FN Archimer Export Format PT J TI Sea state bias in altimeter sea level estimates determined by combining wave model and satellite data BT AF TRAN, N. VANDEMARK, D. LABROUE, S. FENG, H. CHAPRON, Bertrand TOLMAN, H. L. LAMBIN, J. PICOT, N. AS 1:1;2:7;3:1;4:7;5:2,3;6:6;7:4;8:5; FF 1:;2:;3:;4:;5:PDG-DOP-DCB-OPS-LOS;6:;7:;8:; C1 CLS, DOS, F-31520 Ramonville St Agne, France. IFREMER, Ctr Brest, F-29280 Plouzane, France. IFREMER, Space Oceanog Lab, F-29280 Plouzane, France. CNES, DCT, SI, F-31401 Toulouse, France. CNES, DCT, PO, F-31401 Toulouse, France. NOAA, NCEP, EMC, Marine Modeling & Anal Branch, Camp Springs, MD 20746 USA. Univ New Hampshire, Ocean Proc Anal Lab, Durham, NH 03824 USA. C2 CLS, FRANCE IFREMER, FRANCE IFREMER, FRANCE CNES, FRANCE CNES, FRANCE NOAA, USA UNIV NEW HAMPSHIRE, USA SI BREST SE PDG-DOP-DCB-OPS-LOS IN WOS Ifremer jusqu'en 2018 copubli-france copubli-int-hors-europe IF 3.303 TC 31 UR https://archimer.ifremer.fr/doc/00002/11276/7851.pdf https://archimer.ifremer.fr/doc/00002/11276/7855.pdf LA English DT Article AB This study documents a method for increasing the precision of satellite-derived sea level measurements. Results are achieved using an enhanced three-dimensional (3-D) sea state bias (SSB) correction model derived from both Jason-1 altimeter ocean observations (i.e., sea state and wind) and estimates of mean wave period from a numerical ocean wave model, NOAA's WAVEWATCH III. A multiyear evaluation of Jason-1 data indicates sea surface height variance reduction of 1.26 (+/- 0.2) cm(2) in comparison to the commonly applied two-parameter SSB model. The improvement is similar for two separate variance reduction metrics and for separate annual data sets spanning 2002-2004. Spatial evaluation of improvement shows skill increase at all latitudes. Results indicate the new model can reduce the total Jason-1 and Jason-2 altimeter range error budgets by similar to 7.5%. In addition to the 2-D (two-dimensional) and 3-D model differences in correcting the range for wavefield variability, mean model regional differences also occur across the globe and indicate a possible 1-2 cm gradient across ocean basins linked to the zonal variation in wave period (short fetch and period in the west, swells and long period in the east). Overall success of this model provides first evidence that operational wave modeling can support improved ocean altimetry. Future efforts will attempt to work within the limits of wave modeling capabilities to maximize their benefit to Jason-1 and Jason-2 SSB correction methods. PY 2010 PD MAR SO Journal Of Geophysical Research-oceans SN 0148-0227 PU American Geophysical Union VL 115 IS C03020 UT 000275859600001 BP 1 EP 7 DI 10.1029/2009JC005534 ID 11276 ER EF