High-resolution ocean pH dynamics in four subtropical Atlantic benthic habitats

Calibração da perda de pressão da sonda do pressiômetro de Ménard utilizado no furo no 2 PMT 2 e o sétimo metro do furo no 1 PMT 1 Figura 3.81 – Ajuste da curva de calibração

2a framed by box.; AW: Amazon Water; STMW: Subtropical Mode Water; MW: Mediterranean Water; SACW: South Atlantic Central Water; NACW: North Atlantic Central Water; AAIW:

DMS and DMSP surface concentrations were measured dur- ing the ATA-03 study in the Mauritanian coastal upwelling region as well as in the open ocean between Mauritania and the

and pH are already or nearly detectable at the open-ocean time series sites, whereas high variability and autocorrelation in [CO 2 3 − ] may obscure the detection of

T-S-diagram in (a) framed by box.; AW: Amazon Water; STMW: Subtropical Mode Water; MW: Mediterranean Water; SACW: South Atlantic Central Water; NACW: North Atlantic Central Water;

The observed deep water carbon increase is of both natu- ral and anthropogenic origin and has several possible expla- nations; (a) remineralisation due to increased fraction of

Time Series Station (station 10 in Fig. 1) collected during September 2008 and March 2009 were used in this study as well (data available at the CARIACO Ocean Time Series

Data were separated into the principal regions: North Atlantic, South Atlantic, Indian Ocean and Pacific Ocean (Table 1), with subcategories for regions such as the Arctic Ocean,