http://www.cnr.it/ontology/cnr/individuo/prodotto/ID6918
Pelagic primary production in the Algero-Provençal basin by means of multisensor satellite data: focus on interannual variability and its drivers (Articolo in rivista)
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- Pelagic primary production in the Algero-Provençal basin by means of multisensor satellite data: focus on interannual variability and its drivers (Articolo in rivista) (literal)
- Anno
- 2011-01-01T00:00:00+01:00 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
- 10.1007/s10236-011-0405-8 (literal)
- Alternative label
Olita A., Sorgente R., Ribotti A., Fazioli, L., Perilli, A. (2011)
Pelagic primary production in the Algero-Provençal basin by means of multisensor satellite data: focus on interannual variability and its drivers
in Ocean dynamics (Print)
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- Olita A., Sorgente R., Ribotti A., Fazioli, L., Perilli, A. (literal)
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- Titolo
- Pelagic primary production in the Algero-Provençal basin by means of multisensor satellite data: focus on interannual variability and its drivers (literal)
- Abstract
- In this work, we make use of satellite esti-
mates of chlorophyll
a
, photosynthetically active radia-
tion and sea surface temperatures, to compute regional
estimates of primary production integrated throughout
the euphotic layer for the Algero-Provençal Basin, by
means of a modified version of the vertically general-
ized production model. The seasonal and interannual
variability of the primary production has been analysed
over the decade 1997-2007. Empirical orthogonal func-
tions analysis has been applied to decompose the vari-
ability of the primary production dataset in orthogonal
modes of variability. The seasonal signal is distributed
between the two first modes of variability, temporally
shifted each other and respectively related to the north-
ern (early spring) and the southern (winter) part of the
basin. We found a minimum of the annual production
in 2003, when a summer heatwave strongly enhanced
the stratification of surface waters, further limiting the
injection of nutrients into the surface layers. Maxima
in the annual series are found in 1999 and 2005, due
to two particularly intense and extended (in space)
spring-blooms in the northern part of the basin. These
two maxima, clearly identified in space and time by
EOF analysis (EOF1 and EOF3), are related to strong
mistral-wind interannual events occurring during win-
ters of 1999 and 2005, preceding the blooms by some
Responsible Editor: Joachim W Dippner
A. Olita (
B
)
·
R. Sorgente
·
A. Ribotti
·
L. Fazioli
·
A. Perilli
National Research Council,
Institute for Coastal Marine Environment,
Loc. Sa Mardini, 09170 Torre Grande, Oristano Italy
e-mail: antonio.olita@iamc.cnr.it
few months. We found that these production maxima
are due both to a more intense production in the usual
blooming area (shown by EOF1-PC1) as well as to an
exceptional local production in the eastern side of the
basin, off the Corsica western coasts (EOF3-PC3). Pre-
vious observations of exceptional deep-water forma-
tion events in 1999 and 2005, with easterly spots close
to the primary production-observed anomalies, and the
meridional character of the mistral 1999 and 2005 peaks
both support the idea that such eastern PP interannual
maxima would be actually due to exceptional produc-
tion more than to an easterly advection of biomass from
the usual bloom area. Finally, the potential link of the
observed features with large-scale atmospheric forcing
is discussed, and a potential relation of such interannual
events with the East Atlantic pattern is drawn. (literal)
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