«0* 



O' CO 

 ZEMLYA FRANTSA 



lOSIFA 



75' 



-1— 



90° 



—I— 





Circulation Pattern 



Surface Currents 

 Johnson and 

 Milligan (1967) 

 Zenkevitch (1963) 



Bottom Currents 

 Zenkevitch (1963) — ~ ' 

 ■ 



Figure I. Physiography and circulation pattern of the Kara Sea. 



16 



