TABLE IVD. Instrument measurement error 



Station No. 



True 



dynamic 



height 



DM 



Dynamic 

 height with 

 maximum 

 instrument 



error 

 ±0.05° C. ± 

 0.0307„<, DM 



Dynamic 

 height with 

 maxiniam 

 instrument 



error 

 ±0.01° C. ± 

 0.0307oo DM 



Dynamic 



height with 



maximum 



instrument 



error 



±0.016° C, ± 



0.014°/„„ DM 



Maximum 

 error 



2<7 0f 



normal 



distribution 



curve 



9236 



9241 



9242 



9243 



9247 



9248 



9249 



9268 



9379 



9385 



9396 



9398 



9399 



9400 



9408 



Averages - 



0. 5737 

 .5925 

 .5663 

 .6825 

 .5950 

 .7341 

 .5892 

 .5291 

 .5248 

 .6035 

 .5613 

 .6960 

 .6028 

 .5960 

 . 5332 



0.6016 

 .6195 

 .5942 

 .7116 

 .6270 

 .7634 

 .6176 

 .5571 

 .5527 

 .6344 

 .5894 

 .7251 

 .6313 

 .6249 

 .5589 



0.5971 

 .6159 

 .5896 

 .7060 

 .6221 

 .7574 

 .6128 

 .5525 

 .5483 

 .6270 

 .5848 

 .7194 

 . 6262 

 .6191 

 .5528 



0. 5859 

 .6043 

 .5786 

 .6947 

 .6084 

 .7466 

 .6015 

 .5413 

 .5370 

 .6158 

 .5734 

 .7086 

 .6152 

 .6086 

 .5454 



0.0122 

 .0118 

 .0123 

 .0122 

 .0134 

 .0125 

 .0123 

 .0122 

 .0122 

 .0123 

 .0121 

 .0126 

 .0124 

 .0126 

 .0122 

 .0124 



0.0120 

 .0116 

 .0121 

 .0120 

 .0132 

 .0123 

 .0121 

 .0120 

 .0120 

 .0121 

 .0119 

 .0124 

 .0122 

 .0124 

 .0120 

 .0122 



•All Dynamic Heights must be added to the standard 970.403 based on the 1,000-decibar level. 



TABLE VD. Thermometer comparisons 



TABLE OF OCEANOGRAPHIC DATA 



The following is the observed and interpolated data for the Coast Guard 

 Oceanograpliic Unit oceanographic stations taken in conjunction with the 

 International Ice Patrol 1965 in the Grand Banks of Newfoundland area. 

 The data was obtained from CG cutter Evergreen, 30 March 1965, to 25 May 

 1965. Presentation is from National Oceanographic Data Center Cruise 

 Listing No. 31-540. 

 Notes: 



Depth to bottom — -uncorrected sounding depth in meters based on a 



speed of sound in sea water of 4,800 ft. /sec. 

 Depth (m) — postscript T indicates a depth determined by ther- 



mometric calculations. 

 Sound velocity — in meters per second to tenths according to Wilson's 



formula. 

 A complete description of codes can be found in NODC publication 

 M-2, "Processing Physical and Chemical Data From Oceano- 

 graphic Stations." 



80 



