Full metadata record
DC FieldValueLanguage
dc.contributor.authorMELIN FREDERICen_GB
dc.contributor.authorCLERICI MARCOen_GB
dc.contributor.authorZIBORDI GIUSEPPEen_GB
dc.contributor.authorBULGARELLI BARBARAen_GB
dc.date.accessioned2010-02-25T16:14:22Z-
dc.date.available2006-11-20en_GB
dc.date.available2010-02-25T16:14:22Z-
dc.date.issued2006en_GB
dc.date.submitted2006-03-17en_GB
dc.identifier.citationJOURNAL OF GEOPHYSICAL RESEARCH vol. 111 p. D22201en_GB
dc.identifier.urihttp://publications.jrc.ec.europa.eu/repository/handle/JRC32868-
dc.description.abstractThe aerosol optical properties in the Adriatic Sea are presented using a 9-year time series (1996-2005) of automated measurements collected on the Acqua Alta Oceanographic Tower (AAOT) in the northern part of the basin and a coincident satellite record obtained from an atmospheric correction scheme adapted for European seas and applied to SeaWiFS. At AAOT, the overall averages of aerosol optical thickness taua at 500 nm and Angstrom exponent alpha are 0.29+/-0.21 and 1.51+/-0.34, respectively. The average single scattering albedo varies from 0.957 at 440 nm to 0.910 at 1020 nm. The aerosol size distribution derived by optical data inversion exhibits an increase of the radius of the accumulation mode with taua. From 402 coincident data records, the agreement between satellite and field taua is remarkable, with mean relative absolute differences of 17-20% in the 412-870 nm spectral range. On the other hand, the satellite record tends to filter out occurrences of high taua. The satellite products are used to analyze the seasonal cycle over the Adriatic basin, showing minima in winter and maxima in summer (taua(500) from 0.06 to 0.23). Then, the results of radiative transfer simulations are combined with the satellite derived seasonal cycles of taua and cloud fraction to determine the clear-sky aerosol direct radiative effect for the Adriatic Sea. At the surface, the aerosol load results in a monthly average cooling effect ranging from -1 W.m-2 in winter up to -9.6 W.m-2 in August and a corresponding atmospheric warming from 0.5 to 4.6 W.m-2.en_GB
dc.description.sponsorshipJRC.H.3-Global environement monitoringen_GB
dc.format.mediumPrinteden_GB
dc.languageENGen_GB
dc.publisherAMER GEOPHYSICAL UNIONen_GB
dc.relation.ispartofseriesJRC32868en_GB
dc.titleAeresol Variability in the Adriatic Sea from Automated Optical Field Measurements and SeaWiFSen_GB
dc.typeArticles in periodicals and booksen_GB
JRC Directorate:Sustainable Resources

Files in This Item:
There are no files associated with this item.


Items in repository are protected by copyright, with all rights reserved, unless otherwise indicated.