FN Archimer Export Format PT J TI Impact of global ocean model resolution on sea-level variability with emphasis on interannual time scales BT AF PENDUFF, Thierry JUZA, Melanie BRODEAU, L. SMITH, G. C. BARNIER, B. MOLINES, J. -M. TREGUIER, Anne-Marie MADEC, G AS 1:1,2,3;2:1,2;3:1,2;4:4;5:1,2;6:1,2;7:5,6;8:4,7,8; FF 1:;2:;3:;4:;5:;6:;7:;8:; C1 CNRS, UMR 5519, Lab Ecoulements Geophys & Ind, F-38041 Grenoble, France. Univ Grenoble, F-38041 Grenoble, France. Florida State Univ, Dept Oceanog, Tallahassee, FL 32306 USA. Natl Oceanog Ctr, Southampton, Hants, England. IFREMER, CNRS, UMR 6523, Lab Phys Oceans, F-29280 Plouzane, France. UBO, F-29280 Plouzane, France. IPSL, CNRS, UMR 7159, Lab Oceanog & Climat Experimentat & Approches Num, F-75252 Paris, France. UPMC, F-75252 Paris, France. C2 CNRS, FRANCE UNIV GRENOBLE, FRANCE UNIV FLORIDA STATE, USA NOC, UK CNRS, FRANCE UBO, FRANCE IPSL, FRANCE UNIV PARIS 06, FRANCE IF 1.443 TC 105 UR https://archimer.ifremer.fr/doc/00003/11386/7965.pdf LA English DT Article AB Four global ocean/sea-ice simulations driven by the same realistic 47-year daily atmospheric forcing were performed by the DRAKKAR group at 2 degrees, 1 degrees, 1/2 degrees, and 1/4 degrees resolutions. Simulated mean sea-surface heights (MSSH) and sea-level anomalies (SLA) are collocated over the period 1993-2004 onto the AVISO dataset. MSSH fields are compared with an inverse estimate. SLA datasets are filtered and compared over various time and space scales with AVISO regarding three characteristics: SLA standard deviations, spatial correlations between SLA variability maps, and temporal correlations between observed and simulated band-passed filtered local SLA timeseries. Beyond the 2 degrees-1 degrees transition whose benefits are moderate, further increases in resolution and associated changes in subgrid scale parameterizations simultaneously induce (i) strong increases in SLA standard deviations, (ii) strong improvements in the spatial distribution of SLA variability, and (iii) slight decreases in temporal correlations between observed and simulation SLA timeseries. These 3 effects are not only clear on mesoscale (14-180 days) and quasi-annual (5-18 months) fluctuations, but also on the slower (interannual), large-scale variability ultimately involved in ocean-atmosphere coupled processes. Most SLA characteristics are monotonically affected by successive resolution increases, but irregularly and with a strong dependance on frequency and latitude. Benefits of enhanced resolution are greatest in the 1 degrees-1/2 degrees and 1/2 degrees-1/4 degrees transitions, in the 14-180 day range, and within eddy-active mid-and high-latitude regions. In the real ocean, most eddy-active areas are characterized by a strong SLA variability at all timescales considered here; this localized, broad-banded temporal variability is only captured at 1/4 degrees resolution. PY 2010 PD FEB SO Ocean Science SN 1812-0784 PU Copernicus Gesellschaft Mbh VL 6 IS 1 UT 000276175700019 BP 269 EP 284 DI 10.5194/os-6-269-2010 ID 11386 ER EF