±0.0255 DM. By comparing this figure with dynamic height calculations are concerned with 



that of the greatest continuous sampler error of the contmuous sampler providing a much more 



±0.0282 DM shown above, it is concluded that complete description of the temperature and 



both systems give comparable results insofar as salinity distribution. 



REFERENCES 



KoUmeyer, Ronald C. (1964). An Examination of Errors Whitney, G. G., Jr. (1957). Factors Affecting the Accu- 



in Dynamic Height Determinations. U.S. Coast racy of Thermometric Depth Determination. Journal 



Guard. Unpublished manuscript, series, October 1963. du Conseil, vol. XXII, No. 2, pp. 167-173. 



70 



