MIMOSA (Modeling Isentrope du transport Méso-échelle de l’Ozone Stratophérique par Advection) er en modell som følger bevegelsen til luftmassene i stratosfæren, og studerer hvordan disse utvikler seg i tid og rom. Siden luftmassene i stratosfæren ikke blandes med luftmasser over eller under den, kan MIMOSA følge de «samme» luftmassene i flere dager.

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