Eric Leuliette

Dr. Eric Leuliette

orcid

Research Focus & Metrics

Academic Career Length

30Years (1997-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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1 January 2004 in Marine Geodesy
Verified
Journal Article
Closed access
ELEric Leuliette
Eric Leuliette
RNR. Steven Nerem
R. Steven Nerem
GMGary T. Mitchum
Gary T. Mitchum
Jason, the successor to the TOPEX/POSEIDON (T/P) mission, has been designed to continue seamlessly the decade-long altimetric sea level record initiated by T/P. Intersatellite calibration has determined the relative bias to an accuracy of 1.6 mm rms. Tide gauge calibration of the T/P record during its original mission shows a drift of −0.1 ± 0.4 mm/year. The tide gauge calibration of 20 months of nominal Jason data indicates a drift of −5.7 ± 1.0 mm/year, which may be attributable to errors in the orbit ephemeris and the Jason Microwave Radiometer. The analysis of T/P and Jason altimeter data over the past decade has resulted in a determination of global mean sea level change of +2.8 ± 0.4 mm/year.

25 February 2009 in Geophysical Research Letters
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Journal Article
Closed access
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ELEric Leuliette
Eric Leuliette
LMLaury Miller
Laury Miller

1 June 2011 in Oceanography
Verified
Journal Article
Open access
ELEric Leuliette
Eric Leuliette
JWJosh Willis
Josh Willis

1 October 1999 in Geophysical Research Letters
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Journal Article
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RNR. S. Nerem
R. S. Nerem
DCD. P. Chambers
D. P. Chambers
ELEric Leuliette
Eric Leuliette
GMG. T. Mitchum
G. T. Mitchum
BGB. S. Giese
B. S. Giese

17 October 2006 in Comptes Rendus. Géoscience
Verified
Journal Article
Open access
RNRobert Steven Nerem
Robert Steven Nerem
ELEric Leuliette
Eric Leuliette
Anny CazenaveAnny Cazenave
Anny Cazenave
Understanding of sea-level change has improved considerably over the last decade. Present-day knowledge of sea-level change is derived from tide gauge observations and satellite altimetry measurements. The average rate of sea-level change obtained from tide gauges over the last 50 years is + 1.8 ± 0.3 mm yr −1 . In comparison, altimeter measurements from TOPEX/Poseidon and Jason-1 have shown an average rise of + 3.1 ± 0.4 mm yr −1 since 1993. It is not clear yet whether the larger rate of rise of the last decade reflects acceleration or decadal fluctuation. The causes of the present-day rate are a combination of increases in ocean temperatures and land ice melt from mountain glaciers, Greenland, and Antarctica. Regional variability in sea-level change, as evidenced by the quasi global coverage of altimeter satellites, appears dominated by non uniform change of thermal expansion. New satellite technologies, such as InSAR, ICESat, and GRACE make significant contributions to understanding sea-level change.

21 October 2005 in Geophysical Research Letters
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Journal Article
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MTM. E. Tamisiea
M. E. Tamisiea
ELEric Leuliette
Eric Leuliette
JDJ. L. Davis
J. L. Davis
JMJ. X. Mitrovica
J. X. Mitrovica