The second mesoscale experiment in the Pomo pits (Middle Adriatic Sea, May-June 1993)

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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, 60125 Ancona, ITALY Web: http://adria.irpem.an.cnr.it 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 The second mesoscale experiment in the Pomo pits (Middle Adriatic Sea, May-June 1993)

description

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) - PowerPoint PPT Presentation

Transcript of The second mesoscale experiment in the Pomo pits (Middle Adriatic Sea, May-June 1993)

Page 1: 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, 60125 Ancona, ITALY Web: http://adria.irpem.an.cnr.it

N. PINARDI, M. ZAVATARELLIC.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

The second mesoscale experiment in the Pomo pits

(Middle Adriatic Sea, May-June 1993)

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12° E 13° E 14° E 15° E 16° E 17° E 18° E 19° E39° N

40° N

41° N

42° N

43° N

44° N

45° N

46° N

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P o

A n c o n a

V i e s t e

S p l i t

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IONIAN SEA

Otranto

Pescara

Sibenik

Bari

Dubrovnik100

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Pelagosa sill

Otranto sill

Pomo Pits

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

101103

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AM EX2-A station positions

14° 10' E 15° 00' E42° 10' N

43° 00' N

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AM EX2-B station positions

14° 10' E 15° 00' E42° 10' N

43° 00' N

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9-11 May 1993 6-9 June 1993

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Position of the stations for the two experiments. The maps are rotated and converted to a cartesian reference system.

-40 -20 0 20 40k m

A M E X 2 - 1 S t a t i o n p o s i t i o n s

-40

-20

0

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km

2 0 0

1 00

-40 -20 0 20 40k m

A M E X 2 - 2 S t a t i o n p o s i t i o n s

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9-11 May 199375 CTD casts

6-9 June 199382 CTD casts

+ CTD cast Chem ical cast

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Cumulative vertical profiles

1 0 1 5 2 0 2 5Tem perature (°C )

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pres

sure

(db

)

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35 36 37 38 39Salin ity (psu)

AMEX2-B June 1993

AMEX2-A May 1993

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Dep

th (

m)

% sat. O2 Nitrate (µM) Silicate (µM)

Vertical profiles in the Western Pomo Pit in the 1993-96 period

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

AM EX2-A bottom tem perature

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10.210.310.410.510.610.710.810.911.011.111.211.311.411.511.611.711.811.9

AM EX2-B bottom d isso lved oxygen

20 40 60 80100

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5.005.055.105.155.205.255.305.355.405.455.505.555.605.655.705.755.805.855.905.956.00

AM EX2-B bottom tem perature

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10.210.310.410.510.610.710.810.911.011.111.211.311.411.511.611.711.811.9

AM EX2-B bottom sa lin ity

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38.2038.2238.2438.2638.2838.3038.3238.3438.3638.3838.4038.4238.4438.4638.4838.50

AM EX2-A bottom sa lin ity

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38.2038.2238.2438.2638.2838.3038.3238.3438.3638.3838.4038.4238.4438.4638.4838.50 AM EX2-A bottom d isso lved oxygen (m l/l)

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5.005.055.105.155.205.255.305.355.405.455.505.555.605.655.705.755.805.855.905.956.00

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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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Global OA parametersZonal and meridional zero crossing of the correlation: 40 kmZonal decorrelation (decay) scale: 20 kmTime decorrelation: 7 daysPE model domainGrid: 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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Wind AMEX

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-6

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-8 -6 -4 -2 0 2 4 6 8

may93

june93ECMWF 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).

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- Nesting in an Adriatic model to improve boundary conditions

- Refinements of meteo forcing (ECMWF reanalyzes, offshore

platforms)

- Real time regional forecast experiment

- Ecosystem studies.

- 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

Main remarks from the first simulations

Future Perspectives

Page 27: The second mesoscale experiment  in the Pomo pits  (Middle Adriatic Sea, May-June 1993)

AMEX1 Sep. 1989 Profili verticali modi baroclini

From Paschini et al., D.S.R.1993

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Profili verticali modi baroclini

Baroclinic vertical modes

Squared Brunt-Vaisala frequency(N2)

First internal Rossby radius:AMEX Sept. 1989: 5.4 kmAMEX2-A May 1993: 3.5 - 4.0 kmAMEX2-B June 1993: 4.5 - 5.0 km

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Profili verticali modi baroclini

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Brunt-Vaisala

0.00E+00

1.00E-03

2.00E-03

3.00E-03

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413B BVF 413A BVF

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Alongshore cross-section in the Western Pomo Pit (May 1993)

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0 20 40 60 80 100 120 140 160km

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W IN TER

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Tem perature (°C ) a long the Pescara-S ibenik section (c.i. 0.5)

SPRIN G

SUM M ER AUTUM N6.07.08.09.010.011.012.013.014.015.016.017.018.019.020.021.022.023.024.025.026.027.0

Temperature at Pescara section