of bulletin No. 44 (1958 soasonj should he coircM'tcd lo the following 

 values: ^ 



Iiit(Miui'(li;it(' waliT 



2000 meters 



2500 meters 



3000 iiKMcrs 



3r)()0 meters 



While the tabulation of the salinity corrections being- listed accord- 

 ing to stations permits the correction of specific sections of salinity, 

 the corrections to certain illustrations are not apparent as for instance 

 the ciu'ves representing the T-S relationship of the water masses 

 found in the CJi-and Banks region. For those, the following corrections 

 to the salinities are necessary. 



Fiijii 



of 



It should be noted that beginning with the 105(5 season, the T-S 

 curv^es foi- the _\'ear have been compared with postwar averages. The 

 average curves shown are in error and should be disregarded. The 

 corrected postwar averages are conii)are(l with the })re\var averages 

 in figure 30. 



Other published figures show pot(Mitial densities and uccmI the 



following corrections : 



Bidleti'. 

 Year No. Figure I'lUje Correelion to <Je 



1953 39 40 87 +0.02o 



+ 0.02 



+ 0.024 for broken lines 

 + 0.02. fdi- solid liiie.s 

 + 0.024 



SlalioH 4!»71-4980, +0.02. 

 4981-4984, +O.O23 

 498.5-4988, +O.O23 

 4989-4994, +0.02. 



1954 40 33,31,35, 109 113 lO.OU except +0.02. for the 



3(), 37 bi'okeii lines in figure 37. 



1 955 41 22 79 + 0.02,, 



< In ill! till! bulletins of this scries ;in inferior final digit in a number indieale.s that that digit is in doubt :iricl 

 the luiraber has not been rounded oil. Thus a salinity of 34.896 would bo rounded oti to 34.90. 



42 



