Relevant bibliographies by topics / Ocean general circulation

Academic literature on the topic 'Ocean general circulation'

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Published: 4 June 2021
Last updated: 19 February 2022

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Journal articles on the topic "Ocean general circulation"

1

Barron, Eric J., and William H. Peterson. "The Cenozoic ocean circulation based on ocean General Circulation Model results." Palaeogeography, Palaeoclimatology, Palaeoecology 83, no. 1-3 (February 1991): 1–28. http://dx.doi.org/10.1016/0031-0182(91)90073-z.

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Klinck, John M. "General Circulation of the Ocean." Eos, Transactions American Geophysical Union 68, no. 27 (1987): 621. http://dx.doi.org/10.1029/eo068i027p00621-02.

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Smith, R. D., J. K. Dukowicz, and R. C. Malone. "Parallel ocean general circulation modeling." Physica D: Nonlinear Phenomena 60, no. 1-4 (November 1992): 38–61. http://dx.doi.org/10.1016/0167-2789(92)90225-c.

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Smith, Robin S., Clotilde Dubois, and Jochem Marotzke. "Global Climate and Ocean Circulation on an Aquaplanet Ocean–Atmosphere General Circulation Model." Journal of Climate 19, no. 18 (September 15, 2006): 4719–37. http://dx.doi.org/10.1175/jcli3874.1.

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Abstract A low-resolution coupled ocean–atmosphere general circulation model (OAGCM) is used to study the characteristics of the large-scale ocean circulation and its climatic impacts in a series of global coupled aquaplanet experiments. Three configurations, designed to produce fundamentally different ocean circulation regimes, are considered. The first has no obstruction to zonal flow, the second contains a low barrier that blocks zonal flow in the ocean at all latitudes, creating a single enclosed basin, while the third contains a gap in the barrier to allow circumglobal flow at high southern latitudes. Warm greenhouse climates with a global average air surface temperature of around 27°C result in all cases. Equator-to-pole temperature gradients are shallower than that of a current climate simulation. While changes in the land configuration cause regional changes in temperature, winds, and rainfall, heat transports within the system are little affected. Inhibition of all ocean transport on the aquaplanet leads to a reduction in global mean surface temperature of 8°C, along with a sharpening of the meridional temperature gradient. This results from a reduction in global atmospheric water vapor content and an increase in tropical albedo, both of which act to reduce global surface temperatures. Fitting a simple radiative model to the atmospheric characteristics of the OAGCM solutions suggests that a simpler atmosphere model, with radiative parameters chosen a priori based on the changing surface configuration, would have produced qualitatively different results. This implies that studies with reduced complexity atmospheres need to be guided by more complex OAGCM results on a case-by-case basis.
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HANAWA, Kimio. "Ocean General Circulation and Climate Change." Journal of Geography (Chigaku Zasshi) 114, no. 3 (2005): 485–95. http://dx.doi.org/10.5026/jgeography.114.3_485.

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Bellucci, A., S. Gualdi, E. Scoccimarro, and A. Navarra. "NAO–ocean circulation interactions in a coupled general circulation model." Climate Dynamics 31, no. 7-8 (April 18, 2008): 759–77. http://dx.doi.org/10.1007/s00382-008-0408-4.

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Apel, John R., Henry D. I. Abarbanel, W. R. Young, and Arnold L. Gordon. "Principles of Ocean Physics and General Circulation of the Ocean." Physics Today 41, no. 7 (July 1988): 71–72. http://dx.doi.org/10.1063/1.2811502.

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Schiller, A., and J. S. Godfrey. "Indian Ocean Intraseasonal Variability in an Ocean General Circulation Model." Journal of Climate 16, no. 1 (January 2003): 21–39. http://dx.doi.org/10.1175/1520-0442(2003)016<0021:ioivia>2.0.co;2.

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Wu, Yang, Xiaoming Zhai, and Zhaomin Wang. "Decadal-Mean Impact of Including Ocean Surface Currents in Bulk Formulas on Surface Air–Sea Fluxes and Ocean General Circulation." Journal of Climate 30, no. 23 (December 2017): 9511–25. http://dx.doi.org/10.1175/jcli-d-17-0001.1.

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The decadal-mean impact of including ocean surface currents in the bulk formulas on surface air–sea fluxes and the ocean general circulation is investigated for the first time using a global eddy-permitting coupled ocean–sea ice model. Although including ocean surface currents in air–sea flux calculations only weakens the surface wind stress by a few percent, it significantly reduces wind power input to both geostrophic and ageostrophic motions, and damps the eddy and mean kinetic energy throughout the water column. Furthermore, the strength of the horizontal gyre circulations and the Atlantic meridional overturning circulation are found to decrease considerably (by 10%–15% and ~13%, respectively). As a result of the weakened ocean general circulation, the maximum northward global ocean heat transport decreases by about 0.2 PW, resulting in a lower sea surface temperature and reduced surface heat loss in the northern North Atlantic. Additional sensitivity model experiments further demonstrate that it is including ocean surface currents in the wind stress calculation that dominates this decadal impact, with including ocean surface currents in the turbulent heat flux calculations making only a minor contribution. These results highlight the importance of properly accounting for ocean surface currents in surface air–sea fluxes in modeling the ocean circulation and climate.
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Yamanaka, Yasuhiro. "Development of Ocean Biogeochemical General Circulation Model." Oceanography in Japan 8, no. 1 (1999): 25–35. http://dx.doi.org/10.5928/kaiyou.8.25.

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Dissertations / Theses on the topic "Ocean general circulation"

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Chechelnitsky, Michael Y. (Michael Yurievich) 1972. "Adaptive error estimation in linearized ocean general circulation models." Thesis, Massachusetts Institute of Technology, 1999. http://hdl.handle.net/1721.1/58516.

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Thesis (Ph. D.)--Joint Program in Physical Oceanography (Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences; and the Woods Hole Oceanographic Institution), 1999.
Includes bibliographical references (p. 206-211).
Data assimilation methods, such as the Kalman filter, are routinely used in oceanography. The statistics of the model and measurement errors need to be specified a priori. In this study we address the problem of estimating model and measurement error statistics from observations. We start by testing the Myers and Tapley (1976, MT) method of adaptive error estimation with low-dimensional models. We then apply the MT method in the North Pacific (5°-60° N, 132°-252° E) to TOPEX/POSEIDON sea level anomaly data, acoustic tomography data from the ATOC project, and the MIT General Circulation Model (GCM). A reduced state linear model that describes large scale internal (baroclinic) error dynamics is used. The MT method, closely related to the maximum likelihood methods of Belanger (1974) and Dee (1995), is shown to be sensitive to the initial guess for the error statistics and the type of observations. It does not provide information about the uncertainty of the estimates nor does it provide information about which structures of the error statistics can be estimated and which cannot. A new off-line approach is developed, the covariance matching approach (CMA), where covariance matrices of model-data residuals are "matched" to their theoretical expectations using familiar least squares methods. This method uses observations directly instead of the innovations sequence and is shown to be related to the MT method and the method of Fu et al. (1993). The CMA is both a powerful diagnostic tool for addressing theoretical questions and an efficient estimator for real data assimilation studies. It can be extended to estimate other statistics of the errors, trends, annual cycles, etc. Twin experiments using the same linearized MIT GCM suggest that altimetric data are ill-suited to the estimation of internal GCM errors, but that such estimates can in theory be obtained using acoustic data. After removal of trends and annual cycles, the low frequency /wavenumber (periods> 2 months, wavelengths> 16°) TOPEX/POSEIDON sea level anomaly is of the order 6 cm2. The GCM explains about 40% of that variance. By covariance matching, it is estimated that 60% of the GCM-TOPEX/POSEIDON residual variance is consistent with the reduced state linear model. The CMA is then applied to TOPEX/POSEIDON sea level anomaly data and a linearization of a global GFDL GCM. The linearization, done in Fukumori et al.(1999), uses two vertical mode, the barotropic and the first baroclinic modes. We show that the CMA method can be used with a global model and a global data set, and that the estimates of the error statistics are robust. We show that the fraction of the GCMTOPEX/ POSEIDON residual variance explained by the model error is larger than that derived in Fukumori et al.(1999) with the method of Fu et al.(1993). Most of the model error is explained by the barotropic mode. However, we find that impact of the change in the error statistics on the data assimilation estimates is very small. This is explained by the large representation error, i.e. the dominance of the mesoscale eddies in the TIP signal, which are not part of the 20 by 10 GCM. Therefore, the impact of the observations on the assimilation is very small even after the adjustment of the error statistics. This work demonstrates that simultaneous estimation of the model and measurement error statistics for data assimilation with global ocean data sets and linearized GCMs is possible. However, the error covariance estimation problem is in general highly underdetermined, much more so than the state estimation problem. In other words there exist a very large number of statistical models that can be made consistent with the available data. Therefore, methods for obtaining quantitative error estimates, powerful though they may be, cannot replace physical insight. Used in the right context, as a tool for guiding the choice of a small number of model error parameters, covariance matching can be a useful addition to the repertory of tools available to oceanographers.
by Michael Y. Chechelnitsky.
Ph.D.
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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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Beare, Matthew Ivor. "The development of a general purpose parallel ocean circulation model." Thesis, University of East Anglia, 1998. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.266748.

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Font, i. Ferré Jordi. "La circulació general a la mar Catalana." Barcelona : Centre de Publicacions, Intercanvi Cientific i Extensio Universitaria, Universitat de Barcelona, 1986. http://catalog.hathitrust.org/api/volumes/oclc/32908084.html.

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Weaver, Anthony T. "On assimilating sea surface temperature data into an ocean general circulation model." Thesis, University of British Columbia, 1990. http://hdl.handle.net/2429/29204.

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The feasibility of sea surface temperature (SST) data improving the performance of an ocean general circulation model (OGCM) is investigated through a series of idealized numerical experiments. The GFDL Bryan-Cox-Semtner primitive equation model is set-up as an eddy resolving, unforced, flat bottomed channel of uniform depth. 'Observed' SST data taken from a reference ocean established in a control run are continuously assimilated into an 'imperfect' model using a simple 'nudging' scheme based on a surface relaxation condition of the form Q = C(SST — T₁) where Q is the heat flux and T₁ is the temperature at the top level of the model. The rate of assimilation is controlled by adjusting the constant inverse relaxation time parameter C. Numerical experiments indicate that the greatest improvement in the model fields is achieved in the extreme case of infinite assimilation (i.e., C = ᅇ) in which the 'observed' SST is directly inserted into the model. This improvement is quantified by monitoring the reduction in the root mean square (RMS) errors relative to the simulated reference ocean. Assimilation with longer relaxation time-scales (i.e., smaller C's) proves quite ineffective in reducing the RMS errors. The improvement in the direct insertion numerical experiment stems from the model's ability to transfer assimilated SST into subsurface information through strong advective processes. The assimilation of cool surface data induces convective overturning which transfers the 'cool' information downward rapidly but adversely affects the vertical thermal structure by an unrealistic deepening of the mixed layer. By contrast, warm surface data do not penetrate downward readily. Thus, the systematically biased downward flux of coolness gradually produces unrealistically cool subsurface waters.
Science, Faculty of
Earth, Ocean and Atmospheric Sciences, Department of
Graduate
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Brown, Catherine Alicia. "Oscillatory behavior in an ocean general circulation model of the North Atlantic." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1999. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape9/PQDD_0004/MQ46006.pdf.

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Dubois, Clotilde. "The role of diapycnal mixing in coupled atmosphere-ocean general circulation models." Thesis, University of Southampton, 2006. https://eprints.soton.ac.uk/63133/.

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The value of ocean diapycnal diffusivity (v) sets the rate at which dense bottom water can be mixed up through the stratified water column and thus plays an important role in the meridional overturning circulation (MOC). Previous idealised experiments and simplified theory suggest that the strength of the MOC and the ocean heat transport scale with the v. This study investigates the dependence of the MOC and other parameters on v using atmosphere-ocean general circulation models (AOGCM). Firstly, the dependence of the MOC strength on v is studied using a low resolution AOGCM with realistic geometry, FORTE, with spatially constant v values ranging from 0.1 cm2/s to an unrealistic high value of 5 cm2/s. At the cyclostationary state, global MOC strength is found to scale with v (in agreement with previous studies) according to a power law of 0.5. No power law is found for the MOC in the individual basins. The increase in MOC strength in the Atlantic and Pacific Oceans is associated with an increase in the ocean heat transport. The atmosphere responds to the change in the ocean state by a decrease of its energy transport and surface winds. Only a partial compensation is found between the ocean and atmosphere energy transport. The strength of v is found to have a strong impact on coupled phenomena, such as a cessation of El Niño at high v. Secondly, similar experiments are conducted with a state-of-the-art AOGCM, ECHAM5/ MPIOM. In this model, v is derived from a constant background diapycnal diffusion (b), wind induced mixing, the Richardson number and the convective adjustment. A set of 3 coupled experiments is conducted, with b = 0.1, 0.25 and 1 cm2/s. The scaling law from simple theory and the previous experiments with FORTE is not observed with this coupled model. At the cyclostationary state, the MOC strength weakens by 16% as b increases from 0.1 to 1 cm2/s. This behavior is not found when the experiments are repeated with an ocean-only model. The reduction in MOC in the coupled model is linked to a strong reduction in the convective mixing at high latitudes. The convective mixing is reduced by a continuous strong freshening in the Arctic region due to an increase in surface air temperature and melting of the sea-ice in the coupled experiments, which is not observed in the ocean-only experiments. The responses of the two coupled models show many similarities as b increases. Both models show convection in the Pacific for high values of b. The main difference is the response of the MOC in the Atlantic is linked to the different locations of the deep convection and their relative changes in the models. I conclude that the diapycnal mixing and the ocean-atmosphere interactions both control the strength of the MOC, and their influences cannot be considered separately.
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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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Weddle, Charles A. OCEAN CURRENTS PACIFIC OCEAN OCEAN MODELS WIND STRESS STRESSES MATHEMATICAL MODELS WIND SENSITIVITY DEPTH CIRCULATION TROPICAL CYCLONES LONGITUDE INSTABILITY CYCLONES AIR WATER INTERACTIONS MIXED LAYER(MARINE) IMAGES METEOROLOGICAL SATELLITES THESES EQUATORIAL REGIONS TEMPERATURE. "The effect of westerly wind bursts on a tropical ocean general circulation model /." Monterey, Calif. : Springfield, Va. : Naval Postgraduate School ; Available from National Technical Information Service, 1993. http://handle.dtic.mil/100.2/ADA276423.

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Thesis (M.S. in Meteorology and M.S. in Physical Oceanography) Naval Postgraduate School, December 1993.
Thesis advisor(s): Murphree, James Thomas ; Garwood, Roland W. "December 1993." Bibliography: p. 115-118. Also available online.
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Weddle, Charles A., and CURRENTS PACIFIC OCEAN OCEAN MODELS WIND STRESS STRESSES MATHEMATICAL MODELS WIND SENSITIVITY DEPTH CIRCULATION TROPICAL CYCLONES LONGITUDE INSTABILITY CYCLONES AIR WATER INTERACTIONS MIXED LAYER(MARINE) IMAGES ME OCEAN. "The effect of westerly wind bursts on a tropical ocean general circulation model." Thesis, Monterey, California. Naval Postgraduate School, 1993. http://hdl.handle.net/10945/26516.

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A primitive equation general circulation model with imbedded mixed layer physics has been used to investigate the response of the equatorial Pacific ocean to daily varying winds and westerly wind bursts. The major issue addressed by this study is the impact of daily varying winds, including westerly wind bursts, in the modeling of the tropical Pacific ocean and El Nino. In the developmental phase, the sensitivity of the model to the integration time step and the domain size were investigated. The results of this work were used to determine the optimal time step and model domain size for the main experimental model runs. In the experimental phase, the model was spun-up using time averaged wind stresses. The model ocean was then exposed to two years of realistic daily varying wind stresses covering the period of 1991 and 1992. The model developed an El Nino like response that corresponded in several respects with observed features of the 1991-92 El Nino. The model also developed tropical instability waves in the eastern Pacific similar to those observed in situ and in satellite SST images. The model's responses to the tropical cyclones that occurred during 1991-92 were also consistent in several ways with observations
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Books on the topic "Ocean general circulation"

1

Abarbanel, Henry D. I. General Circulation of the Ocean. New York, NY: Springer New York, 1987.

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Abarbanel, Henry D. I., and W. R. Young, eds. General Circulation of the Ocean. New York, NY: Springer New York, 1987. http://dx.doi.org/10.1007/978-1-4612-4636-7.

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Chechelnitsky, Michael Y. Adaptive error estimation in linearized ocean general circulation models. Cambridge, Mass: Massachusetts Institute of Technology, 1999.

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Oberhuber, Josef M. Simulation of the Atlantic circulation with a coupled sea ice-mixed layer-isopycnal general circulation model. Hamburg, Germany: Max-Planck-Institut fuer Meteorologie, 1990.

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Chou, Ru Ling. Derivation of revised formulae for eddy viscous forces used in the ocean general circulation model. [Washington, DC]: National Aeronautics and Space Administration, Scientific and Technical Information Division, 1989.

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Chou, Ru Ling. Derivation of revised formulae for eddy viscous forces used in the ocean general circulation model. New York, NY: Goddard Institute for Space Studies, 1988.

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Summer Study Program in Geophysical Fluid Dynamics (1989 Woods Hole Oceanographic Institution). General circulation of the oceans: 1989 Summer Study Program in Geophysical Fluid Dynamics. Woods Hole, Mass: Woods Hole Oceanographic Institution, 1989.

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Truckchev, Dimitru Ivanov. The Black Sea general circulation and climatic temperature and salinity fields. Woods Hole, MA: Woods Hole Oceanographic Institution, 1992.

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Brown, Catherine Alicia. Oscillatory behavior in an ocean general circulation model of the North Atlantic. Ottawa: National Library of Canada, 1999.

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Weddle, Charles A. The effect of westerly wind bursts on a tropical ocean general circulation model. Monterey, Calif: Naval Postgraduate School, 1993.

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Book chapters on the topic "Ocean general circulation"

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McWilliams, James C. "Oceanic General Circulation Models." In Ocean Modeling and Parameterization, 1–44. Dordrecht: Springer Netherlands, 1998. http://dx.doi.org/10.1007/978-94-011-5096-5_1.

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Özsoy, Emin. "Elements of Ocean General Circulation." In Geophysical Fluid Dynamics I, 193–220. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-16973-2_8.

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Veronis, G. "Inverse Methods for Ocean Circulation." In General Circulation of the Ocean, 102–33. New York, NY: Springer New York, 1987. http://dx.doi.org/10.1007/978-1-4612-4636-7_3.

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Mitchell, John F. B. "General Circulation Modelling of the Atmosphere." In Climate-Ocean Interaction, 67–86. Dordrecht: Springer Netherlands, 1990. http://dx.doi.org/10.1007/978-94-009-2093-4_4.

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Yoon, Jin-Ho, and Po-Lun Ma. "Oceanic General Circulation Models ocean/oceanic general circulation models (OGCM)." In Encyclopedia of Sustainability Science and Technology, 7365–81. New York, NY: Springer New York, 2012. http://dx.doi.org/10.1007/978-1-4419-0851-3_356.

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Young, W. R. "Baroclinic Theories of the Wind Driven Circulation." In General Circulation of the Ocean, 134–201. New York, NY: Springer New York, 1987. http://dx.doi.org/10.1007/978-1-4612-4636-7_4.

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Hendershott, M. C. "Single Layer Models of the General Circulation." In General Circulation of the Ocean, 202–67. New York, NY: Springer New York, 1987. http://dx.doi.org/10.1007/978-1-4612-4636-7_5.

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Pedlosky, Joseph. "Thermocline Theories." In General Circulation of the Ocean, 55–101. New York, NY: Springer New York, 1987. http://dx.doi.org/10.1007/978-1-4612-4636-7_2.

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Niiler, P. P. "The Observational Basis for Large Scale Circulation." In General Circulation of the Ocean, 1–54. New York, NY: Springer New York, 1987. http://dx.doi.org/10.1007/978-1-4612-4636-7_1.

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Monin, A. S. "General Circulation of the Atmosphere and Ocean." In Theoretical Geophysical Fluid Dynamics, 279–311. Dordrecht: Springer Netherlands, 1990. http://dx.doi.org/10.1007/978-94-009-1880-1_8.

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Conference papers on the topic "Ocean general circulation"

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Wang, Ping, Daniel S. Katz, and Yi Chao. "Optimization of a parallel ocean general circulation model." In the 1997 ACM/IEEE conference. New York, New York, USA: ACM Press, 1997. http://dx.doi.org/10.1145/509593.509618.

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Andrich, P., and G. Madec. "Performance evaluation for an ocean general circulation model: vectorization andmultitasking." In the 2nd international conference. New York, New York, USA: ACM Press, 1988. http://dx.doi.org/10.1145/55364.55393.

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Masuda, Yoshio, and Yasuhiro Yamanaka. "Simulation of 50 Mton CO2 injection per year into the ocean using an ocean general circulation model." In OCEANS 2008 - MTS/IEEE Kobe Techno-Ocean. IEEE, 2008. http://dx.doi.org/10.1109/oceanskobe.2008.4531030.

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TANAKA, Y., M. TSUGAWA, Y. MIMURA, and T. SUZUKI. "DEVELOPMENT OF PARALLEL OCEAN GENERAL CIRCULATION MODELS ON THE EARTH SIMULATOR." In Proceedings of the Tenth ECMWF Workshop on the Use of High Performance Computers in Meteorology. WORLD SCIENTIFIC, 2003. http://dx.doi.org/10.1142/9789812704832_0005.

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Agarwal, Neeraj, Rashmi Sharma, Sujit Basu, and Vijay K. Agarwal. "Impact of Argo data assimilation in an ocean general circulation model." In Asia-Pacific Remote Sensing Symposium, edited by Tiruvalam N. Krishnamurti, B. N. Goswami, and Toshiki Iwasaki. SPIE, 2006. http://dx.doi.org/10.1117/12.693674.

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Zhu, Rui, Wei Zhao, and Dexun Chen. "The Application of the SIMD Optimization in Ocean General Circulation Model POP." In 2012 International Conference on Computer Science and Service System (CSSS). IEEE, 2012. http://dx.doi.org/10.1109/csss.2012.437.

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Denisova, Nina Y., Konstantin G. Gribanov, and Martin Werner. "Verification of the isotopic atmospheric general circulation model for a monitoring station in Labytnangi." In 26th International Symposium on Atmospheric and Ocean Optics, Atmospheric Physics, edited by Gennadii G. Matvienko and Oleg A. Romanovskii. SPIE, 2020. http://dx.doi.org/10.1117/12.2575615.

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Masumoto, Yukio, Takashi Kagimoto, Toshio Yamagata, Masahiro Yoshida, Masahiro Fukuda, and Naoki Hirose. "Simulated circulation in the Indonesian archipelago from a high resolution global ocean general circulation model on the numerical wind tunnel." In the 1999 ACM/IEEE conference. New York, New York, USA: ACM Press, 1999. http://dx.doi.org/10.1145/331532.331567.

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Dick, S., and E. Kleine. "The BSH's new operational circulation model using general vertical co-ordinates." In 2006 IEEE US/EU Baltic International Symposium on Integrated Ocean Observation Syst. for Managing Global & Regional Ecosys.Marine Resch. IEEE, 2006. http://dx.doi.org/10.1109/baltic.2006.7266135.

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Anderson, Thomas R., and Michael J. Follows. "Representing Plankton Functional Types in Ocean General Circulation Models: Competition, Tradeoffs and Self-Organizing Architecture." In 2010 15th IEEE International Conference on Engineering of Complex Computer Systems (ICECCS). IEEE, 2010. http://dx.doi.org/10.1109/iceccs.2010.49.

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Reports on the topic "Ocean general circulation"

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Harrison, Walter A. Effects of Bottom Topography on Ocean General Circulation. Fort Belvoir, VA: Defense Technical Information Center, June 1992. http://dx.doi.org/10.21236/ada253121.

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Wickett, Michael Everett. A Reduced Grid Method for a Parallel Global Ocean General Circulation Model. Office of Scientific and Technical Information (OSTI), December 1999. http://dx.doi.org/10.2172/791655.

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Zhang, Jiaxu, Wilbert Weijer, Mathew Einar Maltrud, Carmela Veneziani, Nicole Jeffery, Elizabeth Clare Hunke, Jorge Rolando Urrego Blanco, and Jonathan David Wolfe. An eddy-permitting ocean-sea ice general circulation model (E3SMv0-HiLAT03): Description and evaluation. Office of Scientific and Technical Information (OSTI), July 2019. http://dx.doi.org/10.2172/1542803.

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Broecker, W. S. Geochemical constraints on ocean general circulation models. Final report, May 1, 1995--April 30, 1997. Office of Scientific and Technical Information (OSTI), May 1998. http://dx.doi.org/10.2172/666234.

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Barnett, T. P. Studies of Ocean Predictability at Decade to Century Time Scales Using a Global Ocean General Circulation Model in a Parallel Computing Environment. Office of Scientific and Technical Information (OSTI), November 1998. http://dx.doi.org/10.2172/761901.

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Gates, W., and K. Sperber. Temporal behavior of tropical Pacific SST (supersonic transport) in the OSU (Oregon State University) coupled atmosphere: Upper ocean GCM (general circulation models). Office of Scientific and Technical Information (OSTI), February 1990. http://dx.doi.org/10.2172/7106559.

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Barnett, Tim P. Final Report: Studies of Ocean Predictability at Decade to Century Time Scales Using a Global Ocean General Circulation Model in a Parallel Computing Environment (August 7, 1991-November 30, 1998). Office of Scientific and Technical Information (OSTI), November 1998. http://dx.doi.org/10.2172/755811.

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[Studies of ocean predictability at decade to century time scales using a global ocean general circulation model in a parallel competing environment]. Progress report. Office of Scientific and Technical Information (OSTI), March 1992. http://dx.doi.org/10.2172/10169958.

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(Studies of ocean predictability at decade to century time scales using a global ocean general circulation model in a parallel competing environment). [Large Scale Geostrophic Model]. Office of Scientific and Technical Information (OSTI), March 1992. http://dx.doi.org/10.2172/7284605.

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