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Dynamics of the oceanographic properties during mucilage appearance in the Northern Adriatic Sea: analysis of the 1997 event in comparison to earlier events (Articolo in rivista)
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- Dynamics of the oceanographic properties during mucilage appearance in the Northern Adriatic Sea: analysis of the 1997 event in comparison to earlier events (Articolo in rivista) (literal)
- Anno
- 2004-01-01T00:00:00+01:00 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
- 10.1016/j.jmarsys.2004.01.007 (literal)
- Alternative label
Cozzi S. (a); Ivancic I. (b); Catalano G. (a); Djakovac T. (b); Degobbis D. (b) (2004)
Dynamics of the oceanographic properties during mucilage appearance in the Northern Adriatic Sea: analysis of the 1997 event in comparison to earlier events
in Journal of marine systems; Elsevier, Amsterdam (Paesi Bassi)
(literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- Cozzi S. (a); Ivancic I. (b); Catalano G. (a); Djakovac T. (b); Degobbis D. (b) (literal)
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- doi:10.1016/j.jmarsys.2004.01.007 (literal)
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- http://www.sciencedirect.com/science/journal/09247963 (literal)
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- (a) Laboratory of Chemical and Physical Oceanography, CNR-ISMAR, Marine Science Institute, Section of Trieste, Viale R. Gessi 2, I-34123, Trieste, Italy
(b) Rudjer Boskovic Institute, Center for Marine Research (CMR), G. Paliaga 5, I-52210 Rovinj, Croatia (literal)
- Titolo
- Dynamics of the oceanographic properties during mucilage appearance in the Northern Adriatic Sea: analysis of the 1997 event in comparison to earlier events (literal)
- Abstract
- The dynamics of the oceanographic properties in Northern Adriatic Sea during the 1997 mucilage event is
reported. These observations, compared to a longer time series (1985-1998), indicate that processes on short temporal
scales and abrupt changes of the physical and biogeochemical conditions in the basin have a great effect on mucilage
events.
The seawater warming during the years with the mucilage was delayed in May and June compared to those
without aggregate. Since the same typical summer values were afterward reached in both cases, a more abrupt
warming is supposed in the period preceding mucilage events.
During 1997, the Po River regime had an abrupt change from very low flow rates in April-May (526-985 m3 s? 1)
to a strong freshet in July (4870 m3 s? 1). This river pulse, coupled to the scarce intrusion of the high salinity Middle
Adriatic Deep Water (MAdDW), determined the large retention of low salinity waters in the Northern Adriatic Sea from
July to September. In 1997, as well as during the events in 1989, 1991, the freshwater content in the basin was two times
higher (4-5%) with respect to the years without aggregates from 1992 to 1998 ( < 2%).
The biological response to these physical forcings was an intense phytoplankton bloom in the western low salinity
waters in July 1997 (O2sat. up to 206%, Chlorophyll-a (Chl-a) up to 7.64 Ag dm? 3), a common feature in all years with
mucilage. It determined a strong increase of dissolved organic nitrogen (DON, + 100%) and phosphorus (DOP, + 39%)
in the most productive western waters of the basin, which constitute available material for mucilage formation. Nutrient
content in the upper waters shifted in concomitance to mucilage appearance, from a PO4-scarce condition in spring
(Si/N/P = 225:105:1), to a rather severe dissolved inorganic nitrogen (DIN) and SiO4-depletion in summer (Si/N/P = 21:13:1).
This drastic change can stimulate exudate hyperproduction and/or modify bacteria degradation capacity of organic
matter.
As a consequence of degradation of sinking aggregates, in summer 1997 strong hypoxic conditions were reached in
the deeper waters (down to 55% in most of the profile, down to 16% in the western area). Increasing AOU/DIN (up to 143) and AOU/PO4 (up to 2500) ratios indicated a progressive nitrogen and phosphorous impoverishment in aged
aggregates. (literal)
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