The following statistics were computed for Sj, uj, and vj. (Here 
the dummy variable xj is used.) 
< 
© 
Kh 
he 
p 
Bp 
Q 
@ 
Q 
i] 
Standard deviation, o = vo2 
=I 
Skewness 
SIN 
Kurtosis 
3.3 East and North vs. Time 
These diagrams, which accentuate inertial and tidal period 
oscillations, were generated from the uj and vq series by computing the 
60 
SE eae of non-overlapping groups of 60 points, e.aq., Uj = ao } Uys 
U2 = = ) uy and similarly for V. The Um and Vm data sets were the 
61 
l-hour vector averaged east and north component series. 
