Figure 4 

 of the Se 

 expand c 

 NOTE 



VHR d qfa^ n a rth eat t Sa g o f J a pa n, So viet Ca(m« Snkhn l in, nnd the wpstprn p ort 



of Okhotsk .\ Ascending node Oi4/;C~t^Ap r i I 1*^^, ^^/^b/ ^fy.. Jx>jy/,e.QhQnce , 

 n,rBrr7^SQUjt)sfk^suai range daV 

 ^^'■'^gfanmar 'Structure and fracturing of tTi^i^ea /c/& in the Sea of Okhotsk 

 (egst^d north of Sakhalin). All of the drift ic^a^^is probably 50-90 cm thick 

 and the varrcition in shading is due to y9CiP^''on in\ice «^ncentrations (from 3 

 to 10 tenths)\ north of the ice edge 



West of Sat^iw'Tn, off the mouth of the Amur River, Vhe landfastTcfe-s-sm0sriy 

 ■^ ' ' ' ' * ' ■' .1. nting snow,Av<if5nion the 



ie sea sycf^ce nirtheast 



white vi^j*f^fhe dark bqnd against the coastlines repres 

 ice^ajfa 'surf ace pudol/ng of the ice itself. 

 3. T^uiyjcface waller fl^ patterns outlined by drift ice. 



of Hokkaido. 



301 T8A?ai1AJ. 



4. In the Sea of Ok^ho+sCLthe wind drift-asTa resul 

 System moves the\i<^SDut}je^dg5aai creating 

 aOQi^mg the ice^st^^^ngsolong tne eastern ice e'd 



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