Engineering topics
Fukumori, I.
Publications and source records attributed to Fukumori, I..
NASA Supercomputer Improves Prospects for Ocean Climate Research
Estimates of ocean circulation constrained by in situ and remotely sensed observations have become routinely available during the past five years, and they are being applied to myriad scientific and operational problems [Stammer et al.,2002]. Under the Global Ocean Data Assimilation Experiment (GODAE), several regional and global estimates have evolved for applications in climate research, seasonal forecasting, naval operations, marine safety, fisheries,the offshore oil industry, coastal management, and other areas. This article reports on recent progress by one effort, the consortium for Estimating the Circulation and Climate of the Ocean (ECCO), toward a next-generation synthesis of ocean and sea-ice data that is global, that covers the full ocean depth, and that permits eddies.
Temperature advection: internal versus external processes
Local advection of temperature is the inner product of vector velocity and spatial gradient of temperature. This product is often integrated spatially to infer temperature advection over a region.
Eastern equatorial Pacific Ocean T-S variations with El Nino
Temperature-Salinity (T-S) relationship variability in the pycnocline of the eastern equatorial Pacific Ocean (NINO3 region, 5 degrees S ??degrees N, 150 degrees W ?? degrees W) over the last two decades is investigated using observational data and model simulation.
On the physical consistency of data assimilation and a computationally effective approximate smoother
Explore the source record for details and available documents.
Earth oblateness variations: unraveling glacial melting, ocean mass redistribution and post-glacial rebound effects
Explore the source record for details and available documents.
The ECCO routine global ocean data assimilation system
Explore the source record for details and available documents.
GRACE gravity model: assssment in terms of deep ocean currents from hydrography and from the ECCO ocean model
Here we assess the new generation of gravity models, derived from GRACE data. The differences between a global geoid model (one from GRACE data and one the well-known EGM-96), minus a Mean Sea Surface derived from over a decade of altimetric data are compared to hydrographic data from the Levitus compilation and to the ECCO numerical ocean model, which assimilates altimetry and other data.
Atmospheric and oceanic excitation of length-of-day variations during 1980-2000
Explore the source record for details and available documents.
The ECCO routine global ocean data assimilation system
Explore the source record for details and available documents.
The ECCO routine global ocean data assimilation system
Explore the source record for details and available documents.
An open-circuit and a short-circuit in the Pacific Ocean subtropical-tropical exchange
Explore the source record for details and available documents.
A global comparision of Ekman pumping from satellite scatterometers and ocean data assimilation estimates
Ekman pumping obtained from various scaterometers are compared with those derived from ECCO model which assimilate TOPEX-derived sea level anomalies using the adjoint and Kalman filter/smoother methods.
Estimating the circulation and climate of the ocean; the circulation pathway of subtropical-tropical exchange
Explore the source record for details and available documents.
Interannual-to-decadal variation of tropical-subtropical exchange in the Pacific Ocean: boundary versus interior pathways
In this study, we address issues using sea level measurements obtained by the TOPEX/Poseidon satellite altimter and circulation estimated by the Consortium for Estimating the Circulation and Climate of the Ocean (ECCO).
Calibrating the ECCO ocean general circulation model using Green's functions
Green's functions provide a simple, yet effective, method to test and calibrate General-Circulation-Model(GCM) parameterizations, to study and quantify model and data errors, to correct model biases and trends, and to blend estimates from different solutions and data products.
Upper-ocean heat budget inferred from ECCO-2 ocean data assimilation
Explore the source record for details and available documents.
Upper-ocean heat budget inferred from ECCO-2 ocean data assimilation
Explore the source record for details and available documents.