Interannual variability of water transport by the East Kamchatka and East Sakhalin Currents and their influence on dissolved oxygen concentration in the Sea of Okhotsk and subarctic pacific

Author:

Andreev A. G.,Shevchenko G. V.

Publisher

Allerton Press

Subject

Atmospheric Science,Fluid Flow and Transfer Processes,Water Science and Technology

Reference24 articles.

1. A. G. Andreev and I. A. Zhabin, “Distribution of Freons and Dissolved Oxygen in Intermediate Waters of the Sea of Okhotsk,” Meteorol. Gidrol., No. 1 (2000) [Russ. Meteorol. Hydrol., No. 1 (2000)].

2. K. V. Moroshkin, Water Masses of the Sea of Okhotsk (Nauka, Moscow, 1966) [in Russian].

3. A. A. Romanov, G. V. Shevchenko, and O. S. Sedaeva, “Seasonal Variations in the Sea of Okhotsk Level from Data of Coastal Tide-gauge Stations and Satellite Altimetry,” Issledovanie Zemli iz Kosmosa, No. 6 (2004) [Earth Research from Space, No. 6 (2004)].

4. O. S. Sedaeva and G. V. Shevchenko, “About Relation Between Seasonal Variations in Sea Level and Atmospheric Pressure in the Region of the Kuril Chain,” in Dynamic Processes on Shelves of the Sakhalin and Kuril Islands (IMGiG DVO RAN, Yuzhno-Sakhalinsk, 2001) [in Russian].

5. A. G. Andreev and V. I. Baturina, “Impacts of the Tides and Atmospheric Forcing Variability on Dissolved Oxygen in the Subarctic North Pacific,” J. Geophys. Res., No. C05007, 111 (2006).

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