FN Archimer Export Format PT J TI New production stimulated by high-frequency winds in a turbulent mesoscale eddy field BT AF LEVY, M. KLEIN, Patrice BEN JELLOUL, M. AS 1:1;2:2;3:2; FF 1:;2:;3:; C1 Univ Paris 06, CNRS, IPSL, LOCEAN, F-75252 Paris 05, France. UBO, CNRS, IFREMER, LPO, F-29280 Brest, France. C2 LOCEAN, FRANCE UBO, FRANCE IFREMER, FRANCE CNRS, FRANCE SI BREST SE PDG-DOP-DCB-OPS-LPO IN WOS Ifremer jusqu'en 2018 copubli-france copubli-univ-france IF 3.204 TC 35 UR https://archimer.ifremer.fr/doc/2009/publication-6767.pdf LA English DT Article AB Using an idealized model of an oligotrophic open-ocean region characterized by intense sub-mesoscale turbulence, we show that the presence of energetic near-inertial motions, forced by high-frequency winds, triggers transient nutrient inputs in the surface mixed-layer, stimulating new production. We also show that this production increase is larger than the increase due to the Ekman transport resulting from a slow-evolving wind forcing. The nutrient supplies are due to the interaction between near-inertial motions and the submesoscale frontogenetic dynamics that reinforces both the vertical advection and vertical diffusion, especially within sub-mesoscales features. The net result is an uplift of new production from the subsurface to the mixed-layer. A direct consequence is that the sub-mesoscale filamentary patterns of phytoplankton should become much more observable from space in the presence of high-frequency winds. Citation: Levy, M., P. Klein, and M. Ben Jelloul (2009), New production stimulated by high-frequency winds in a turbulent mesoscale eddy field, Geophys. Res. Lett., 36, L16603, doi:10.1029/2009GL039490. PY 2009 PD AUG SO Geophysical Research Letters ( GRL ) SN 0094-8276 PU American Geophysical Union VL 36 IS L16603 UT 000269349100005 BP 1 EP 5 DI 10.1029/2009GL039490 ID 6767 ER EF