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Mimosa routines: V8.1
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Daily production of PV and Temperature maps from MIMOSA : High Resolution Transport Model

- Mimosa overview

MIMOSA (Modélisation Isentrope du transport Méso-échelle de l'Ozone Stratosphérique par Advection) high resolution advection model of potential vorticity (PV) has been developed at Service d'Aéronomie in the frame of the European Union project METRO (MEridional TRansport of Ozone in the lower stratosphere) which was part of THESEO (Third European Stratospheric Experiment on Ozone) 2000 campaigns. A full description of MIMOSA is given in Hauchecorne et al. [2001].
The model runs on an isentropic surface, starting on an orthogonal grid in an azimuthal equidistant projection centered at North or South Pole (parallels are represented as concentric equidistant circles). It covers latitudes between 90°S and 90°N in the present version. The size of an elementary grid cell 37*37 km (3 grid points/degree of latitude).


- Potential vorticity and temperature forecasts from (J) to day J+5

North Hemisphere Maps
PV Analysis - 380K 380K - 24h 380K - 48h 380K - 72h 380K - 96h 380K - 120h
 
PV Analysis - 435K 435K - 24h 435K - 48h 435K - 72h 435K - 96h 435K - 120h
 
PV Analysis - 475K 475K - 24h 475K - 48h 475K - 72h 475K - 96h 475K - 120h
 
PV Analysis - 550K 550K - 24h 550K - 48h 550K - 72h 550K - 96h 550K - 120h
 
PV Analysis - 675K 675K - 24h 675K - 48h 675K - 72h 675K - 96h 675K - 120h
 
PV Analysis - 950K 950K - 24h 950K - 48h 950K - 72h 950K - 96h 950K - 120h
 

South Hemisphere Maps
PV Analysis - 380K 380K - 24h 380K - 48h 380K - 72h 380K - 96h 380K - 120h
 
PV Analysis - 435K 435K - 24h 435K - 48h 435K - 72h 435K - 96h 435K - 120h
 
PV Analysis - 475K 475K - 24h 475K - 48h 475K - 72h 475K - 96h 475K - 120h
 
PV Analysis - 550K 550K - 24h 550K - 48h 550K - 72h 550K - 96h 550K - 120h
 
PV Analysis - 675K 675K - 24h 675K - 48h 675K - 72h 675K - 96h 675K - 120h
 
PV Analysis - 755K 755K - 24h 755K - 48h 755K - 72h 755K - 96h 755K - 120h
 
PV Analysis - 950K 950K - 24h 950K - 48h 950K - 72h 950K - 96h 950K - 120h
 

PV - Tropical Maps
PV Analysis - 380K 380K - 24h 380K - 48h 380K - 72h 380K - 96h 380K - 120h
 
PV Analysis - 435K 435K - 24h 435K - 48h 435K - 72h 435K - 96h 435K - 120h
 
PV Analysis - 475K 475K - 24h 475K - 48h 475K - 72h 475K - 96h 475K - 120h
 
PV Analysis - 550K 550K - 24h 550K - 48h 550K - 72h 550K - 96h 550K - 120h
 
PV Analysis - 675K 675K - 24h 675K - 48h 675K - 72h 675K - 96h 675K - 120h
 

North Hemisphere Maps
T Analysis - 380K 380K - 24h 380K - 48h 380K - 72h 380K - 96h 380K - 120h
 
T Analysis - 435K 435K - 24h 435K - 48h 435K - 72h 435K - 96h 435K - 120h
 
T Analysis - 475K 475K - 24h 475K - 48h 475K - 72h 475K - 96h 475K - 120h
 
T Analysis - 550K 550K - 24h 550K - 48h 550K - 72h 550K - 96h 550K - 120h
 
T Analysis - 675K 675K - 24h 675K - 48h 675K - 72h 675K - 96h 675K - 120h
 
T Analysis - 950K 950K - 24h 950K - 48h 950K - 72h 950K - 96h 950K - 120h
 

South Hemisphere Maps
T Analysis - 380K 380K - 24h 380K - 48h 380K - 72h 380K - 96h 380K - 120h
 
T Analysis - 435K 435K - 24h 435K - 48h 435K - 72h 435K - 96h 435K - 120h
 
T Analysis - 475K 475K - 24h 475K - 48h 475K - 72h 475K - 96h 475K - 120h
 
T Analysis - 550K 550K - 24h 550K - 48h 550K - 72h 550K - 96h 550K - 120h
 
T Analysis - 675K 675K - 24h 675K - 48h 675K - 72h 675K - 96h 675K - 120h
 
T Analysis - 755K 755K - 24h 755K - 48h 755K - 72h 755K - 96h 755K - 120h
 
T Analysis - 950K 950K - 24h 950K - 48h 950K - 72h 950K - 96h 950K - 120h
 

T - Tropical Maps
T Analysis - 380K 380K - 24h 380K - 48h 380K - 72h 380K - 96h 380K - 120h
 
T Analysis - 435K 435K - 24h 435K - 48h 435K - 72h 435K - 96h 435K - 120h
 
T Analysis - 475K 475K - 24h 475K - 48h 475K - 72h 475K - 96h 475K - 120h
 
T Analysis - 550K 550K - 24h 550K - 48h 550K - 72h 550K - 96h 550K - 120h
 
T Analysis - 675K 675K - 24h 675K - 48h 675K - 72h 675K - 96h 675K - 120h