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Mean Dynamic Topography of the Ocean Derived from Satellite and Drifting Buoy Data Using Three Different Techniques

Journal of atmospheric and oceanic technology, 2009-09, Vol.26 (9), p.1910-1919

2009

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Jean O’Brien Dickey (1945–2018)

Eos (Washington, D.C.), 2018-11, Vol.99

2018

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Modeling the high-frequency barotropic response of the ocean to atmospheric disturbances: Sensitivity to forcing, topography, and friction

Journal of Geophysical Research. C. Oceans, 2001-12, Vol.106 (C12), p.30987-30995

2001

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Ocean Measurements from Space in 2025

Oceanography (Washington, D.C.), 2010-12, Vol.23 (4), p.144-161

2010

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A record-high ocean bottom pressure in the South Pacific observed by GRACE

Geophysical research letters, 2011-02, Vol.38 (4), p.n/a

2011

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Correlated environmental corrections in TOPEX/POSEIDON, with a note on ionospheric accuracy

Journal of Geophysical Research, 1994-12, Vol.99 (C12), p.24907-24914

Zlotnicki, V.

1994

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A record-high ocean bottom pressure in the South Pacific observed by GRACE: RECORD-HIGH OBP OBSERVED BY GRACE

Geophysical research letters, 2011-02, Vol.38 (4), p.n/a

2011

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Antarctic circumpolar current transport variability during 2003-05 from GRACE

Journal of physical oceanography, 2007-02, Vol.37 (2), p.230-244

2007

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Short-period oceanic circulation: Implications for satellite altimetry

Geophysical research letters, 2000-05, Vol.27 (9), p.1255-1258

2000

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Ocean bottom pressure waves predicted in the tropical Pacific

Geophysical research letters, 2004, Vol.31 (5), p.L05306.1-L05306.4

2004

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Evaluating models of sea state bias in satellite altimetry

Journal of Geophysical Research, 1994-06, Vol.99 (C6), p.12581-12591

1994

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Quality of wind stress fields measured by the skill of a barotropic ocean model: Importance of stability of the Marine Atmospheric Boundary Layer

Geophysical research letters, 2003, Vol.30 (3), p.29.1-29.4

2003

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Mean Dynamic Topography of the Ocean Derived from Satellite and Drifting Buoy Data Using Three Different Techniques super()

Journal of atmospheric and oceanic technology, 2009-09, Vol.26 (9), p.1910-1919

2009

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Comparisons of mesoscale variability in the Semtner-Chervin 1/4° model, the Los Alamos Parallel Ocean Program 1/6° model, and TOPEX/POSEIDON data

Journal of Geophysical Research: Oceans, 1997-11, Vol.102 (C11), p.25203-25226

1997

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Sea level differences across the Gulf Stream and Kuroshio extension

Journal of physical oceanography, 1991-04, Vol.21 (4), p.599-619

Zlotnicki, Victor

1991

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Time-variable gravity from GRACE: First results

Geophysical research letters, 2004, Vol.31 (11), p.L11501.1-L11501.4

2004

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The NASA Mass Change Designated Observable Study: Overview, Progress, and Future Plans

IGARSS 2020 - 2020 IEEE International Geoscience and Remote Sensing Symposium, 2020, p.6121-6124

2020

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The 26 December 2004 tsunami source estimated from satellite radar altimetry and seismic waves

Geophysical research letters, 2005, Vol.32 (20), p.L20601.1-L20601.5

2005

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Correction to "Comparisons of mesoscale variability in the Semtner-Chervin 1/4° model, the Los Alamos Parallel Ocean Program 1/6° model, and TOPEX/POSEIDON data" by J. L. McClean et al

Journal of Geophysical Research: Oceans, 1998-03, Vol.103 (C3), p.5645-5645

1998

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Comparisons of mesoscale variability in the Semtner-Chervin 1/4 degree model, the Los Alamos Parallel Ocean Program 1/6 degree model, and TOPEX /POSEIDON data

Journal of Geophysical Research, Washington, DC, 1997-01, Vol.102 (C11), p.25203-25226

1997

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Can the weak surface currents of the Cape Verde frontal zone be measured with altimetry?

Journal of Geophysical Research. C. Oceans, 1993-02, Vol.98 (C2), p.2485-2493

1993

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Can the weak surface current of the Cape Verde frontal zone be measured with altimetry?

Journal of Geophysical Research, 1993-02, Vol.98 (C2)

1993

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Sea level variabilities in the Gulf Stream between Cape Hatteras and 50°W: A Geosat study

Journal of Geophysical Research: Oceans, 1990-10, Vol.95 (C10), p.17957-17964

1990

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The accuracy of altimétric surfaces

Geophysical Journal of the Royal Astronomical Society, 1984-09, Vol.78 (3), p.795-808

1984

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Sea level variabilities in the Gulf Stream between Cape Hatteras and 50 deg W - A Geosat study

Journal of Geophysical Research, 1990-10, Vol.95

1990

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Mean Dynamic Topography of the Ocean Derived from Satellite and Drifting Buoy Data Using Three Different Techniques

Jean O’Brien Dickey (1945–2018)

Modeling the high-frequency barotropic response of the ocean to atmospheric disturbances: Sensitivity to forcing, topography, and friction

Ocean Measurements from Space in 2025

A record-high ocean bottom pressure in the South Pacific observed by GRACE

Correlated environmental corrections in TOPEX/POSEIDON, with a note on ionospheric accuracy

A record-high ocean bottom pressure in the South Pacific observed by GRACE: RECORD-HIGH OBP OBSERVED BY GRACE

Antarctic circumpolar current transport variability during 2003-05 from GRACE

Short-period oceanic circulation: Implications for satellite altimetry

Ocean bottom pressure waves predicted in the tropical Pacific

Evaluating models of sea state bias in satellite altimetry

Quality of wind stress fields measured by the skill of a barotropic ocean model: Importance of stability of the Marine Atmospheric Boundary Layer

Mean Dynamic Topography of the Ocean Derived from Satellite and Drifting Buoy Data Using Three Different Techniques super()

Comparisons of mesoscale variability in the Semtner-Chervin 1/4° model, the Los Alamos Parallel Ocean Program 1/6° model, and TOPEX/POSEIDON data

Sea level differences across the Gulf Stream and Kuroshio extension

Time-variable gravity from GRACE: First results

The NASA Mass Change Designated Observable Study: Overview, Progress, and Future Plans

The 26 December 2004 tsunami source estimated from satellite radar altimetry and seismic waves

Correction to "Comparisons of mesoscale variability in the Semtner-Chervin 1/4° model, the Los Alamos Parallel Ocean Program 1/6° model, and TOPEX/POSEIDON data" by J. L. McClean et al

Comparisons of mesoscale variability in the Semtner-Chervin 1/4 degree model, the Los Alamos Parallel Ocean Program 1/6 degree model, and TOPEX /POSEIDON data

Can the weak surface currents of the Cape Verde frontal zone be measured with altimetry?

Can the weak surface current of the Cape Verde frontal zone be measured with altimetry?

Sea level variabilities in the Gulf Stream between Cape Hatteras and 50°W: A Geosat study

The accuracy of altimétric surfaces

Sea level variabilities in the Gulf Stream between Cape Hatteras and 50 deg W - A Geosat study

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