Estimating the Circulation & Climate of the Ocean
about ecco | products | model | automatic differentiation | news archive | publications | computing
home > publications
+ papers, manuscripts, proceedings



1) Published Papers


* Lee, T. and J. Marotzke, 1997: Inferring meridional mass and heat transportsof the Indian Ocean by fitting a GCM to climatological data. J. Geophys. Res., 102, 10585-10602.
* Marshall, J., A. Adcroft, C. Hill, L. Perelman and C. Heisey, 1997: A finite-volume, incompressible Navier Stokes model for studies of the ocean on parallel computers. J. Geophys. Res., 102, 5753-5766.
* Marshall, J., C. Hill, L. Perelman and A. Adcroft, 1997: Hydrostatic, quasi-hydrostatic, and nonhydrostatic ocean modeling. J. Geophys. Res., 102, 5733-5752.
* Stammer, D., C. Wunsch, R. Giering, Q. Zhang,J. Marotzke, J. Marshall and C.N. Hill, 1997: The global ocean circulation estimated from TOPEX/POSEIDON altimetry and the MIT general circulation model. MIT Center for Global Change Science, Report 49.


* Lee, T., and J. Marotzke, 1998: Seasonal cycle of meridional overturning and heat transport of the Indian Ocean. J. Phys. Oceanogr., 28, 923-943.
* Fukumori, I., R. Raghunath, and L. Fu, 1998. Nature of global large-scale sea level variability in relation to atmospheric forcing: A modeling study, Journal of Geophysical Research, 103, 5493-5512
* Stammer, D., I. Fukumori and C. Wunsch, 1998: Report of a GODAE/WOCE meeting on large-scale ocean state estimation. WOCE IPO Report, 161/98, GODAE Report, 2, 21pp.


* Fukumori, I., R. Raghunath, L. Fu, and Y. Chao, 1999: Assimilation of TOPEX/POSEIDON data into a global ocean circulation model: How good are the results? J. Geophys. Res., 104, 25,647-25,665.
* Hirose, N., I. Fukumori, and J.-H. Yoon, 1999. Assimilation of TOPEX/POSEIDON altimeter data with a reduced gravity model of the Japan Sea, Journal of Oceanography, 55, 53-64.
* Marotzke, J., R. Giering, Q. K. Zhang, D. Stammer, C. N. Hill and T. Lee, 1999: Construction of the adjoint MIT ocean general circulation model and application to Atlantic heat transport sensitivity, J. Geophys. Res., 104, 29,529 - 29,548.
* Zhang, Q. and J. Marotzke, 1999: The importance of open-boundary estimation for an Indian Ocean GCM-data synthesis. J. Mar. Res, 57, 305-334.


* Fukumori, I., 2000. Data Assimilation by Models, in "Satellite Altimetry and Earth Sciences", L.-L. Fu and A. Cazenave, editors, Academic Press, 463pp.
* Lee, T., J.-P. Boulanger, A. Foo, L.-L. Fu, and R. Giering, 2000: Data assimilation by an intermediate coupled ocean-atmosphere model: application to the 1997-1998 El Niño. J. Geophys. Res.,105, 26063-26087.
* McKinley, G. M.J. Follows and J. Marshall, 2000: Interannual variability of oxygen fluxes in the North Atlantic. Geo. Res. Letters., 27, 2933-2936
* Ponte, R., D. Stammer and C. Wunsch, 2000: Improved ocean angular momentum estimates using an ocean model constrained by large-scale data. Geophys. Res. Lett., 28, 1775-1778.
* Stammer, D., 2000: Ocean state estimation in support of CLIVAR and GODAE. CLIVAR Exchanges Newsletter, 17.
* Stammer, D. and E. P.Chassignet, 2000: Ocean state estimation and prediction in support of oceanographic research. Oceanography,13, 51--56.


* Adcroft, A., J.R. Scott and J. Marotzke, 2001: Impact of Geothermal Heating on the Global Ocean Circulation. Geophys. Res. Lett. 28(9), 1735-1738.
* Cheng, B., 2001: Some performance comparisons for an ocean model on the SGI Origin 2000 and the HP V-class 2500. Proceedings of the Cray Users Group Summit 2001, Indian Wells, CA.
* Dushaw, B., G. Bold, C.-S. Chiu, J. Colosi, B. Cornuelle, Y. Desaubies, M. Dzieciuch, A. Forbes, F. Gaillard, A. Gavrilov, J. Gould, B. Howe, M. Lawrence, J. Lynch, D. Menemenlis, J. Mercer, P. Mikhalevsky, W. Munk, I. Nakano, F. Sshott, U. Send R. Spindel, T. Terre, P. Worcester, C. Wunsh (2001). Observing the Ocean in the 2000s: A Strategy for the Role of Acoustic Tomography in Ocean Climate Observation. In Observing the Oceans in the 21st Century, C. J. Koblinsky and N. R. Smith (Eds), GODAE Project Office and Bureau of Meteorology, Melbourne.
* Dutkiewicz, S., Follows, M., Marshall, J and W. Gregg, 2001: Interannual variability in phytoplankton abundances in the North Atlantic. Deep-Sea Res. II, 48, 2323-2344.
* Hirose, N., I. Fukumori, and R. Ponte, 2001. A non-isostatic global sea level response to barometric pressure near 5-days, Geophysical Research Letters, 28, 2441-2444.
* Hirose, N., I. Fukumori, R. Ponte, and V.Zlotnicki, 2001. High-frequency barotropic response to atmospheric disturbances: Sensitivity to forcing, topography, and friction, Journal of Geophysical Research, 106, 30987-30995.
* Kaese, R., A. Biastoch and D. Stammer, 2001: On the mid-depth Circulation in the Labrador and Irminger Seas. Geophys. Res. Lett., 28 , 3433 --
* Scott, J.R., J. Marotzke and A. Adcroft, 2001: Geothermal heating and its influence on the meridional overturning circulation. J. Geophys. Res.-Oceans 106 (C12), 31141-31154.
* Stammer, D., R. Bleck, C. Boning, P. DeMey, H. Hurlburt, I. Fukumori, C. LeProvost, R. Tokmakian, Wenzel, 2001: Global ocean modeling and state estimation in support of climate research. In: Observing the Ocean in the 21st Century, C.J. Koblinsky and N.R. Smith (Eds.), Bureau of Meteorology, Melbourne, Australia, 511--528.
* Talley, L., D. Stammer and I. Fukumori, 2001: Towards a WOCE synthesis. In: Ocean Circulation and Climate, Siedler, G., J. Church and J. Gould (Eds.), Academic Press, 525-546.
* Wunsch, C., 2001: Ocean observations and the climate forecast problem. In: Meteorology at the Millennium. R. P. Pearce (Ed.), 217-224, Academic, London.


* Dickey, J. O., S. L. Marcus, O. de Viron, and I. Fukumori, 2002. Recent Earth oblateness variations: Unraveling climate and postglacial rebound effects, Science, 298, 1975-1977.
* Dongarra, J.J., P.M.A. Sloot and C.J.K. Tan (Eds.),In: Lecture Notes in Computer Science (LNCS), Vol. 2330, pp. 1019-1028, Springer-Verlag.
* Fukumori, I., 2002: A partitioned Kalman filter and smoother. Monthly Weather Review, 130, 1370-1383.
* Heimbach, P., C. Hill and R. Giering, 2002: Automatic Generation of Efficient Adjoint Code for a Parallel Navier-Stokes Solver.
* Lee, T., I. Fukumori, D. Menemenlis, Z. Xing, L.-L. Fu, 2002: Effects of the Indonesian Throughflow on the Pacific and Indian Oceans. J. Phys. Oceanogr., 32, 1404-1429.
* Stammer, D., C. Wunsch, I. Fukumori and J. Marshall, 2002: State Estimation in Modern Oceanographic Research. EOS, Transactions, American Geophysical Union, Volume 83, Nr. 27, p. 289, 294--295.
* Stammer, D., C. Wunsch, R. Giering, C. Eckert, P. Heimbach, J. Marotzke, A. Adcroft, C.N. Hill and J. Marshall, 2002: The global ocean circulation during 1992 --1997, estimated from ocean observations and a general circulation model. J. Geophys. Res., 107, C9 3118, doi:10.1029/2001JC000888.
* Wunsch, C., 2002: Oceanic age and transient tracers, analytical and numerical solutions. J. Geophys. Res., Vol 107, No.C6, 1-16.
* Wunsch, C., 2002: What is the Thermohaline Circulation. , Science, Vol 298, No. 5596, Nov. 8, 2002, p. 1179-1181.


* Biastoch, A., R. Kaese and D. Stammer, 2003: The sensitivity of the Denmark-Scotland Ridge Overflow to forcing changes. J. Phys. Oceanogr., 3, 2307-2319.
* Chao, B. F., A. Y. Au, J. P. Boy and C. M. Cox, 2003: Time-variable gravity signal of an anomalous redistribution of water mass in the extratropic Pacific during 1998-2002, Geochemistry Geophysics Geosystems, 4, doi:10.1029/2003gc000589
* Fieguth, P., D. Menemenlis, and I. Fukumori, 2003. Mapping and pseudo-inverse algorithms for ocean data assimilation, IEEE Transactions on Geoscience and Remote Sensing,41, 43-51.
* Gross, R. S., I. Fukumori, and D. Menemenlis, 2003. Atmospheric and oceanic excitation of the Earth's wobbles during 1980-2000, J. Geophys. Res., 108 (B8), 2370, doi:10.1029/2002JB002143.
* Lee, T. and I. Fukumori, 2003: Interannual to decadal variation of tropical-subtropical exchange in the Pacific Ocean: boundary versus interior pycnocline transports. J. Clim. 16, 4022-4042
* Legg and A. Adcroft, 2003: Internal wave breaking at concave and convex continental slopes. J. Phys. Oceanogr. 33, 2224-2246.
* Li, X., and C. Wunsch (2003), Constraining the North Atlantic circulation between 4.5 S and 39.5 N with transient tracer observations, J. Geophys. Res., 108(C10), 3318, doi:10.1029/2002JC001765.
* Losch, A. Adcroft and J-M. Campin, 2003: How sensitive a Coarse General Circulation Models to Fundamental Approximations in the Equations of Motion? J. Phys. Oceanogr. 34 (1), 306-319S.
* Losch, M. and C. Wunsch, 2003: Bottom topography as a control parameter in an ocean circulation model. J. Atmosph. and Oc. Technology, 1685-1696.
* Stammer, D., C. Wunsch, R. Giering, C. Eckert, P. Heimbach, J. Marotzke, A. Adcroft, C.N. Hill and J. Marshall, 2003: Volume, heat and freshwater transports of the global ocean circulation 1993 --2000, estimated from a general circulation model constrained by World Ocean Circulation Experiment (WOCE) data . J. Geophys. Res., 108, C1 3007, doi:10.1029/2001JC001115.
* Wunsch, C., and D. Stammer, 2003: Global Ocean Data Assimilation and Geoid Measurements , in G. Beutler, R. Rummel, M.R. Drinkwater, and R. von Steiger, Earth Gravity Field from Space - from Sensors to Earth Sciences, Space Sciences Series of ISSI, Vol. 17, and Space Science Reviews, 108, 147-162, 2003.


* Adcroft, A. and J-M. Campin, 2004: Rescaled height coordinates for accurate representation of free-surface flows in ocean circulation models. Accepted by Ocean Modelling.
* Adcroft, A., J-M. Campin, C.N. Hill and J.C. Marshall, 2004: Implementation of an atmosphere-ocean general circulation model on the expanded spherical cube. Mon. Wea. Rev., 132 (12), 2845-2863
* Campin, J-M., A. Adcroft, C. Hill and J. Marshall, 2004: Conservation of properties in a free-surface model. Ocean Modelling. 6, 221-244.
* Dommenget, D. and D. Stammer, 2004: Assessing ENSO Simulations and Predictions Using Adjoint Ocean State Estimation. J. Climate, Vol. 17, No. 22, pages 4301-4315.
* Fukumori, I., T. Lee, B. Cheng, and D. Menemenlis, 2004. The origin, pathway, and destination of Niño3 water estimated by a simulated passive tracer and its adjoint, J. Phys. Oceanogr., 34, 582-604.
* Gross, R. S., I. Fukumori, D. Menemenlis, P. Gegout, 2004. Atmospheric and oceanic excitation of length-of-day variations during 1980-2000, J. Geophys. Res., 109 (B1), art no. B01406.
* Hill, C., V. Bugnion, M. Follows and J. Marshall, 2004: Evaluating carbon sequestration efficiency in an ocean circulation model by adjoint sensitivity analysis. JGR Oceans, vol 109, C11005, doi:10.1029/2002JC001598
* Ito, T., J.C. Marshall and M.J. Follows, 2004: What controls the uptake of transient tracers in the Southern Ocean? Global Biogeochem. Cycles., 18, GB2021, doi:10.1029/2003GB002103
* Kim, S.B., T. Lee, and I. Fukumori, 2004: The 1997-99 abrupt change of the upper ocean temperature in the northcentral Pacific. Geophys. Res. Lett., 31, L22304, doi:10.1029/2004GL021142.
* Köhl, A., and D. Stammer, 2004: Optimal Observations for Variational Data Assimilation . J. Phys. Oceanogr., Volume 34, March 2004, pp. 529-542
* Lee, T., 2004: Decadal weakening of the shallow overturning circulation in the South Indian Ocean. Geophys. Res. Lett., 31, L18305, doi:10.1029/2004GL020884.
* Lee., T., I. Fukumori, B. Tang, 2004: Temperature advection: internal versus external processes. J. Phys. Oceanogr., 34, 1936-1944.
* Li, X. and C. Wunsch, 2004: An adjoint sensitivity study of chlorofluorocarbons in the North Atlantic, J. Geophys. Res., 109, C01007, doi:10.1029/2003JC002014.
* Lu, Y., and D. Stammer, 2004: Vorticity balance in coarse-resolution global ocean simulations . J. Phys. Oceanogr., Volume 34, March 2004, pp. 605-622
* Marshall, J.C., A. Adcroft, J-M. Campin and C. Hill, 2004: Atmosphere-Ocean Modeling exploiting fluid isomorphisms. Mon. Wea. Rev., 132 (12), 2882-2894
* McKinley, G., M.J. Follows and J. Marshall, 2004: Mechanisms of air-sea CO2 flux variability in the Equatorial Pacific and north Atlantic: Global Biogeochemical Cycles, vol 18,doi:10.1029/2003GB002179
* Reddy, P. R. C., P. S. Salvekar, A. A. Deo and D. W. Ganer, 2004: Westward propagating twin gyres in the equatorial Indian Ocean, Geophys Res Lett, 31(1), doi:10.1029/2003gl018615
* Stammer, D., and J. Theiss, 2004: Velocity statistics inferred from the TOPEX/POSEIDON-JASON Tandem Mission Data. Marine Geodesy, 27, 551-576.
* Stammer, D., K. Ueyoshi, A. Köhl, W.B. Large, S. Josey and C. Wunsch, 2004: Estimating air-sea flux estimates through global ocean data assimilation , J. Geophys. Res., 109, C05023, doi:10.1029/2003JC002082.
* Wang, O., I. Fukumori, T. Lee, and B. Cheng, 2004: On the cause of eastern equatorial Pacific Ocean T-S variations associated with El Nino. Geophys. Res. Lett., 31, L15310, doi:10.1029/2004GL02472.
* Wang, O., I. Fukumori, T. Lee, and G. Johnson, 2004. Eastern equatorial Pacific Ocean T-S variations with El Niño, Geophysical Research Letters, 31, L04305, 10.1029/2003GL019087.
* Worcester, P., B. Cornuelle, B. Dushaw, M. Dzieciuch, B. Howe, D. Menemenlis, J. Mercer, W. Munk, R. Spindel, D. Stammer, and M. Zarnetske (2004). Acoustic remote sensing of large-scale temperature variability in the North Pacific Ocean. 68, 576-577.
* Wunsch, C., 2004: Thermohaline Loops, Stommel Box Models, and Sandstroems Theorem, Tellus, 57A, 1-16, 2004
* Zerbini, S., F. Matonti, F. Raicich, B. Richter and T. van Dam, 2004: Observing and assessing nontidal ocean loading using ocean, continuous GPS and gravity data in the Adriatic area, Geophys Res Lett, 31(23), doi:10.1029/2004gl021185


* Davis, R.E., 2005. Intermediate-depth circulation of the Indian and South Pacific Oceans measured by autonomous floats. J. Phys. Oceanogr., 35(5), 683-707, doi:10.1175/jpo2702.1
* Köhl, A., 2005: Anomalies of Meridional Overturning: Mechanisms in the North Atlantic. J Phys Oceanogr, 35(8), 1455-1472, doi:10.1175/JPO2767.1
* Stammer, D., 2005: Adjusting internal model errors through ocean state estimation. J. Phys Oceanogr., 35, pages 1143--1153.
* Stammer, D., C. Wunsch and K. Ueyoshi, 2005: Temporal Changes in Ocean Eddy Transports. J. Phys. Ocean., 36(3), 543-550, doi:10.1175/jpo2858.1

back to publications

back to top