Supplement of

Abstract In order to investigate the effect of glacial water on the CO 2 system in the fjord, we studied the variability of the total alkalinity (A T ), total dissolved inorganic

Figure 1: Differences between CRM measurements and CRM pH calculated from certified values of TA, DIC, salinity, silicate, and phosphate using the constants of Roy et al. (1993) at 15

Physical oceanography silicate, of dissolved inorganic carbon and alkalinity, of particulate organic carbon (POC) and of phytoplankton pigments such as chlorophyll, of isotopes

Total alkalinity (TA) and total dissolved inorganic carbon (DIC) were measured on board by C.Brunet and C.Grosbois (LBCM) using a technique based on the potentiometric method of

Carbonate chemistry speciation at variable dissolved inorganic carbon (DIC) and constant total alkalinity (TA), describing ongoing ocean acidification (OA), in comparison to four

[ 1 ] Normalization to a constant salinity (S) is widely used for the adjustment of marine inorganic carbon chemistry data such as total alkalinity (A T ) and total dissolved

dissolved inorganic carbon (DIC), total alkalinity (TA), proton acceptors, proton donors, zero level of protons, conservative quantities,.. buffering,

o The differences in carbonate chemistry between the two manipulation methods cause no substantial differences in the general ecophysiological responses of two strains of E.. o