Tomonori Azumaya

Effect of winter meteorological conditions on the formation of the cold bottom water in the eastern Bering Sea shelf

The cold bottom water, formed in the previous winter on the eastern Bering Sea shelf, remains throughout the summer. in order to examine the mechanism for the formation of the cold bottom water, we used minimum water temperature in the cold bottom water observed over the eastern Bering Sea shelf for 30 years. The interannual variation in the minimum water temperature of the cold bottom water was closely related to that of mean air temperature during cooling period at St. Paul Island. The air temperature in previous winter primarily affects the cold bottom water. We estimated decrement of the water temperature due to ice melting with simple box model. It was found with the box model that decreasing of the water temperature and lowering of the salinity depend on ice melting. To investigate the cause of interannual variation in air temperature in winter, we applied EOF analysis to the 500 hPa height. The Pacific/North American pattern (PNA) was related to mean air temperature at St. Paul Island in cooling season and the cold bottom water temperature. These results suggest the connection between ENSO events and warming or cooling in the Bering Sea shelf in winter.

Monthly variations of hydrographic structures and water mass distribution off the Doto area, Japan

Monthly variations of hydrographic structures and water mass distributions were investigated over a nearly 30-year period (January 1982–March 2011) off the Doto area, Japan, to examine temporal evolutions and devolutions of representative water masses in this area. In the continental shelf area, the Coastal Oyashio Water (COW) was distributed along the coast during January–May, when COW has been modified by relatively higher salinity water, which may have originated from the Oyashio Water (OW) off the Kuril Islands. On the other hand, the Surface COW (S-COW) may have formed with COW heated by solar radiation, simultaneously mixing with the Tokachi River freshwater and OW in the continental shelf area, and the area of this S-COW spread offshoreward during June and July, and stayed in the offshore area during June and October. Although coastal density current structures, probably due to the Modified Soya Warm Current Water (M-SWCW) inflows, were conspicuous in the continental shelf area during August–October, those structures were weak after November. These weakening structures may be due to developed surface mixed layer caused by surface cooling, and decay of volume transport of the Soya Warm Current in the Okhotsk Sea, and such weakening accordingly may lead to weakening of higher salinity water inflows from the upstream regions. M-SWCW was radically replaced by COW during December and January with rapid salinity decreases, which suggest extremely lower salinity water inflows, probably due to influences of the East Sakhalin Current Water.

Temporal variation in chum salmon, Oncorhynchus keta, diets in the central Bering Sea in summer and early autumn

Seasonal, ontogenetic, and diel variations in the diets of chum salmon, Oncorhynchus keta, were examined by analyzing the stomach contents of 1398 fish (300–755xa0mm fork length) collected in the Bering Sea during summer and early autumn of 2002. Whereas mesozooplankton, including euphausiids, hyperiids, and gastropods, constituted the greatest portion of the stomach contents during the summer, forage fishes (Stenobrachius leucopsarus and Atka mackerel, Pleurogrammus monopterygius) were the most important items during early autumn. Although no apparent diel trend was found in feeding intensity, distinct diel differences in prey composition were observed. Chum salmon caught in the morning contained Stenobrachius leucopsarus, whereas those caught in the afternoon had mainly fed on euphausiids. Thus, chum salmon diets change temporally because of changes in prey availability that result from differences in the annual life cycles and diurnal vertical migrations of prey species.