@conference{Karageorgis2015,
title = {Particle distribution and composition in the NE Aegean Sea based on transmissometry, optical backscattering and size measurements},
author = {A.P. Karageorgis and A. Androni and G. Assimakopoulou and A.C. Banks and P. Drakopoulos and G. Kabouri and Th. Kanellopoulos and E. Krasakopoulou and A. Lagaria and M. Morfis and K. Pagou and V. Papadopoulos and K. Parinos and S. Psarra and P. Renieris and N. Spyridakis},
url = {https://www.researchgate.net/publication/306441194_Particle_distribution_and_composition_in_the_NE_Aegean_Sea_based_on_transmissometry_optical_backscattering_and_size_measurements},
isbn = {978-960-9798-08-2},
year = {2015},
date = {2015-05-01},
pages = {777-780},
organization = {Proc. 11th Panhel. Symp. Oceanogr. & Fish},
abstract = {The complex optical properties of NE Aegean Sea particles were studied in the framework of Perseus and AegeanMarTech projects. Inherent optical properties (IOPs; beam attenuation, optical backscattering, fluorescence) and discrete bottle data (PMC, POC, TChl-a) were measured during October 2013. Black Sea water (BSW) enters into the Aegean Sea from the Dardanelles and disperses to the west-northwest, as traced by characteristic salinity minima. The core of the BSW to the east of Limnos Island was relatively particle-enriched, showing maxima in beam c p , b bp , fluorescence, D 50 , PMC, POC, and TChl-a. Organic particles dominated in the upper water column, whereas resuspension of surface sediments was detected.},
keywords = {IOP, NE Aegean Sea, particle size, particulate matter, scattering},
pubstate = {published},
tppubtype = {conference}
}
The complex optical properties of NE Aegean Sea particles were studied in the framework of Perseus and AegeanMarTech projects. Inherent optical properties (IOPs; beam attenuation, optical backscattering, fluorescence) and discrete bottle data (PMC, POC, TChl-a) were measured during October 2013. Black Sea water (BSW) enters into the Aegean Sea from the Dardanelles and disperses to the west-northwest, as traced by characteristic salinity minima. The core of the BSW to the east of Limnos Island was relatively particle-enriched, showing maxima in beam c p , b bp , fluorescence, D 50 , PMC, POC, and TChl-a. Organic particles dominated in the upper water column, whereas resuspension of surface sediments was detected.
