http://www.cnr.it/ontology/cnr/individuo/prodotto/ID6510
Effects of the 2003 European heatwave on the Central Mediterranean Sea: surface fluxes and the dynamical response (Articolo in rivista)
- Type
- Label
- Effects of the 2003 European heatwave on the Central Mediterranean Sea: surface fluxes and the dynamical response (Articolo in rivista) (literal)
- Anno
- 2007-01-01T00:00:00+01:00 (literal)
- Alternative label
Olita A., Sorgente R., Natale S., Gabersek S., Ribotti A., Bonanno A., and Patti B.. (2007)
Effects of the 2003 European heatwave on the Central Mediterranean Sea: surface fluxes and the dynamical response
in Ocean science (Print)
(literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- Olita A., Sorgente R., Natale S., Gabersek S., Ribotti A., Bonanno A., and Patti B.. (literal)
- Pagina inizio
- Pagina fine
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
- Rivista
- Note
- ISI Web of Science (WOS) (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
- Titolo
- Effects of the 2003 European heatwave on the Central Mediterranean Sea: surface fluxes and the dynamical response (literal)
- Abstract
- The effects of the 2003 European heatwave on the
sea surface layer of the Central Mediterranean were studied
using a regional 3-D ocean model. The model was used to
simulate the period 2000 to 2004 and its performance was
validated using remotely-sensed and in situ data. Analysis
of the results focused on changes in the Sea Surface Temperature
(SST) and on changes to the surface and sub-surface
current field. This permitted us to identify and quantify the
anomalies of atmospheric and sea surface parameters that accompanied
the heatwave. The dominant annual cycle in each
variable was first removed and a wavelet analysis then used
to locate anomalies in the time-frequency domain.
We found that the excess heating affecting the sea surface
in the summer of 2003 was related to a significant increase in
air temperature, a decrease in wind stress and reduction of all
components of the upward heat flux. The monthly averages
of the model SST were found to be in good agreement with
remotely-sensed data during the period studied, although the
ocean model tended to underestimate extreme events. The
spatial distribution of SST anomalies as well as their timefrequency
location was similar for both the remotely-sensed
and model temperatures. We also found, on the basis of the
period of the observed anomaly, that the event was not limited
to the few summer months of 2003 but was part of a
longer phenomenon. Both the model results and experimental
data suggest the anomalous heating mainly affected the
top 15m of ocean and was associated with strong surface
stratification and low mixing.
The skill of the model to reproduce the sub-surface hydrographic
features during the heatwave was checked by comparison
with temperature and salinity measurements. This
showed that the model was generally in good agreement with
observations. The model and observations showed that the
anomalous warming also modified the currents in the region,
most noticeably the Atlantic Ionian Stream (AIS) and the Atlantic
Tunisian Current (ATC). The AIS was reduced in intensity
and showed less meandering, mainly due to the reduced
density gradient and low winds, while the ATC was
enhanced in strength, the two currents appearing to modulate
each other in order to conserve the total transport of Modi-
fied Atlantic Water. (literal)
- Prodotto di
- Autore CNR
Incoming links:
- Autore CNR di
- Prodotto
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#rivistaDi