%0 Journal Article %T Seasonality Of Sporadic Physical Processes Driving Temperature And Nutrient High-Frequency Variability In The Coastal Ocean Off Southeast Australia %+ School of Mathematics and Statistics [Sydney] (UNSW) %+ IMOS eMarine Information Infrastructure %+ DYNBIO LEGOS %+ The Oceans Institute and School of Environmental Systems Engineering %A Rossi, V. %A Schaeffer, A. %A Wood, J. %A Galibert, G. %A Morris, B. %A Sudre, J. %A Roughan, M. %A Waite, A. M. %Z ISI Document Delivery No.: AB6DZ Times Cited: 0 Cited Reference Count: 47 Cited References: Ajani P., 2000, J COASTAL RES, V34, P60 Alvarez I, 2008, J GEOPHYS RES-OCEANS, V113, DOI 10.1029/2008JC004744 Alvarez I, 2011, CONT SHELF RES, V31, P388, DOI 10.1016/j.csr.2010.07.009 Armbrecht L. 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Australian Research Council [DP1093510]; Australian Government through the National Collaborative Research Infrastructure Strategy; Australian Government through the Super Science Initiative; NASA Ocean Vector Winds Science Team; MICINN; FEDER through the ESCOLA project [CTM2012-39025-C02-01] The authors thank D. Krikke, P. Davies, H. MacDonald, and all the other persons involved in the field surveys. This research was supported under the Australian Research Council's Discovery Projects funding scheme (DP1093510) to A.W., M.R., and coworkers, which also supported V.R. The Integrated Marine Observing System (IMOS) is supported by the Australian Government through the National Collaborative Research Infrastructure Strategy and the Super Science Initiative. Data from the ocean reference station (ORS065) were provided by Sydney Water Corporation. SST data presented in Figure 1 were extracted from the microwave Optimally Interpolated SST (background) and from AVHRR reprocessed by IMOS (insert). QuikSCAT and SeaWinds data are produced by Remote Sensing Systems and sponsored by the NASA Ocean Vector Winds Science Team. V.R. acknowledges support from MICINN and FEDER through the ESCOLA project (CTM2012-39025-C02-01) while revising this paper. The authors thank three anonymous reviewers for their constructive comments that helped improve greatly the original manuscript. 0 AMER GEOPHYSICAL UNION WASHINGTON J GEOPHYS RES-OCEANS %< avec comité de lecture %@ 2169-9275 %J Journal of Geophysical Research. Oceans %I Wiley-Blackwell %V 119 %N 1 %P 445-460 %8 2014 %D 2014 %R 10.1002/2013jc009284 %K continental shelf oceanography %K remote-sensing %K multisensor %K wind-driven %K upwelling %K downwelling %K current-driven upwelling %K East Australian %K Current %K Western Boundary Current %K INTERANNUAL VARIABILITY %K CONTINENTAL-SHELF %K IBERIAN PENINSULA %K LOCAL %K WIND %K WESTERN %K WALES %K ENRICHMENT %K EDDY %K SEA %K ENCROACHMENT %Z Sciences of the Universe [physics]/Ocean, AtmosphereJournal articles %X Physical processes forced by alongshore winds and currents are known to strongly influence the biogeochemistry of coastal waters. Combining in situ observations (moored platforms, hydrographic surveys) and satellite data (sea surface wind and sea surface height), we investigate the transient occurrence of wind-driven upwelling/downwelling and current-driven upwelling events off southeast Australia. Remote-sensed indices are developed and calibrated with multiannual time series of in situ temperature and current measurements at two shelf locations. Based on archives up to 10 years long, climatological analyses of these indices reveal various latitudinal regimes with respect to seasonality, magnitude, duration of events, and their driving mechanisms (wind or current). Generally, downwelling-favorable winds prevail in this region; however, we demonstrate that up to 10 wind-driven upwelling days per month occur during spring/summer at 28-33.5 degrees S and up to 5 days in summer further south. Current-driven upwelling upstream of the East Australian Current separation zone (approximate to 32 degrees S) occurs twice as often as downstream. Using independent in situ data sets, we show that the response of the coastal ocean is consistent with our climatology of shelf processes: upwelling leads to a large range of temperatures and elevated nutrient concentrations on the shelf, maximized in the wind-driven case, while downwelling results in destratified nutrient-poor waters. The combination of these sporadic wind- and current-driven processes may drive an important part of the high-frequency variability of coastal temperature and nutrient content. Our results suggest that localized nutrient enrichment events of variable magnitude are favored at specific latitudes and seasons, potentially impacting coastal ecosystems. Key Points Multisensor analysis of shelf processes combining in situ and satellite data Spatio-temporal variability of transient wind and current-driven up/downwelling Cold/nutrient-rich water intrusions favoured at specific locations/seasons %G English %2 https://hal.science/hal-00998669/document %2 https://hal.science/hal-00998669/file/Rossi_etal_JGR2014.pdf %L hal-00998669 %U https://hal.science/hal-00998669 %~ IRD %~ INSU %~ METEO %~ UNIV-TLSE3 %~ CNRS %~ CNES %~ OMP %~ OMP-LEGOS %~ DYNBIO %~ GIP-BE %~ SYSCO2 %~ UNIV-UT3 %~ UT3-INP %~ UT3-TOULOUSEINP