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The second mesoscale experiment in the Pomo pits (Middle Adriatic Sea, May-June 1993)
Aniello RUSSO, Antonio ARTEGIANI, Mauro GALASSI, Mauro MARINI, Elio PASCHINI C.N.R. - Istituto di Ricerche sulla PEsca Marittima (IRPEM) L.go Fiera della Pesca, Ancona, ITALY Web: N. PINARDI, M. ZAVATARELLI C.N.R. - Istituto per le Metodologie Geofisiche Ambientali, Bologna, Italy F. RAICICH C.N.R. - Istituto Talassografico Sperimentale, Trieste, Italy A. R. ROBINSON, C. J. LOZANO Department of Earth and Planetary Sciences, Harvard University, Cambridge, USA
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Mappa Adriatico
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Schematic of the Adriatic Sea General Circulation (from Artegiani et al., 1997)
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Position of the stations for the two experiments
9-11 May 1993 6-9 June 1993
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Position of the stations for the two experiments
Position of the stations for the two experiments. The maps are rotated and converted to a cartesian reference system. 9-11 May 1993 75 CTD casts 6-9 June 1993 82 CTD casts
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Cumulative vertical profiles
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Vertical profiles in the Western Pomo Pit in the 1993-96 period
Depth (m) % sat. O2 Nitrate (µM) Silicate (µM) After a bottom water renewal, in the bottom layer density(not showed) and % of dissolved oxygen saturation decrease while temperature (not showed) and nutrient salts concentration increase
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Bottom maps
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SW-NE cross-section (May 1993)
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SW-NE cross-section (June 1993)
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OAG AMEX2-2
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Bathy model
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Zonal and meridional zero crossing of the correlation: 40 km
Global OA parameters Zonal and meridional zero crossing of the correlation: 40 km Zonal decorrelation (decay) scale: 20 km Time decorrelation: 7 days PE model domain Grid: 39*39*20 levels 2 km horizontal resolution, 5 flat level and 15 sigma levels 11 May 1993 7 June 1993 Base Base + ext. Forcing Assimilation Base B Base + ext. Forcing B Simulations table
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Base C4 10 day
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Base C4 11 day
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Base C4 12 day
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Base C4 13 day
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Base C4 14 day
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Base C4 15 day
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Base May Baro 4 days
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Base June Baro 4 days
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Frc June Baro 4 days
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Base June Salinity and velocity 40m
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Frc June Salinity and velocity 40m
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ECMWF wind in the AMEX domain.
The average intensity in June 1993 (3.4 m/s) was about 20% greater than in May 1993 (2.8 m/s). Wind AMEX
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Main remarks from the first simulations
- Barotropic velocities dominate the Pits area in spring, with currents forming filaments about 10 km wide - Baroclinic field determines the coastal currents, with an evident 5 days oscillation - Wind forcing do not affect the May 1993 simulation, while it is able to reverse the June circulation in the Pits Future Perspectives - Nesting in an Adriatic model to improve boundary conditions - Refinements of meteo forcing (ECMWF reanalyzes, offshore platforms) - Real time regional forecast experiment - Ecosystem studies.
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AMEX1 Sep. 1989 Profili verticali modi baroclini
From Paschini et al., D.S.R.1993 AMEX1 Sep Profili verticali modi baroclini
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Profili verticali modi baroclini
Squared Brunt-Vaisala frequency (N2) Baroclinic vertical modes First internal Rossby radius: AMEX Sept. 1989: km AMEX2-A May 1993: km AMEX2-B June 1993: km Profili verticali modi baroclini
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Profili verticali modi baroclini
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Brunt-Vaisala
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Alongshore cross-section in the Western Pomo Pit (May 1993)
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Temperature at Pescara section
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