Merging of barotropic symmetric vortices. A case study for gulf stream rings
MASINA and N. PINARDI Istituto per lo Studio delle Metodologie Geofisiche Ambientali, CNR - Modena, Italia (ricevuto il 18 Gennalo 1990; approvato il 10 Maggio 1991) Summary. - - We made numerical experiments to study the merging dynamics of axisymmetric barotropic ringlike vortices
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PII: 0278-4343(94)90049-3
~ ) Pergamon Continental Shelf Research, Vol. 14, No. 12, pp. 1293-1310, 1994 Elsevier Science Ltd Printed in Great Britain. 0278~-343/94 $7.00 + 0.00 Mesoscale data assimilation studies in the Middle Adriatic Sea SIMONA MASINA*~ and NADIA PINARDI* (Received 13 February 1992; in
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PII: 0967-0637(93)90117-L
Deep-Sea Research I. Vol 40 No 7 pp 1365-1377, 1993 0967-0637/93 $6 00 + 0 0fl Printed m Great Bntam (~ 1993 Pergamon Press Ltd The ... November 1990, m revtsed form 6 October 1992, accepted 6 October 1992) Abst rac t - -The analysis of the first mesoscale exper iment m the middle
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AdriaClim Application ID: 10252001 29th and 30th November 2022 6th Project Meeting & 7th Steering Committee Agenda Meeting venue: Zadar Tuesday 29 November 2022, Morning Session: 09:00 – 12:30 9:00 -9:20 Day 1 Welcome coffee & Registration ZADRA NOVA and Arpae 9:20 – 9:40 Welcome
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PII: 0377-0265(89)90057-2
Dynamics of Atmospheres and Oceans, 14 (1989) 65-76 65 • ~ . . Elsevier Science Pubhshers B.V., Amsterdam - Pnnted in The Netherlands A NOTE ON CONSISTENT QUASI-GEOSTROPHIC BOUNDARY CONDITIONS IN PARTIALLY OPEN, SIMPLY AND MULTIPLY CONNECTED DOMAINS N A D I A PINARDI * and RALPH
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Geosci. Model Dev., 6, 1851–1869, 2013 www.geosci-model-dev.net/6/1851/2013/ doi:10.5194/gmd-6-1851-2013 © Author(s) 2013. CC Attribution 3.0 License. Geoscientific Model Development O pen A ccess MEDSLIK-II, a Lagrangian marine surface oil spill model for short-term forecasting – Part 1:
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PII: S0079-1946(98)00071-8
Pergamon Phys. Chem. Earth, Vol. 23, No. 5~ , pp. 569 574, 1998 1998 Elsevier Science Ltd. All rights reserved Plh S0079- i 946 ... 1-40129, Bologna, Italy Received 25 April 1997; accepted 1 December 1997 Abstract . Sea surface heat budgets are estimated for the Mediterranean
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PII: S0079-1946(98)00070-6
25 April 1997: accepted 1 December 1997 Abst rac t . Adriatic Sea surface heat and water fluxes for the i~riod 1991-1994 have been computed from the ECM`WF (European Center for Medium Range ̀ weather Forecast) operational analyses data. The obtained sur- face heat flux climatology
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42(4)-02.fm
Italy Received 9 May 2007; Revised 9 October 2007; Accepted 18 October 2007 Abstract − We compare insolation results calculated from two well ... on SMS of changing the ‘Sun-Earth distance factor ( f )’, a parameter which is commonly assumed to be constant in the oceanographic context.
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doi:10.1016/j.jmarsys.2006.03.006
deterministic models. This approach is sufficiently generic that may be used to describe other existing biomass-based ecosystem model. © 2006 Elsevier ... ical constituents and associated rates has not been ⁎ Corresponding author. Tel.: +39 051 4151 456; fax: +39 051 4151 499. E-mail address:
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PII: 0924-7963(94)00011-Y
Implications for altimetric data assimilation studies N. Pinardi ‘, A. Rosati, R.C. Pacanowski GFDL-NOAA, Forrestal Campus, Princeton, NJ 08542, USA ... satellite altimetry seems to be the next promising data set to be considered. It is ’ Permanent address: IMGA-CNR, Via Emilia Est 770, 41100,
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PII: S0079-1946(98)00060-3
0079-1946(98)00060-3 007% 1946/98/$- see front matter A S p e c t r a l E l e m e n t O c e a n M o d e l on the C r a y T 3 D : the I n t e r a n n u a l V a r i a b i l i t y o f the M e d i t e r r a n e a n S e a G e n e r a l C i r c u l a t i o n A. J. Molcard, N. Pinardi ] and R. Ansaloni 2 I
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clim_13_118.732_745
erature one can trace a variety of applications of this 15 FEBRUARY 2000 733K O R R E S E T A L . technique. Extended EOF (EEOF) and canonical ... 1989). Let us indicate by f j(x) a time series of 2D fields (e.g., the barotropic streamfunction) from the model simulation, where x 5 1, . . . ,
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jcliD1300139 442..447
Bologna, Italy. E-mail: nadia.pinardi@unibo.it 442 JOURNAL OF CL IMATE VOLUME 27 DOI: 10.1175/JCLI-D-13-00139.1 � 2014 American Meteorological ... equation. In our case we make the assumption that the density is written as r 5 r0 1 r 0, where r0 is a constant such that (r 0/r0) � 1 (Chusman-
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Mediterranean Forecasting System: An improved assimilation scheme for sea-level anomaly and its validation
Kalman filter it is propagated by the linear model ∗ Corresponding author: Istituto di Geofisca e Vulcanologia, Via Creti 12, 40128 Bologna, ... approximation of the Kalman filter with the analysis calculated from the formula: xa = xb + K{y −H(xb)}, (1) where xa is the analysis state vector, xb
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