TY  - JOUR
AU  - Bouruet-Aubertot, P.
AU  - Mercier, H.
AU  - Gaillard, F.
AU  - Lherminier, P.
PY  - 2005//
TI  - Evidence of strong inertia-gravity wave activity during the POMME experiment
T2  - J. Geophys. Res.
JO  - Journal of geophysical research-atmospheres
VL  - 110
PB  - American Geophysical Union
KW  - inertia-gravity waves
KW  - turbulent mixing
KW  - 4544 Oceanography: Physical: Internal and inertial waves
KW  - 4568 Oceanography: Physical: Turbulence
KW  - diffusion
KW  - and mixing processes
KW  - 4572 Oceanography: Physical: Upper ocean and mixed layer processes
N2  - The purpose of this paper is to characterize inertia-gravity waves (IGW) activity and to investigate the variability of these waves in relationship to atmospheric forcing and larger-scale motions. To this aim, we analyzed Eulerian measurements of horizontal currents and temperature collected over 1 year during the Programme Océan Multidisciplinaire Méso Echelle (POMME). We focused on the main frequency components of the IGW spectrum, namely the inertial frequency f and the semidiurnal frequency M2. Time evolution of the relative energy of these two components gave evidence of isolated events of high intensity. We performed a detailed analysis of these events and identified mechanisms of generation of these waves. Localized spots of intense, near-inertial IGW were observed in winter. During the mixed layer deepening, one event was correlated with plume-like structures resulting from peaks of intense surface cooling. This suggests a local generation process driven by strong downward vertical motions. Instead, other events of strong IGW could be related to submesoscale features, characteristic of a frontal region, in particular, wave trapping within anticyclonic eddies. In contrast, a downward energy propagation down to about 500 m below the mixed layer was isolated after a stormy period. Eventually, internal tidal beams, possibly generated at a nearby seamount, intermittently crossed the mooring, though less energetically than the previous events. Last, we estimated the eddy diffusivity from the velocity vertical shear. Large variations were obtained, from 10?6 m2/s up to 10?3 m2/s, consistent with the intense events previously isolated.
SN  - 0148-0227
UR  - http://dx.doi.org/10.1029/2004JC002747
N1  - exported from refbase (http://publi.ipev.fr/polar_references/show.php?record=5590), last updated on Mon, 27 Apr 2009 13:39:26 +0200
ID  - Bouruet-Aubertot_etal2005
ER  -