• Aucun résultat trouvé

Interactions between the Somali Current eddies during the summer monsoon: insights from a numerical study

N/A
N/A
Protected

Academic year: 2021

Partager "Interactions between the Somali Current eddies during the summer monsoon: insights from a numerical study"

Copied!
22
0
0

Texte intégral

Figure

Figure 1. Climatological mean of the sea surface height (colour shading; cm) with currents at 15 m depth superimposed (vectors; m s −1 ) in the 1/4 ◦ S4-1 simulation and in the observational reference for: (a) the month of June and (b) the month of Septemb
Figure 2. Top panels: snapshot (on 14 June 1984 from the 1/12 ◦ S12-2 experiment) of surface currents (vectors; m s −1 ) superimposed on (a) the relative vorticity (ζ ; colour shading; s −1 ) at depth 50 m; (b) the spiciness on σ 0 = 23.8 (5; colour shadin
Figure 3. Sequence of relative vorticity (ζ ; colour shading; s −1 ) and currents (vectors; m s −1 ) at 50 m, (a) in the 1/4 ◦ S4-1 simulation, and (b) in the 1/12 ◦ S12-2 simulation
Figure 4. Snapshots of current (vectors; m s −1 ) at 50 m superimposed on (a) relative vorticity (ζ ; colour shading; s −1 ) at 50 m and (b) spici- spici-ness on isopycnal σ 0 = 23.8 (5; colour shading; kg m −3 ), at three different stages of the Southwest
+7

Références

Documents relatifs

The crows then started to become more cryptic and careful. Although not yet able to identify the shooter, observer, or the car as a threat to avoid, the crows became

So, the second step to ensure that our work reaches the right audience is drawing attention to our work, creating a community, and engaging the public.. As written by

While it is natural for us to talk about cumulated gain over time, the traditional cumulated gain measures have substi- tuted document rank for time and implicitly model a user

For conservative dieomorphisms and expanding maps, the study of the rates of injectivity will be the opportunity to understand the local behaviour of the dis- cretizations: we

Consider an infinite sequence of equal mass m indexed by n in Z (each mass representing an atom)... Conclude that E(t) ≤ Ce −γt E(0) for any solution y(x, t) of the damped

The number of detected eddies is increased in the case of the high resolution simulation, which demonstrates that high resolution numerical models are needed to resolve mesoscale

An anticyclonic eddy, in good agreement with satellite imagery as far as its size and position, is for the first time reproduced numerically, in the western side of the gulf of Lion,

[ 1 ] All climate models predict a freshening of the North Atlantic at high latitude that may induce an abrupt change of the Atlantic Meridional Overturning Circulation (here-