51.03, spécifie les niveaux admissibles que peut rayonner un véhicule automobile en roulage. Ce règlement est entré en vigueur depuis le 1er juillet 2016 pour remplacer l'ancien règlement ECE R51.02 (changement de méthode d’essai et sévérisation des niveaux de bruit admissibles). La diminution drastique des niveaux sonores tolérés se fait en trois étapes : passage de 74 dB (A) sous l'ancien règlement, à 68 d

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37

Kehoe, Ryan M. "Characteristic errors in 120-H tropical cyclone track forecasts in the western North Pacific." Thesis, Monterey, Calif. : Springfield, Va. : Naval Postgraduate School ; Available from National Technical Information Service, 2005. http://handle.dtic.mil/100.2/ADA432822.

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38

Pelteku, Altin E. "Development of an electromagnetic glottal waveform sensor for applications in high acoustic noise environments." Link to electronic thesis, 2004. http://www.wpi.edu/Pubs/ETD/Available/etd-0114104-142855/.

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Thesis (M.S.)--Worcester Polytechnic Institute.<br>Keywords: basis functions; perfectly matched layers; PML; neck model; parallel plate resonator; finite element; circulator; glottal waveform; multi-transmission line; dielectric properties of human tissues; radiation currents; weighted residuals; non-acoustic sensor. Includes bibliographical references (p. 104-107).

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39

Stachnik, Justin Paul. "Observed Characteristics of Clouds and Precipitating Systems Associated with the Tropical Circulation in Global Models and Reanalyses." Thesis, 2013. http://hdl.handle.net/1969.1/149356.

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This dissertation presents a series of work related to the representation of the Hadley circulation (HC) in atmospheric reanalyses and general circulation models (GCMs), with connections to the underlying tropical and subtropical cloud systems that comprise the mean meridional circulation. An intercomparison of eight atmospheric reanalyses showed that significant variability exists in the mean state for HC intensity, with less variability in HC width. Ensemble trends were broadly consistent with previous work and suggest a strengthening and widening of the tropical circulation over the last 30

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40

O'Brien, Karen Linda. "An evaluation of the uncertainties in using general circulation models to assess the impacts of global warming the case of Mexico /." 1990. http://catalog.hathitrust.org/api/volumes/oclc/23042405.html.

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Thesis (M.S.)--University of Wisconsin--Madison, 1990.<br>Typescript. eContent provider-neutral record in process. Description based on print version record. Includes bibliographical references (leaves 157-162).

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41

Anandhi, Aavudai. "Impact Assessment Of Climate Change On Hydrometeorology Of River Basin For IPCC SRES Scenarios." Thesis, 2007. http://hdl.handle.net/2005/888.

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There is ample growth in scientific evidence about climate change. Since, hydrometeorological processes are sensitive to climate variability and changes, ascertaining the linkages and feedbacks between the climate and the hydrometeorological processes becomes critical for environmental quality, economic development, social well-being etc. As the river basin integrates some of the important systems like ecological and socio-economic systems, the knowledge of plausible implications of climate change on hydrometeorology of a river basin will not only increase the awareness of how the hydrological

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42

Stryhal, Jan. "Využití klasifikací atmosférické cirkulace v interpretaci výstupů z klimatických modelů." Doctoral thesis, 2018. http://www.nusl.cz/ntk/nusl-392475.

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The application of atmospheric circulation classifications in the interpretation of climate model outputs Mgr. Jan Stryhal Automated (computer-assisted) classifications of atmospheric circulation patterns (circulation classifications, for short) constitute a tool widely used in synoptic and dynamic climatology to study atmospheric circulation and its link to various atmospheric, environmental, and societal phenomena. The application of circulation classifications to output of dynamical models of the atmosphere has developed considerably since the pioneering studies about three decades ago, ref

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43

Ngcobo, Simphiwe Innocent. "Projected impacts of climate change on water quality constituents and implications for adaptive management." Thesis, 2013. http://hdl.handle.net/10413/9480.

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The past few decades have seen, amongst other topical environmental issues, increased concerns regarding the imminent threat of global warming and the consequential impacts of climate change on environmental, social and economic systems. Numerous groundbreaking studies conducted independently and cooperatively have provided abundant and conclusive evidence that global climates are changing and that these changes will almost certainly impact natural and socio-economic systems. Increased global change pressures, which include, inter alia, climate change, have increased concerns over the supply o

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Pankine, Alexey Anatolyevich. "Low order model of Martian circulation and interannual variability of global dust storms." Thesis, 2001. https://thesis.library.caltech.edu/4431/3/03part1.pdf.

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<p>The main theme of this work is the development of a simplified model of the martian circulation suitable for conducting computationally fast long term simulations of the martian climate system. In particular, we are looking for causes of the irregular occurrence of the martian global dust storms (GDSs). The low-order model (LOM) is constructed by Galerkin projection of a 2D (zonally averaged) general circulation model (GCM) onto a truncated set of basis functions. The resulting low-order model consists of twelve coupled nonlinear ordinary differential equations (ODEs). The forcing of the mo

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Brix, Holger [Verfasser]. "North Atlantic deep water and antarctic bottom water : their interaction and influence on modes of the global ocean circulation / vorgelegt von Holger Brix." 2001. http://d-nb.info/96315799X/34.

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