DATE 



NO OF HYDRO STATION 



NO OF BT 



G.M TIME 



LATITUDE (NORTH) 



LONGITUDE (WEST) 



SURFACE SALINITY %. 



SURFACE TEMPERATURE °C. 



DISTANCE! NAUTICAL MILES) ^j, 



26-MAY-63 



037- HOOT 



184 



1500 



36°I3' 



73°5I' 



185 

 1656 

 36»I0' 

 73°46' 

 34.35 

 17,6 



1740 

 36°06' 

 73°42' 

 36.61 

 13.8 



187 



1815 



36"03' 



73"37' 



038-HOOa- — 



IBS 190 191 



1850 2055 2130 



35''59' 3S°55' 35°52' 



73°33' 73°29' 73''25' 



192 

 2200 

 35-48' 

 73*21' 



— 039-H009 



193 194 

 2235 2300 

 35°44' 35°42' 

 73°I7' 73°I5' 



196 197 



0030 0100 

 35"373' 35°33' 

 73°09.7' 73°06' 



I9B 

 0145 

 35°29' 

 73-02' 



36.42 

 227 



040-HOIO 

 199 

 0225 

 35-25' 

 72-59' 



LEGEND 



ISOTHERM 



BOTTOM OF THE 



MIXED LAYER gOO 



s%o a. 



„ ® 



O2 PO,- P 



■ AREA OF INSTABILITY 



Figure 15.-Transect I-Section 12, May 26, 1963. (See caption for fig. 13.) 



nected with development of an intermediate 

 zone. The boundary during a well-developed 

 intermediate zone was found i-ight of its mean 

 position, but the boundary during a weakly 

 developed intermediate zone was left of its 

 mean. Along transect II. the limited number of 



observations suggests that the pattern of oscil- 

 lation was similar to that in transect 1. 



WARM CORE OF THE GULF STREAM 



The core of warmest water was found at or 

 near the left boundarv of the Gulf Stream. The 



GULF STREAM OFF CHESAPEAKE BAY 



401 



