ABSTRACT
Instantaneous determinations of photosynthetically active radiation (PAR) over the sea from the Ocean and Land Color Instrument (OLCI) on Sentinel-3 are compared with in-situ measurements at the island of Lampedusa in the central Mediterranean Sea. Radiative transfer calculations show that the PAR measured at the island site is representative for open ocean conditions. Satellite data show a good agreement (5.2% positive bias, R2 = 0.97) with in-situ data, in line with similar analyses for other satellite sensors. Larger satellite-in situ differences are found during summer, and the possible role of aerosols in degrading PAR estimate has been investigated by comparing AOD values measured at Lampedusa and derived by OLCI. The relative difference between OLCI and in-situ PAR appears to be negatively correlated with the relative differences between OLCI and in-situ AOD, suggesting that a more accurate determination of AOD, in particular, for cases with AOD > 0.2, mostly related to Saharan dust, may lead to improved satellite PAR estimates.
Acknowledgments
Contributions by Pamela Trisolino, Fabrizio Anello, and Salvatore Piacentino are gratefully acknowledged.
The authors thank EUMETSAT and the EU Copernicus service for making available the OLCI data and the University of Valladolid and AERONET staff for the provision of Cimel photometer calibration and processing.
Mirko Nobili is thanked for the Lampedusa aerial picture shown in .
The International Space Station picture of is courtesy of the Earth Science and Remote Sensing Unit, NASA Johnson Space Center (https://eol.jsc.nasa.gov).
The reviewers are thanked for their valuable suggestions and contributions.
Disclosure statement
No potential conflict of interest was reported by the author(s).
Data availability statement
Data available on request from the authors.