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Tesi sul tema "Ocean-atmosphere interaction"

Autore: Grafiati

Pubblicato: 4 giugno 2021

Ultima modifica: 31 luglio 2024

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1

Seo, Hyodae. "Mesoscale coupled ocean-atmosphere interaction". Diss., Connect to a 24 p. preview or request complete full text in PDF format. Access restricted to UC campuses, 2007. http://wwwlib.umi.com/cr/ucsd/fullcit?p3263355.

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Abstract (sommario):

Thesis (Ph. D.)--University of California, San Diego, 2007.
Title from first page of PDF file (viewed July 10, 2007). Available via ProQuest Digital Dissertations. Vita. Includes bibliographical references (p. 138-152).

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2

Zhang, Yuan. "An observational study of atmosphere-ocean interactions in the northern oceans on interannual and interdecadal time-scale /". Thesis, Connect to this title online; UW restricted, 1996. http://hdl.handle.net/1773/10038.

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3

Helber, Robert William. "Upper ocean upwelling, temperature, and zonal momentum analyses in the western equatorail [sic] Pacific". [Tampa, Fla. : s.n.], 2003. http://purl.fcla.edu/fcla/etd/SFE0000073.

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4

Weinstein, Sarah Elizabeth. "Sources, transport, and fates of particulate trace metals in the Gulf of Maine-Scotian Shelf and Labrador Sea /". View online ; access limited to URI, 2003. http://0-wwwlib.umi.com.helin.uri.edu/dissertations/dlnow/3115641.

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5

Kern, Bastian [Verfasser]. "Chemical interaction between ocean and atmosphere / Bastian Kern". Mainz : Universitätsbibliothek Mainz, 2014. http://d-nb.info/1060212412/34.

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6

Kochanski, Adam. "On the practical applications of atmosphere-ocean and atmosphere-wave coupling in mesoscale numerical modeling". abstract and full text PDF (UNR users only), 2008. 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:3316369.

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7

Eichelberger, Scott James. "The effects of meridional heating gradients on the atmospheric general circulation and its variability /". Thesis, Connect to this title online; UW restricted, 2005. http://hdl.handle.net/1773/10029.

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8

施錦杯 e Kam-pui Sze. "Effects of the interaction of atmosphere and ocean on humanactivities". Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 1999. http://hub.hku.hk/bib/B31254378.

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9

Mosedale, Timothy James. "North Atlantic Ocean-atmosphere interaction using simple and complex models". Thesis, University of Reading, 2004. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.430918.

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10

Guo, Larsén Xiaoli. "Air-sea exchange of momentum and sensible heat over the Baltic Sea /". Uppsala : Acta Universitatis Upsaliensis : Univ.-bibl. [distributör], 2003. http://publications.uu.se/theses/91-554-5565-4/.

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11

Chen, Chi-Shao. "Equatorial entrainment zone simulations". Thesis, Monterey, California : Naval Postgraduate School, 1990. http://handle.dtic.mil/100.2/ADA237234.

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Abstract (sommario):

Thesis (M.S. in Physical Oceanography)--Naval Postgraduate School, June 1990.
Thesis Advisor(s): Garwood, Roland W. Second Reader: Chu, Pecheng. "June 1990." Description based on signature page as viewed on October 19, 2009. DTIC Identifier(s): Air water interactions, ocean models, ocean currents, entrainment, ocean circulation, heat flux, wind velocity, mathematical prediction, equatorial regions, theses. Author(s) subject terms: Air-sea interaction, equatorial circulation. Includes bibliographical references (p. 73-75). Also available in print.

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12

Walker, Nan Delene. "Sea surface temperature-rainfall relationships and associated ocean-atmosphere coupling mechanisms in the southern African region". Doctoral thesis, University of Cape Town, 1989. http://catalog.hathitrust.org/api/volumes/oclc/32830668.html.

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13

Davidson, Fraser. "Wind driven circulation in Trinity and Conception Bays /". Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1999. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape9/PQDD_0020/NQ47495.pdf.

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14

Kiss, Andrew Elek. "Dynamics of laboratory models of the wind-driven ocean circulation". View thesis entry in Australian Digital Theses Program, 2000. http://thesis.anu.edu.au/public/adt-ANU20011018.115707/index.html.

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15

Li, Hui. "Numerical modeling of South China Sea circulation /". View abstract or full-text, 2005. http://library.ust.hk/cgi/db/thesis.pl?AMCE%202005%20LI.

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16

Xing, Zeda. "The response of a simple model atmosphere to sea surface temperature anomalies in the North Pacific". Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1997. http://www.collectionscanada.ca/obj/s4/f2/dsk2/ftp01/MQ37178.pdf.

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17

Nelkien, Haim. "Thermally driven circulation". Woods Hole, Mass. : Woods Hole Oceanographic Institution, 1987. http://hdl.handle.net/1912/3152.

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Abstract (sommario):

Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric and Planetary Sciences, and (Ph. D.)--Woods Hole Oceanographic Institution, 1987.
Cover title. Includes bibliographical references (leaves 181-186).

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18

Zappa, Christopher Joseph. "Microscale wave breaking and its effect on air-water gas transfer using infrared imagery /". Thesis, Connect to this title online; UW restricted, 1999. http://hdl.handle.net/1773/10184.

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19

Wang, Weimin. "The seasonal-interannual surface layer heat balance in the equatorial Pacific Ocean /". Thesis, Connect to this title online; UW restricted, 2000. http://hdl.handle.net/1773/11047.

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20

Dong, Shenfu. "Interannual variations in upper ocean heat content and heat transport convergence in the western North Atlantic /". Thesis, Connect to this title online; UW restricted, 2004. http://hdl.handle.net/1773/11021.

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21

Semedo, Alvaro. "Atmosphere-ocean Interactions in Swell Dominated Wave Fields". Doctoral thesis, Uppsala universitet, Geovetenskapliga sektionen, 2010. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-130650.

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Ocean wind waves represent the atmosphere-ocean boundary, playing a central role in the air-sea exchanging processes. Heat, mass and momentum are transferred across this boundary, with waves mediating the exchange of principally the momentum between the winds and the ocean surface. During the generation process waves are called wind sea. When they leave their generation area or outrun their generating wind they are called swell. The wave field can be said to be dominated either by wind sea or swell. Depending on the wave regime the momentum and energy exchanging processes and the degree of coupling between the waves and the wind is different. During the growing process, waves act as a drag on the surface wind and the momentum flux is directed downward. When swell dominates the wave field a reverse momentum flux mechanism occurs triggered by swell waves traveling considerably faster than the surface winds. The momentum transfer is now directed from the waves to the atmosphere, and takes place because swell waves perform work on the atmosphere as part of their attenuation process. This upward momentum transfer has an impact on the lower atmosphere dynamics, and on the overall turbulence structure of the boundary layer. A detailed qualitative climatology of the global wind sea and swell fields from wave reanalysis data, is presented, revealing a very strong swell dominance of the World Ocean. The areas of larger potential impact of swell on the atmosphere, from a climatological point of view, are also studied. A model that reproduces the swell impact on the lower atmosphere dynamics, conceptually based on the energy transfer from the waves to the atmosphere, is presented – a new parameterization for the wave-induced stress is also proposed. The model results are compared with field observations. A modeling simulation, using a coupled wave-atmosphere model system, is used to study the impact of swell in a regional climate model, by using different formulations on how to introduce the wave state effect in the modeling system.
Gränsen mellan hav och atmosfär beskrivs av vågor, dessa spelar en central roll i utbytesprocesser mellan hav och atmosfär. Värme, massa och rörelsemängd överförs vid ytan och utbytet av rörelsemängd mellan vind och havsyta styrs i stor utsträckning av vågorna. Då vågor skapas kallas de för vinddrivna vågor. När vågorna sedan lämnar området där de genererats eller rör sig fortare än den vind som genererat dem kallas de dyning. Ett vågfält kan sägas vara dominerat av antingen vinddrivna vågor eller dyningsvågor. Beroende på vilken vågregim som råder så är kopplingen mellan vågor och vind olika och därmed också utbytesprocesserna för rörelsemängd och energi. Då vågorna genereras fungerar de som en bromsande kraft för vinden och impulsutbytet är nedåtriktat. När dyning dominerar vågfältet inträffar en mekanism för omvänt impulsutbyte som sätts igång av dyningsvågor som färdas avsevärt snabbare än vinden. Rörelsemängd överförs då från vågorna till atmosfären, eftersom dyningsvågorna utför arbete på atmosfären då de dämpas. Den uppåtriktade transporten av rörelsemängd har en stor effekt på dynamiken och turbulensstrukturen i lägre delen av atmosfären. En detaljerad kvalitativ klimatologi av globala vågfält (vinddrivna och dyning) från återanalysdata presenteras och visar att dyning dominerar vågfältet på världshaven. Områden där man kan förvänta sig störst effekt av dyning på atmosfären har identifierats. En konceptuellt baserad modell som reproducerar effekten av dyning på dynamiken i lägre delen av atmosfären presenteras. Modellen styrs av överföring av energi från vågor till atmosfären. I modellen föreslås även en ny parameterisering för våginducerad kraft på havsytan. Modellresultaten är utvärderade mot fältmätningar. En regional klimatmodell, med ett kopplat våg-atmosfärssystem, har använts för att studera den långtida effekten av dyning vid klimatsimulering. Olika formuleringar för beskrivningen av vågornas effekt på atmosfären har använts, beroende på om vinddrivna vågor eller dyning dominerar vågfältet.

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22

Abel, Rafael [Verfasser]. "Aspects of air-sea interaction in atmosphere-ocean models / Rafael Abel". Kiel : Universitätsbibliothek Kiel, 2018. http://d-nb.info/1171800193/34.

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23

Sze, Kam-pui. "Effects of the interaction of atmosphere and ocean on human activities /". Hong Kong : University of Hong Kong, 1999. http://sunzi.lib.hku.hk/hkuto/record.jsp?B21301414.

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24

Scott, Nicholas Vicente. "Observations of the wind-wave spectrum and steep wave statistics in open ocean waters". View online ; access limited to URI, 2003. http://0-wwwlib.umi.com.helin.uri.edu/dissertations/dlnow/3103724.

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25

Lorenz, David Joseph. "Wave-mean-flow interaction and the annular mode /". Thesis, Connect to this title online; UW restricted, 2003. http://hdl.handle.net/1773/10036.

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26

Dawe, Jordan Tyler. "Aspects of modeling the North Pacific Ocean /". Thesis, Connect to this title online; UW restricted, 2006. http://hdl.handle.net/1773/11015.

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Abstract (sommario):

Thesis (Ph. D.)--University of Washington, 2006.
Vita. "A dissertation submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy." Includes bibliographical references (leaves 94-101).

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27

Back, Larissa. "Towards an improved understanding of deep convection patterns over the tropical oceans /". Thesis, Connect to this title online; UW restricted, 2007. http://hdl.handle.net/1773/10062.

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28

Fan, Yalin. "Effects of surface waves on air-sea momentum and energy fluxes and ocean response to hurricanes /". View online ; access limited to URI, 2007. http://0-digitalcommons.uri.edu.helin.uri.edu/dissertations/AAI3276981.

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29

Porter, Marie. "Linking of the surface North Atlantic Ocean to adjacent terrestrial ice masses". Thesis, University of Aberdeen, 2013. http://digitool.abdn.ac.uk:80/webclient/DeliveryManager?pid=195922.

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30

Bell, Michael M. "Air-sea enthalpy and momentum exchange at major hurricane wind speeds". Monterey, Calif. : Naval Postgraduate School, 2010. http://edocs.nps.edu/npspubs/scholarly/dissert/2010/Jun/10Jun%5FBell%5FPhD.pdf.

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Abstract (sommario):

Dissertation (Ph.D. in Meteorology)--Naval Postgraduate School, June 2010.
Dissertation supervisor: Montgomery, Michael. "June 2010." Description based on title screen as viewed on July 14, 2010. Author(s) subject terms: Air-sea interaction, tropical cyclones, surface fluxes, drag coefficient, CBLAST. Includes bibliographical references (p. 125-131). Also available in print.

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31

Våge, Kjetil. "Winter mixed-layer development in the central Irminger Sea : the effect of strong, intermittent wind events /". Online version of original thesis, 2006. http://hdl.handle.net/1912/1775.

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Abstract (sommario):

Thesis (M.S.)--Joint Program in Oceanography/ Applied Ocean Science and Engineering, Massachusetts Institute of Technology and the Woods Hole Oceanographic Institution, 2006.
"September 2006." Bibliography: p. 74-79.

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32

Pezzi, Luciano Ponzi. "Equatorial Pacific dynamics : lateral mixing and tropical instability waves". Thesis, University of Southampton, 2003. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.274585.

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33

Hunter, Thaddaeus M. "Oceanic-atmospheric variability and western United States snowfall". Laramie, Wyo. : University of Wyoming, 2007. http://proquest.umi.com/pqdweb?did=1404342651&sid=1&Fmt=2&clientId=18949&RQT=309&VName=PQD.

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34

Soukup, Tyrel L. "Long lead-time streamflow forecasting of the North Platte River incorporating oceanic-atmospheric climate variability". Laramie, Wyo. : University of Wyoming, 2008. http://proquest.umi.com/pqdweb?did=1594486091&sid=3&Fmt=2&clientId=18949&RQT=309&VName=PQD.

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35

Chen, Jianli. "Geodynamical interconnections between the atmosphere, ocean, hydrosphere, cryosphere, and solid earth /". Digital version accessible at:, 1998. http://wwwlib.umi.com/cr/utexas/main.

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36

Wanamaker, Alan D. "A Late Holocene Reconstruction of Ocean Climate Variability in the Gulf of Maine, USA, Based on Calibrated Isotope Records and Growth Histories from the Long-lived Ocean Quahog (Arctica islandica L.)". Fogler Library, University of Maine, 2007. http://www.library.umaine.edu/theses/pdf/WanamakerAD2007.pdf.

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37

Brainerd, Keith. "Upper ocean turbulence, mixing, and stratification /". Thesis, Connect to this title online; UW restricted, 1995. http://hdl.handle.net/1773/11007.

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38

Zhuang, Haixiong School of Mathematics UNSW. "Parameterisation of atmosphere-ocean surface interactions, with applications to the Australian monsoon". Awarded by:University of New South Wales. School of Mathematics, 2004. http://handle.unsw.edu.au/1959.4/26170.

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Atmosphere-ocean and atmosphere-land interactions are important processes which determine the development of monsoon systems. In this study, a new atmosphere-ocean surface interaction scheme, referred to as AOSIS, is developed and verified with observed data. AOSIS, together with ALSIS (Atmosphere-Land Surface Interaction Scheme), is then coupled into CEMSYS4 (Computational Environmental Modelling System) to investigate the influences of atmosphere-ocean and atmosphere-land surface interactions on the Australian Monsoon, especially the monsoon onset, break and withdrawal. Numerical experiments are carried out and the simulations are compared with the NCEP (National Center for Environmental Prediction, America) data. AOSIS is constructed with three basic components, i.e., a two-layer ocean temperature model, a wind-wave model and a surface flux model. We divide the ocean into a mixed layer and a deep layer. However, the depth of the mixed layer is not constant but varies with time, depending on surface wind shear and buoyancy flux. In AOSIS, we adapted the approach of relating the stages of wave development by wave age and proposed a new expression for calculating the ocean surface roughness length, $z_{0m}$, with consideration of waves. We test AOSIS in a stand along mode against the Moana data and the NCEP data. The comparison with the Moana data shows that AOSIS has considerable skill in simulating SST (sea surface temperature) and energy fluxes, with the simulated values in good agreement with observed data. AOSIS is also successful in simulating the warm and cool effects considered in the COARE (Coupled Ocean-Atmosphere Response Experiment) scheme. Comparison with the NCEP data also confirms that AOSIS simulates SST well. AOSIS and ALSIS are then coupled into CEMSYS4. We apply the system to the simulation of SST and surface energy fluxes over the Australian region and compared the results with the NCEP data. It is found that the simulated SST and energy fluxes are in good agreement with the NCEP data. Further, we study the synoptic events of the Australian Monsoon onset, break and withdrawal and examine the impacts of atmosphere-ocean and atmosphere-land surface interactions on such synoptic events.

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39

Runco, Susan K. "The relationship between marine aerosol optical depth and satellite-sensed sea surface temperature". Thesis, Monterey, Calif. : Naval Postgraduate School, 1986. http://catalog.hathitrust.org/api/volumes/oclc/58046373.html.

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40

Young, Carina Saxton. "Decadal variability of the Pacific subtropical cells and equatorial sea surface temperature". Thesis, Atlanta, Ga. : Georgia Institute of Technology, 2009. http://hdl.handle.net/1853/31671.

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Thesis (M. S.)--Earth and Atmospheric Sciences, Georgia Institute of Technology, 2010.
Committee Chair: Di Lorenzo, Emanuele; Committee Member: Bracco, Annalisa; Committee Member: Lynch-Stieglitz, Jean. Part of the SMARTech Electronic Thesis and Dissertation Collection.

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41

Kessler, William S. "Observations of long Rossby waves in the northern tropical Pacific /". Thesis, Connect to this title online; UW restricted, 1989. http://hdl.handle.net/1773/10971.

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42

Lee, Craig M. "Observations and models of upper ocean response to atmospheric forcing : wind driven flow, surface heating and near-inertial wave interactions with mesoscale currents /". Thesis, Connect to this title online; UW restricted, 1995. http://hdl.handle.net/1773/11039.

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43

Vimont, Daniel J. "The seasonal footprinting mechanism in the CSIRO coupled general circulation models and in observations /". Thesis, Connect to this title online; UW restricted, 2002. http://hdl.handle.net/1773/10074.

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44

Strauhs, Hilbert. "A numerical modeling study for the Japan/East Sea (JES) seasonal circulation and thermohaline structure". Thesis, access online version, 1999. http://handle.dtic.mil/100.2/ADA374405.

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Thesis (M.S.)--Naval Postgraduate School, 1999.
"September, 1999." Includes abstract. DTIC report no.: ADA374405. Includes bibliographical references (p. 75-79). Full text available online from DTIC.

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45

Ismail, Hassan Ebrahiem. "Seasonal variability and the relationship between dissolved inorganic nutrients and selected environmental parameters inshore and offshore of St. Helena Bay". Thesis, Cape Peninsula University of Technology, 2017. http://hdl.handle.net/20.500.11838/2550.

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Thesis (MTech (Chemistry))--Cape Peninsula University of Technology, 2017.
The purpose of the present study was to apply data collected monthly over a 6-year period along the almost 200 km long St. Helena Bay Monitoring Line in the Southern Benguela upwelling system to investigate co-variation between an upwelling index calculated from nearby wind records and physical and chemical properties along the transect. The extent to which the well-documented seasonal upwelling cycles is manifested at the surface along an inshore-offshore variation was investigated in the context of implications for the validity of remote sensing as a monitoring tool in this ocean area and to improve understanding of the physical drivers of biological processes in St. Helena Bay. This study shows that surface temperature and nutrient concentrations exhibit very poor seasonality and weak correlation with the upwelling index. This is, despite clear evidence for spatial inshore-offshore gradients in temperature, nutrients, and chlorophyll-a, consistent with an upwelling regime. The upper ocean temperature gradient shows a much better correspondence to the upwelling index but at the same time demonstrates that surface heating, and not vertical mixing related to upwelling, controls the upper ocean temperature gradient. In this study linear lagged correlations were also examined and discussed to gain insight into the effect upwelling has on the surface waters in St. Helena Bay with the view of determining the following: (1) Does upwelling lead to an increase or decrease of the water properties? (2) What is the characteristic lag between an upwelling event and its effect on these water properties? (3) Is the effect and/or lag different for the different seasons? and (4) Is the effect and/or lag different for stations inside the bay and those outside the bay?. A combination of surface turbulent cooling through upwelling occurred after a lag of 8 to 10 days in winter and early summer, but less than half in late summer, similar to results obtained with salinity. However, the rest of the salinity results fit in poorly with the temperature results. The only significant correlation obtained with the inshore stations during late summer is the inexplicable positive correlation at a lag of 7 days. For all three seasons virtually none of the oxygen results fit the expected pattern. All three nutrients showed a more positive correlation coefficient and significance than the negative ones. Significant negative correlations occurred mainly during late summer at lags of 7 to 9 days caused by planktonic depletion of nutrients. Also, in this season, significant positive correlations between south-north wind and nutrients only occurred at short lags. This observation supports the earlier temperature-based conclusion that the influence of upwelling develops most rapidly at this time of the year. A rapid increase in chlorophyll-a levels followed by nutrient enrichment of the surface layers are evident. iii The results suggest that remote sensing techniques would be inadequate tools to monitor upwelling events in the Southern Benguela. Secondly, the incidence of phytoplankton blooms is more likely triggered by stratified conditions associated with surface heating than relaxation of upwelling winds. Finally, these results also emphasise the importance of validating lagged outputs against real-time measurements in supporting a simpler hydrological model in narrowing down these significant uncertainties.

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46

Burton, Kenneth R. "Influence of Antarctic oscillation on intraseasonal variability of large-scale circulations over the Western North Pacific /". Monterey, Calif. : Springfield, Va. : Naval Postgraduate School ; Available from National Technical Information Service, 2005. http://library.nps.navy.mil/uhtbin/hyperion/05Mar%5FBurton.pdf.

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47

Gong, Xiaofeng. "Recent interdecadal variations in the tropical atmosphere : evidence and idealized GCM simulations /". Full-text version available from OU Domain via ProQuest Digital Dissertations, 1998.

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48

Dima, Ioana M. "An observational study of the tropical tropospheric circulation /". Thesis, Connect to this title online; UW restricted, 2005. http://hdl.handle.net/1773/10093.

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49

Leifer, Ira. "A validation study of bubble mediated air-sea gas transfer modeling". Diss., Georgia Institute of Technology, 1995. http://hdl.handle.net/1853/25774.

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50

Wang, Jinbo. "On the warm bias along the South-West African Coast in coupled models : an oceanic perspective /". Online version of original thesis, 2008. http://hdl.handle.net/1912/2502.

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