Seasonal and interannual variability of chlorophyll a and primary production in the Equatorial Atlantic: in situ and remote sensing observations

Abstract

The seasonal variability of phytoplankton in the Equatorial Atlantic was analysed using Sea-viewing Wide Field-of-view Sensor (SeaWiFS)-derived chlorophyll a (Chl a) concentration data from 1998 to 2001, together with in situ Chl a and primary production data obtained during seven cruises carried out between 1995 and 2000. Monthly averaged SeaWiFS Chl a distributions were in agreement with previous observations in the Equatorial Atlantic, showing marked differences between 10 W in the Eastern Tropical Atlantic (ETRA) and 25 W in the Western Tropical Atlantic (WTRA) provinces J. Plankton Res., 17, 1245-1271). The seasonal cycle of SeaWiFS-derived Chl a concentration calculated for 0-10 S, 0-20 W (ETRA) is consistent with in situ Chl a measurements, with values ranging from 0.16 mg m 3 , from February to April, to 0.52 mg m 3 in August. Lower variability was observed in 10 N10 S, 20-30 W (WTRA) where minimum and maximum concentrations occurred in April (0.15 mg m 3 ) and in August (0.24 mg m 3 ), respectively. A significant empirical relationship between depth-integrated primary production and in situ measured sea surface Chl a was found for ETRA, allowing us to estimate the seasonal cycle of depthintegrated primary production from SeaWiFS-derived Chl a. As for Chl a, this model was verified in a small area of the Eastern Equatorial Atlantic (0-10 S, 0-20 W), although in this instance it was not completely able to describe the magnitude and temporal variability of in situ primary production measurements. The annual euphotic depth-integrated primary production rate estimated for ETRA by our empirical model was 1.4 Gt C year 1 , which represents 16% of the open ocean primary production estimated for the whole Atlantic Ocean.