Figure 1.
Values of the slope (a_{1}) coefficients from the
weighted linear leastsquares regression between airsea O_{2}
flux and seasonal heat flux anomalies (ƒ_{O2}=a_{0}+a_{1}[DQ]_{sea})
for the Atlantic, Pacific, and Indian basins and the entire ocean
domain. The vertical error bars represent the ±1 SD of the regression
coefficients in each 10° latitudinal band. 
