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$BBj!!L\!'(BInterannual variability of dense water production in
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Interannual variability of dense water production in (Sergey V.Gladyshev) $BH/I=MW;]!'(B
Data of 1996 and 1997 CTD surveys were used to estimate interannual variability of brine water production in the northern Okhotsk Sea polynyas. Annual removal rate of this water from the northern shelf was also defined. Possible influence of ice production in polynyas on the seasonal ice cover in the Sea of Okhotsk and renewal rate of the Okhotsk Sea Mode Water are discussed. The general conclusions are: a)formation of high-dense water in polynyas decreased in nineties; b) north-western shelf and Gizhiga (Shelikhov Bay) polynyas are the main contributors to the high-dense water production and dense water originated from the north-western shelf polynya ventilates intermediate water of the Deryugin Basin as well as dense water from Shelikhov Bay directly ventilates intermediate water in the Tinro Deep. These results will be used to calibrate Cavalieri and Martin (1994) model of dense water production in the Okhotsk Sea.
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