In this note, I show results of several simulations, some with or without sponges. One of them (exp2_l) in particular has zero dissipation in the middle layer and is configured with a sponge layer. This simulation was run with a weaker wind run than in recent simulations (MAG=100 instead of MAG=500 and 1000). The first diagnostic of this simulation shows that, at least in the middle layer, the Eulerian-mean flow stabilizes after about day 2000 (lower panels of Fig. 1).
I show here the Eulerian-mean flow, the Lagrangian-mean flow and the LPV analysis for two different periods: around day 2000 (average over two cycles starting at day 2015 and 2065) and around day 4200 (average over two cycles starting at day 4215 and 4265).
Conclusions are:
Figure 1: Eulerian- and Lagrangian-mean flow around day 2000 (average over two cycles starting at day 2015 and 2065) in the middle layer for exp2_l.
Figure 2: Same as in Fig. 1 but around day 4200 (average over two cycles starting at day 4215 and 4265).
Figure 3: LPV analysis around day 2000 (average over two cycles starting at day 2015 and 2065) in the middle layer for exp2_l.
Figure 4: Same as in Fig. 3 but around day 4200 (average over two cycles starting at day 4215 and 4265).
Computed with theory_test_several_cycles_script.m in RESEARCH/MODELISATION/HIM/studies/diss_train_of_eddies/exp2/exp2_l/analysis_1d on the main disk on ipu1. The Matlab files are diag_VC_two_cycles_100day_long_day2015_day2065_exp2_l.mat and diag_VC_two_cycles_100day_long_day4215_day4265_exp2_l.mat in that same directory.