486 



John B. Tait 



Carruthhrs (1954) for warp- or cable-angle measurement and current meter 

 anchoring have become known -was of course less reliable on account of the 

 necessity to suspend the current meter from a drifting ship. Nevertheless, m the 



Table I 

 Volume transport of oeeanic ^vater {salinity > 34-99 7oo) through the linear hydro- 

 graphic sections, {a) Faroe Bank to Butt of Lewis, and (b) Faroe Islands to Shetland 

 {in 1927 to Fair Isle), when the pair of sections was traversed within an interval of 



14 days 



remarkably calm conditions prevailing, the endeavour was made with not unsatis- 

 factory results within a few days of the corresponding experiments on top of the 

 Wyville Thomson Ridge in the month of May 1953. The depth of the 35-007oo 



