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Book ChapterDOI

The Development of the NASA GSFC and NIMA Joint Geopotential Model

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TLDR
The NASA Goddard Space Flight Center, the National Imagery and Mapping Agency (NIMA) and The Ohio State University have collaborated to produce EGM96, an improved degree 360 spherical harmonic model representing the Earth's gravitational potential as discussed by the authors.
Abstract
The NASA Goddard Space Flight Center, the National Imagery and Mapping Agency (NIMA; formerly the Defense Mapping Agency or DMA) and The Ohio State University have collaborated to produce EGM96, an improved degree 360 spherical harmonic model representing the Earth’s gravitational potential. This model was developed using: (1) satellite tracking data from more than 20 satellites, including new data from GPS and TDRSS, as well as altimeter data from TOPEX, GEOSAT and ERS-1. (2) 30’ x 30’ terrestrial gravity data from NIMA’s comprehensive archives, including new measurements from areas such as the former Soviet Union, South America, Africa, Greenland, and elsewhere. (3) 30’ x 30’ gravity anomalies derived from the GEOSAT Geodetic Mission altimeter data, as well as altimeter derived anomalies derived from ERS-1 by KMS (Kort and Matrikelstyrelsen, Denmark) in regions outside the GEOSAT coverage. The high degree solutions were developed using two different model estimation techniques: quadrature, and block diagonal. The final model is a composite solution consisting a combination solution to degree 70, a block diagonal solution to degree 359, and the quadrature model at degree 360. This new model will be used to define an undulation model that will be the basis for an update of the WGS-84 geoid. In addition, the model will contribute to oceanographic studies by improving the modeling of the ocean geoid and to geodetic positioning using the Global Positioning System (GPS).

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Journal ArticleDOI

Short Note: A global model of pressure and temperature for geodetic applications

TL;DR: The empirical model GPT (Global Pressure and Temperature), which is based on spherical harmonics up to degree and order nine, provides pressure and temperature at any site in the vicinity of the Earth's surface as mentioned in this paper.
Journal ArticleDOI

Precise orbit determination and gravity field improvement for the ERS satellites

TL;DR: In this paper, the Delft Gravity Model (DGM)-E04 has been proposed to reduce the radial orbit error by a factor of 2, and also outperforms the recent Earth Geopotential Model EGM96 in this respect.
Journal ArticleDOI

Global ocean circulation during 1992-1997, estimated from ocean observations and a general circulation model

TL;DR: In this article, a three-dimensional oceanic state is estimated for the period 1992-1997 as it results from combining large-scale ocean data sets with a general circulation model.

NOTES AND CORRESPONDENCE The Work Done by the Wind on the Oceanic General Circulation

TL;DR: In this article, a new estimate is made using altimeter data of the rate at which the wind works on the oceanic general circulation, which is lower than previously estimated and is dominated by the work done by the mean zonal wind in the Southern Ocean.
References
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The Ohio State 1991 geopotential and sea surface topography harmonic coefficient models

TL;DR: In this article, a geosat data was processed to find corrections to the a priori geopotential model, corrections to a radial orbit error model for 76 Geosat arcs, and coefficients of a harmonic representation of the sea surface topography.
Journal ArticleDOI

The Joint Gravity Model 3

TL;DR: An improved Earth geopotential model, complete to spherical harmonic degree and order 70, has been determined by combining the Joint Gravity Model 1 (JGM 1) coefficients, and their associated error covariance, with new information from SLR, DORIS, and GPS tracking of TOPEX/Poseidon, laser tracking of LAGEOS 1, LS1, LS2, and Stella as discussed by the authors.
Journal ArticleDOI

How well does a 1/4° global circulation model simulate large-scale oceanic observations?

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