scholarly journals A review of the Sea of Okhotsk ecosystem response to the climate with special emphasis on fish populations

2012 ◽  
Vol 69 (7) ◽  
pp. 1123-1133 ◽  
Author(s):  
Sen Tok Kim

Abstract Kim, S. T. 2012. A review of the Sea of Okhotsk ecosystem response to the climate with special emphasis on fish populations. – ICES Journal of Marine Science, 69: . This article provides a brief review of climatic, oceanographic, and biological changes in the Sea of Okhotsk in recent decades. The Sea of Okhotsk is distinguished by its high biological productivity and its significant impact on the Pacific Ocean through water exchanges. Long-term temperature data have shown periodic cooling and warming of the Sea that in turn have resulted in changes to its biological communities. In the 1980s, a generally warm period, the Sea of Okhotsk had abundant fish, primarily large stocks of gadoids, especially walleye pollock. The second half of the 1990s was a transitional period when the marine ecosystem was being restructured. In particular, by the mid-1990s, the total biomass of fish in the Sea of Okhotsk had decreased significantly. In the early 2000s, the situation reached a critical level, but by the end of that decade, there was a renewed warming and an increase in the abundance of walleye pollock.

2020 ◽  
Author(s):  
Evgeny Lopatnikov ◽  
Viktor Kalinchuk ◽  
Anatoly Astakhov ◽  
Yang Gang ◽  
Jianjun Zou

<p>Continuous measurements of gaseous elemental mercury (Hg(0)) in the marine boundary layer (MBL) and Hg(0) fluxes were conducted in the Sea of Japan and the Sea of Okhotsk from September 7 to October 17, 2019. All Hg(0) measurements were carried out using two RA-915M mercury analysers (Lumex LLC, Russia). Hg(0) concentrations in the air were measured at two levels (about 2 m and 20 m above the sea surface) with a time resolution of 30 minutes. Hg(0) fluxes were measured at five sample stations using a dynamic flux chamber.</p><p>During the cruise Hg(0) concentrations varied in the range from 0,47 ng/m<sup>3</sup> to 1,55 ng/m<sup>3</sup>, and from 0,31 ng/m<sup>3</sup> to 2,71 ng/m<sup>3</sup> with medians of 0,92 ng/m<sup>3</sup> for 2 m and 20 m, respectively. Atmospheric Hg(0) concentrations in measurements sites were strongly depended on the regions from where air masses came to the study areas. As a result of the Concentration Weighted Trajectory (CWT) analysis we established 2 regions that influenced the Hg(0) concentrations during the cruise: the Northeast China with the Yellow Sea region and the Kurile Islands sector of the Pacific Ocean. The arrival of air masses from China and the Yellow Sea region caused an increase in Hg(0) concentrations in the air in the Sea of Japan and the Sea of Okhotsk. Elevated concentrations were also observed In the Sea of Okhotsk during the periods air masses came from the Kurile Islands sector of the Pacific Ocean.</p><p>Hg(0) fluxes were measured at 3 stations in the Sea of Japan and at 2 stations in the Sea of Okhotsk. The values ranged from 0,57 ng/m<sup>2</sup>/h to 1,55 ng/m<sup>2</sup>/h, with median value of 1,32 ng/m<sup>2</sup>/h. A positive relationships between Hg(0) flux and air and water temperature were observed.</p><p>This work was supported by the Russian Science Foundation (RSF) (Project № 19-77-10011) and by the National Natural Science Foundation of China (Projects №: 41876065, 41420104005, U1606401) and National Program on Global Change and Air-Sea Interaction (Project № GASI-GEOGE-04).</p>


1947 ◽  
Vol 12 (3Part1) ◽  
pp. 173-179
Author(s):  
George I. Quimby

The peninsula of Kamchatka in Siberia is situated between the Sea of Okhotsk on the west and Bering Sea and the Pacific Ocean on on the east. This peninsula is about 750 miles long and 80 to 300 miles wide with a mountainous and volcanic interior and a somewhat severe climate. Forests cover all the land except where there are areas of tundra or alpine vegetation.


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