This was motivated by the goal of developing reliable satellite remote sensing methods for monitoring the phytoplankton biomass and primary productivity from space (see Siegel et al., 2013 and the references therein). Empirical relationships for estimating Chl from remote sensing reflectance Selleck Trichostatin A have been used for routine processing of global satellite imagery of ocean color since the beginning of the SeaWiFS mission in 1997 (O’Reilly et al., 1998 and O’Reilly et al., 2000). In the past several years, interpretation of ocean-color satellite data has progressed beyond the estimation of Chl to include new products. For example, it is now possible to determine

the dominant phytoplankton functional groups present in oceanic surface waters (e.g., Alvain et al., 2005 and Brewin et al., 2011) and to retrieve information about particle size distribution (Kostadinov et al., 2010 and Loisel et al., 2006). In addition, information about important components and processes of the oceanic carbon cycle

such as the primary productivity (Antoine et al., 1996, Behrenfeld and Falkowski, 1997 and Woźniak et al., 2007), the particulate organic carbon concentration (Duforet-Gaurier et al., 2010, Gardner et al., 2006, Stramska and Stramski, 2005 and Stramski et al., 2008), and the colored dissolved and detrital organic matter absorption (Maritorena et al., 2002 and Siegel et al., 2002)

can be derived from satellite data. Before these new data products are broadly used in oceanographic studies, it is extremely important AZD6244 to validate the performance of the various ocean color algorithms with observations. The main objective of this paper is to evaluate the performance of the standard NASA POC algorithm (Stramski et al., 2008). For POC product match-up analysis we have used coincident in situ data and satellite data from SeaWiFS and MODIS Aqua. We searched 16 years of satellite data from 1997 to 2012 for matchups with in situ data. In situ POC data have been obtained from public databases of the U.S. Joint Global Ocean Flux Study (U.S. JGOFS, http://usjgofs.whoi.edu/jg/dir/jgofs/) and the SeaWiFS Bio-optical Carnitine dehydrogenase Archive and Storage System (SeaBASS), the publicly shared archive maintained by the NASA Ocean Biology Processing Group (OBPG) (http://oceancolor.gsfc.nasa.gov). We have selected only these in situ data sets for which POC determinations were made using JGOFS protocols (Knap et al., 1996) and filters were acidified for removal of inorganic carbon prior to combustion. We have assumed that POC values of 10 mg m−3 and less were invalid in situ POC determinations if found outside the hyperoligotrophic waters of the South Pacific Subtropical Gyre (Stramski et al., 2008). We have found 2418 surface in situ POC concentration data fulfilling these requirements.