TABLES 



Coefficients in the harmonic series for the computation of Q^ at lat. 0' 

 10°, 20°, 30°. and 40° N 



Page 



2. Heat exchange processes for each month, cal. cm7^ day"', July 1963 to 

 June 1965, at Christmas Island, lat. 2° N., long. 157° W.; Johnston Is- 

 land, lat. 16° N., long. 169° W.; and Ocean Weather Station November, 

 lat. 30° N., long. 140° W. Subscripts 1, exchange processes computed 

 daily; subscripts 2, exchange processes computed from mean monthly 

 meteorological processes 10 



3. Differences in extremum values of Q(E|), Q(E2), Q(N|), and Q{N2), lat. 



25° to 29° N., long. 140° to 144° W 16 



4. Interyear comparisons of 4-month averages of Q(E|) and Q(E2), lat. 25° 



to 29° N., long. 140° to 144° W.. 16 



5. Interyear comparisons of 3-month averages of Q(N|) and Q(Ng), lat. 25° 



to 29° N., long. 140° to 144° W 16 



6. Interyear differences of Q(E) and Q(N), lat. 32° N., long. 167° W. (from 

 table B) 17 



7. Interyear differences of Q(E) and Q(N), lat. 17° N., long. 152° W. (from 

 table B) 17 



8. Interyear differences of Q(E) and Q(N), lat. 2° N., long. 157° W. (from 

 table B) 17 



