| Abstrak/Abstract |
To clarify the mechanism of hypoxia in the western interior parts of the Ariake Sea (WIAS), field observation data collected in the period of 1972–2004 were analyzed using a twolayer box model. Monthly averages of advection velocity, vertical diffusion coefficient (Kz), and biochemical oxygen consumption rate (R) in WIAS were evaluated quantitatively during
the above period. The estimated advection velocity comparatively corresponded to the observed residual flow pattern of bay head in summer and winter. The estimated Kz was relatively high (0.6– 5.3 cm2 s?1) from September to March but lower
(0.2–0.4 cm2 s?1) from April to August. The estimated R ranged from 0.30 to 0.46 mg L?1 day?1 during May to August. In summer, the temporal variation of dissolved oxygen (DO) concentration in the lower layer was controlled largely by Kz and R. Monthly variations of Kz, R, and degree of density stratification (P) in the 1970s, the 1980s, and the 1990s–early 2000s were analyzed. P, Kz, and R were not significantly different among the calculated periods (p = 0.93, 0.23, and 0.49).However, the variations of R in summer between the 1970s and the other calculated periods changed. DO consumption period was longer in the 1980s and the 1990s–early 2000s than in the 1970s. R in the 1980s was highest among the calculated periods. The increase in R in the 1980s was caused by the increase in organic matter load originating from red tide phytoplankton due to a decrease in the suspension feeders. |
