Seasonal variations in
the inorganic carbon system in
the Pearl River estuary are examined based on data from five surveys during
the spring, summer, fall, and winter seasons. Both total dissolved inorganic carbon (DIC) and total alkalinity (TAlk) values in
the freshwater end-members are high in
the dry season (>2700 μmol kg
−1 for DIC and >2400 μmol kg
−1 for TAlk) and substantially lower in
the wet season (DIC and TAlk were
1000 and 700 μmol kg
−1, respectively). Riverine DIC flux and drainage basin wea
thering rates, however, are significantly higher in
the wet season (611×10
9 mol yr
−1 and 13.6×10
5 mol km
−2 yr
−1) than in
the dry season (237×10
9 mol yr
−1 and 5.3×10
5 mol km
−2 yr
−1).